42C13SE2002 2 17973 WHITE LAKE (NORTH) 010

Geological Report

on the

Spruce Bay Property

White Lake Area, Northern Ontario

Homestake Canada Inc.

3RECEIVED

NOV - 3GEOSCIENCE ASSESSMENT

OFFICE ———-

Ikram (Ike) Osmani, M.Sc.Zlatko Durdevic, B.Sc.Allan MacTavish, M.Sc.|, 0 ^ *

October 20,1997

42C13SE2002 2.17973 WHITE LAKE (NORTH) Q -| QQ

Table Of GUI nema

Page Introduction ..... .. ...... ... ... .. ............ ....................... ... .. ... .... .. ... ...... ... ... lLocation and Access ... ... .. ......... .. ... ... ............... ... ... ... .. ........................... lTopography and Vegetation .......... ... ............... ... .. ... ... ................................. lSurvey Method . . .. ......... ... .. ... ......... .. . .. ... . .. ... ... ........................ ............ lProperty ... ......... .. . .. ............ ... .. ... ....................... ......... ......... ....... .. . 6Regional Geology ............ ... .. . .. ............... ... ... ... ..... ... .... .. ...... ...... ...... . ... 6Exploration History ..... .. . .. ............ ...... ... ..... ... ........................................ 8Property Geology . ... .. ......... ... ..... . .. . .. ... ................................. ......... ... ... 11

Ultramafic to Mafic (komatiitic) Metavolcanic Rocks . ... .. ......... ............... ... .......... 12Mafic Metavolcanic Rocks ........ ... ..... ......... ......... ............................... 13Intermediate Metavolcanic Rocks ............................... ... ........... ... . ........ . . 13Felsic Metavolcanic Rocks . . ................. ... ... .. . ... ........ ... . .. ... ................. 14Chemical Metasedimentary Rocks .................. ...... ... ................................ 14Clastic Metasedimentary Rocks ... ... .. ... ...... ........................... ......... ........ 15Ultramafic Intrusive Rocks ................................................................15Mafic Intrusive Rocks ...... ............... ... ......................................... ... 15Younger Metasedimentary Rocks (Temiskaming-age?) ............ ... ........................... 15Intermediate to Mafic Intrusive Rocks .. ............ ... ... ..... . .............................. 16Intermediate to Felsic Hypabyssal Intrusive Rocks .... ..... ...... ............................... 17Proterozoic Mafic to Ultramafic Intrusive Rocks ................................. ......... ..... 17

Metamorphism .................................... ............... ............................... 17Structural Geology .... ............ ... .. . .. ... ........................ .. .......................... 17Sampling Program .......... ........ ... ......... ................. ......... ....................... 18Lithogeochemistry .......... .. . .. ... ............ .. ... ... ... ... ......... .............. ... ......... 19

Tectonic Environment .......... ... ..... ...... ............................. ............ ... 20Gold and Base Metals Mineralization ... .. . .. ... ... ...... ... .. . .. ...... ............ ...... ... ......... 20Conclusions and Recommendations ... ... .............. ... ... ............... ........ ...... .......... 22Certificate of Qualifications

Ikram (Ike) A. Osmani ... ...... ... ... .. . ............................... ........ ... ........ 23Zlatko Durdevic .............. ... .. ............ .. ... ..................................... 24Allan MacTavish ....... ..... ... ... ........... ............... ..... ....................... 25

References .............. ........ ............ .. . ..... ......... ........ .......................... 26Sample Descriptions ... ..... ... .................... ......... ... ........................... Appendix ISelected Lithogeochemical Results ...... .. . .. ... ............ ................................ Appendix IISelected Lithogeochemical Ranges (Altered and Least Altered) Mean Values for Least Altered Samples . Appendix III Analytical Results ............. ................... .............. . ................. ...... Appendix IVLithogeochemistry and Stereonet Plots ........ ..... ............ .. ... ............ ............. Appendix VOutcrop Photographs ..... ............................ ................................... Appendix VI

List of Figures

Figure l: Location MapFigure 2: Property Location MapFigure 3: Claim Location MapFigure 4: Regional Geology of the Eastern Schreiber-Hemlo Greenstone Belt

List of Maps

Map l: Geology Map ........ ... ......... ... ................. ............................ Back PocketMap 2: Sample Location Map . ......... .. ... .................................. ............ Back Pocket

Introduction

Homestake Canada Inc. optioned the Spruce Bay property from Winslow Gold Corp. in May 1995. This report summarizes the results of geological mapping, lithogeochemical and channel sampling completed on the property between May 26th and July 31, 1997, and presents the data on the l :5000 scale maps accompanying this report (see Back Pockets).

Location and Access

The Spruce Bay property is situated approximately 270 km east of Thunder Bay, Ontario and 50 km northeast of Marathon, Ontario (see Figures l and 2). The northeastern portion of the property straddles Spruce Bay located in the northeastern part of White Lake (see Figure 3). The centre of the property is within NTS 42C/13SE and UTM Zone 16, at 596500E, 5404500N.

Access (see Figure 2) to the eastern claims is by boat or snowmobile, depending on the season, for approximately 9 km north on White Lake from the White Lake narrows public boat launch near Highway 17. The western claims may be accessed by truck or snowmobile along the Wabikoba Lake road, for a distance of 14. l km east from Highway 614 to the Theresa Lake dam, and from there 3 km south by ATC or snowmobile.

Topography and Vegetation

The property exhibits elevations between 1100 m to 1250 m above sea level. The 150 m relief is largely due to a series of west-northwest-trending hills located in the southern and southeastern portions of the property. The western portion of the property is underlain by rolling sand and boulder hills and outcrop exposure is poor to non-existent.

Topographically low and swampy portions of the property are forested by black spruce, cedar, balsam fir, and tag alder, whereas topographically higher, better-drained areas support a growth of white birch, white spruce, trembling aspen, and jack pine.

Survey Method

The Spruce Bay Property was mapped at a scale of 1:5,000 along recently cut grid lines, nominally spaced at 100 m, and oriented at 360" 3 0 . Daily map sheets were drafted onto 1:5,000 scale mylar base maps and digitized using AutoCAD LT. All geological and structural interpretations were completed on hard copy maps plotted by a Hewlett Packard HP 650 Design Jet Plotter. The interpretations were in turn digitized onto the existing digital outcrop maps.

Mapping was completed between May 26 and July 31, 1997, by geologists LA. Osmani, Z. Durdevic, A. Buschman, I. Harrison, and P. Caldbick capably assisted by C. Chataway, D. Pykari, and L. Perron. The mapping and sampling programs were directly supervised by LA. Osmani.

Attawapiskat Lake

Northwestern Ontario

Spruce Bay Property

Figure 1 : Northwestern Ontario Location Map Spruce Bay Property.

•V^—*

SPRUCE BAY PROPERTY

White Lake Provincial ParkCXXDEN QIANT

HOMESTAKE CANADA INC

FIGURE 2SPRUCE BAY PROPERTY LOCATION AND ACCESS

WILLIAMS DAVID BELL

Bomby Date: Revised: Province: NTSune. 1995 October 1 997 Ontario 42C/13SE

HOMESTAKE CANADA INC.

FIGURE 3SPRUCE BAY PROPERTY

CLAIM MAP

Drawn: Data: Scale: GMSI/hci MNDM/hci

Drawing:sb-gfig3.dwg

Date: Revised: Province: NTS:•June, 1995 October 1997 Ontario 42C/13SE

O 0.2 0.4 0.6 0.8 1.0 km

fl LAKE PLUTON

PUKASKWA

GNEISSIC

COMPLEX

LEGEND

PROTEROZOIC

PORT COLDWELL ALKALIC COMPLEX

GRANITOIDS

UNDIFFERENTIATED METASEDIMENTARY ROCKS

HERON BAY ASSEMBLAGE (2.70 Ga)

HEMLO-BLACK RIVER ASSEMBLAGE ^2.71 Ga)

SYMBOLS

^,,"'~ FAULT/SHEAR ZONE

HIGHWAY

CCS - CEDAR CREEK STOCKLSSZ - LAKE SUPERIOR SHEAR ZONEHFZ - HEMLO FAULT ZONERLDZ - ROUS LAKE DEFORMATION ZONEHBDZ - HERON BAY DEFORMATION ZONE

10km

FIGURE 4: Regional geology of the eastern half of the Schreiber—Hemlo greenstone belt. Modified after Williams et al. (1991)

Property

The Spruce Bay property consists of eight contiguous, unpatented mining claims (42 units, approximately 728 hectares) in the White Lake Area (North Part) (Claim Map G-622) of the Thunder Bay Mining Division, Ontario (see Figure 3). The claims are optioned from Winslow Gold Corp. The claims comprising the Spruce Bay Property are listed in Table l, below:

Table 1: Spruce Bay Property Claims List

Claim # No. of Units

10979471183294118673011869781186979119562612103441210345

1112414541

8 claims 42 units

Regional Geology

The Archaean (2.77 Ga to 2.70 Ga, Corfu and Muir 1989) Schreiber-Hemlo greenstone belt of the Wawa Subprovince is situated on the north shore of Lake Superior and extends from near White River in the east to Schreiber in the west (see Figure 4). The eastern Hemlo portion of the belt is separated from the western Schreiber portion by the Middle Proterozoic-age (1.1 Ga, Heaman and Machado 1987), Coldwell Alkalic Complex. The Hemlo belt is bound to the north and south by the composite Black-Pic Batholith/Gowan Lake Pluton and the Pukaskwa Gneissic Complex, respectively. The Pukaskwa Gneissic Complex is composed of migmatitic to gneissic tonalite and, in part, trondhjemite to quartz monzonite. The Black-Pic Batholith is a foliated to massive, composite, domal body composed of a series of tonalitic to granodiorite intrusions. Late-stage, massive gabbro, diorite, tonalite, granite, and granodiorite intrusions have been emplaced through the domal structure (Williams et al. 1991). The southern margins of the Black-Pic Batholith have been intruded by the laterally extensive Gowan Lake Pluton.

The supracrustal rocks of the Hemlo belt were subdivided by Williams et al. (1991) into the 2.77 Ga Hemlo-Black River assemblage to the north and the 2.70 Ga Heron Bay assemblage located south of the Hemlo fault zone. The Hemlo gold deposit and the Spruce Bay Property occur within the highly strained and altered rocks of the Hemlo-Black River assemblage. The property occurs within the North Limb portion of the assemblage.

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The Hemlo-Black River assemblage, as described by Williams et al. (1991), consists of a basal sequence of pillowed, massive and foliated, tholeiitic mafic metavolcanic flows intruded by mafic and ultramafic bodies and an overlying sequence of mafic to felsic, calc-alkalic pyroclastics and flows which may be transitional into greywacke, iron formation, and conglomerate. Volcanic units predominate in the western part of the assemblage, with an increasing abundance of aluminous, clastic metasedimentary rocks to the east (Muir 1982). These supracrustal rocks exhibit widely varying states of strain, with well-preserved primary textures and structures visible within some units and almost completely obliterated original textures in others. The assemblage has been intruded by the Cedar Lake Pluton (2688 Ma) and the Cedar Creek Stock (2684 Ma), in the south, and by the Musher Lake Pluton, in the northeast. It is bound by the Black-Pic Batholith/Gowan Pluton (2.678 Ga) in the northwest, the Dotted Lake Pluton in the east, and the Lake Superior-Hemlo Fault in the south (Williams et al. 1991, Corfu and Muir 1989).

The Heron Bay Assemblage is described by Muir (1982) and Williams et al. (1991) as consisting of two main lithologic divisions comprising one sequence of predominantly tholeiitic mafic metavolcanic rocks and another sequence of calc-alkalic, intermediate to felsic metavolcanic rocks. The mafic metavolcanic rocks are mainly iron tholeiitic, sometimes plagiophyric, massive to pillowed flows that locally host lenses of deformed peridotite, hornblendite, and komatiitic flows. The intermediate to felsic metavolcanic rocks are predominantly pyroclastic with numerous, restricted zones of dacitic to rhyolitic flows, localized interbeds of massive to pillowed mafic iron tholeiitic rocks, and clastic metasedimentary rocks. The intermediate to felsic package strikes roughly east-west and is generally steeply dipping; however, in the Heron Bay area the rocks are gently to moderately northwest-dipping and southwest striking. The assemblage is intruded by the Heron Bay Batholith; in fault contact with the Hemlo-Black River Assemblage to the north; bound to the south and east by the Pukaskwa Gneissic Complex, and truncated to the west by the Coldwell Alkalic Complex.

At least three major (Dt through D3) and one minor deformational events (D4) are documented in the Hemlo area (Muir and Elliott 1987). The Dj event produced a layer-parallel breccia and associated isoclinal folds (FI). The D2 event refolded the Ft folds into S-asymmetry F2 folds and produced tectonic foliation and mineral lineations parallel to the fold axes. The D3 event consisted of major, dextral, ductile shearing and produced associated Z-asymmetry F3 folds. The D3 event is generally thought to accompany, or post-date, the alteration and mineralization related to the Hemlo gold deposits (Muir and Elliott 1987, Williams et al. 1991). The D4 event produced kink folds (F4) commonly exhibiting S-asymmetry. The Hemlo fault zone extends from the Coldwell Alkalic Complex eastward to just south of the Hemlo deposit, where it takes a slight bend, and then extends east-southeast toward the town of White River (Williams et al. 1991). Mafic to ultramafic dykes occur within the fault zone and have been intensely deformed and altered to actinolite-chlorite-talc schists (Williams et al. 1991). The Heron Bay Deformation Zone extends from Heron Bay, on Lake Superior, northeastward where it wraps around the western and northern margins of the Heron Bay Batholith to acquire an easterly strike, joins with the Rous Lake Deformation Zone, identified by HCI geologists during 1996, and then merges with either

the Lake Superior Shear Zone or the Hemlo Fault Zone in the vicinity of the Hemlo deposit (present authors interpretation).

All rock-types are crosscut by north-northeast-trending diabase dykes, possibly of the Marathon swarm, and lesser amounts of northwest-trending quartz diabase dykes of the Matachewan swarm (Osmani 1991).

Exploration History

Exploration activity in the North Limb area has been sporadic with little or no work completed before the 1953 discovery of the Geco Zn-Cu orebody near Manitouwadge. After the Geco discovery the western North Limb area underwent a period of limited base-metal exploration. The 1982 discovery of the Hemlo Gold deposit sparked a staking rush that resulted in considerable renewed interest in the area during the mid 1980's. The subsequent discovery of several gold occurrences in the Armand Lake area during the early 1990's lead to considerable activity which has continued to the present time. All known exploration and government mapping completed in the vicinity of the Spruce Bay Property is summarized below:

1964 to 1965: Township-scale geological mapping by V.G. Milne (1968, Map 2147), of theOntario Department of Mines, documented several base metal occurrences in the area.

1976: Noranda Exploration Co. Ltd. flew an airborne EM and magnetometer survey over the North Limb area.

1976: Noranda Exploration Company Limited completed linecutting, Crone horizontal loop electromagnetic (GEM), vertical loop electromagnetic (VLEM), and magnetometer surveys over a 40 claim group that includes the east-central portion of the Spruce Bay Property. The GEM and VLEM surveys detected numerous weak conductive zones not considered worthy of follow-up.

1978 and 1979: The Geological Survey of Canada (GSC) completed a regional lake sediment and water geochemical survey throughout the North Limb area (Priske et al. 1990b). The original samples were analysed for gold and 25 other elements during 1990.

1983: Aerodat Limited completed a helicopter-borne multi-frequency, multi-coil EM, VLF-EM, and cesium vapour magnetometer survey over the Hemlo area. This data was purchased and submitted for assessment by many companies working in the North Limb area.

1983: Trident Resources Inc. filed the Aerodat airborne data described above on a 22 claimproperty located immediately northwest of the present group. Trident, through contractor AgUis Engineering Ltd., then proceeded with linecutting, geological mapping, rock sampling, soil geochemistry, and ground VLF-EM surveys. The VLF-EM survey delineated 5 major conductive zones within the eastern part of the claims that were

8

thought to have bedrock sources. The geochemical survey detected numerous Au-in-soil anomalies with values ranging from between 20 and 310 ppb. The better soil anomalies roughly coincide with ground VLF-EM conductors. No rock samples returned significant Au or Mo values.

1983: Airborne EM and magnetometer surveys were completed by Baylore Resources Limited over a group located northwest of the Spruce Bay Property that is presently under option to Battle Mountain Gold.

1983: Ventora Resources Limited filed the Aerodat data and completed a reconnaissance grid (200 m line-spacing), preliminary geological mapping, and a soil geochemistry survey on 37 claims overlapping the western Spruce Bay claims. The soil survey detected a few weakly anomalous Mo, As, and Zn values; however these were not thought to be significant and no other work was done.

1983 to 1984: Manwa Exploration Services Ltd completed VLF-EM and magnetometersurveys and geological mapping for R. J. McGowan on the Solong Lake Property, which encompasses the western portion of the Wabikoba Property (adjacent to the northwest of the Spruce Bay Property). Three conductors of uncertain significance were delineated.

1984: A reconnaissance grid (200 m line-spacing) and ground magnetometer and VLF-EMsurveys were completed by David Burda on an 18 claim group straddling the centre of the present claim group. Numerous short strike-length VLF-EM conductors were detected, most associated with the volcano-sedimentary contact or diabase dykes. Conductor 'A' was thought to represent a fault located along the granitoid-sedimentary contact in the south part of the claims.

1984: Midnapore Resources Inc. completed geological mapping, outcrop sampling, ground VLF-EM, magnetometer, and IP surveys, and 7 diamond drill holes, totalling 775.9 m, over claims that included the adjacent Wabikoba Property and areas to the north and northwest. The mapping outlined a zone of sulphide mineralization occurring within felsic crystal tuffs adjacent to a contact with mafic metavolcanic rocks. Three grab samples (MIN-5924,-5926 and -5930) taken to the northeast also contained anomalous gold values ranging between 100 and 255 ppb. These results, in conjunction with soil anomalies and geophysical data led to the delineation of at least five zones of interest. The diamond drill program intersected several zones of disseminated sulphides within the sedimentary and mafic metavolcanic rocks. Anomalous gold values, in the order of 210 to 300 ppb/1.0 m, were reported from the sulphide intersections. Trenching and further diamond drilling were recommended, but were never completed.

1985: G.M. Siragusa of the Ontario Geological Survey mapped the North Limb area at a scale of 1:15840 (l incl^l/4 mile).

1987 and 1988: Noranda Exploration Co. Ltd. optioned three adjacent properties (theMcGowan, Tylox, and Wabikoba projects) located northwest of the Spruce Bay Property. They re-sampled some of Midnapore's drill intersections (49 samples), and also collected 21 surface grab samples. Three grab samples taken from felsic tuff and siliceous argillite near the Theresa Lake dam, assayed 200 ppb Au. Trenching was completed on portions of the Tylox and McGowan claims located to the north of Wabikoba property in the vicinity of Theresa Lake. One sample, taken from pyritic, silicified, sericitized, graphitic sediments within the "McGowan Trench", yielded 120 ppb Au. The McGowan option was terminated and the claims were transferred back to the owner. Noranda also conducted a mapping program on the small Wabikoba claim-block located immediately north of Solong Lake, but no zones of interest are reported.

1989 to 1994: Considerable prospecting, outcrop stripping, bedrock trenching, and rock sampling were completed by Daniel Carroll on 6 claims, one of which is part of the present Spruce Bay Property. Three samples of pyritic metasedimentary rock, taken from a series of trenches in 1990 and 1991, contained 6850 ppb Au (0.20 oz/ton) and 79 ppm Ag; 5400 ppm Zn; and 745 ppb Au, 6730 ppm Zn, 2.4 ppm Ag, and 54 ppm Mo, respectively. Oracle Minerals Inc. optioned the claims in 1994 and completed geological mapping and sampling. Sample results were disappointing and no further work was done.

1991 to 1992: Trenching, and limited prospecting and sampling were completed by Brian Fowler and Mike Shuman on the adjacent Wabikoba claims. A total of 500 m of excavation, in the form of four trenches, were completed along the contact between mafic metavolcanic and intermediate to felsic pyroclastic rocks. A gossanous, mineralized shear was outlined within the mafic volcanic rocks. A few grab samples taken by the owners assayed up to 171 ppb Au, but the locations of these samples are uncertain. A reconnaissance till sampling survey was completed in the vicinity of the property by I.M. Kettles (1993) of the Geological Survey of Canada. Several anomalous copper, zinc, nickel and gold values were reported.

1992: A 25 claim property, which included claims now forming the eastern portion of the Spruce Bay Property, was explored by Brian Fowler and Angus MacDonnell. Work completed included geological mapping, prospecting, trenching and sampling.

1993 to 1994: Exploration work was carried out by Brian Fowler, Mike Shuman, George Daniels, andDoug Kakeeway on the present Spruce Bay property. In 1993 they completed prospecting, sampling, and a beep mat survey. One sample of altered pyritic metasediments, taken from a 2 m wide gossanous zone exhibiting coincident ground VLF- EM, and magnetometer anomalies, graded 2132 ppm Zn. The owners attempted to drill this zone, but collared the hole too far north and missed the target. Exploration in 1994 consisted of linecutting (winter grid, 200 m line-spacing), ground magnetometer, VLF- EM, MaxMin-n (HLEM), and limited IP surveys. The HLEM survey was completed over the entire claim block and outlined 4 conductors of various strengths and strike-lengths.

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The VLF-EM survey was completed over the western portion of the group in order to aid in better defining geology and structure. The survey outlined several east-west-trending conductive zones thought to have bedrock sources. The property was optioned to Winslow Gold Corp. in 1995, but there is no record of any work being done until Homestake Canada Inc. optioned the claims late in April 1996.

1995 to 1997: The adjacent Wabikoba claims, registered to A. MacDonnell, Mike Shuman, and Brian Fowler, were optioned to Oracle Minerals Inc. in 1994, and were subsequently optioned by Homestake Canada Inc. in June 1995. Linecutting, ground magnetometer and VLF-EM surveys were completed by Rayan Exploration Ltd. During mid-1995. This was followed by a gradient/'RealSection' IP/Resistivity survey, contracted to Quantec IP Inc. during March and early April of 1996, and rehabilitation of the existing grid shortly thereafter. Geological mapping at a scale of l: 5000 was completed during September and October of 1996. The property was returned to the owners at the end of May 1997.

1995 to 1997: Homestake Canada Inc. completed a grid and a detailed ground magnetic survey on the Spruce Bay Property late in 1996. A reconnaissance, dipole-dipole IP survey was completed over the western and central portions of the property between the end of March and mid-July 1997.

Property Geology

The Spruce Bay property is located within the southeast-trending, North Limb portion of the eastern Schreiber-Hemlo greenstone belt. The property is located approximately 10 km southeast and apparently along strike from the North Limb property, now owned by Battle Mountain Canada Ltd. The 1995 Annual Report of the former owner, Hemlo Gold Limited, states that results from the North Limb Property were encouraging. Diamond drilling intersected a number of interesting, although subeconomic, gold intercepts within strongly altered rocks interpreted as similar to those observed within the Hemlo gold deposit.

The Spruce Bay Property is underlain by mafic to ultramafic metavolcanic flows, mafic and ultramafic intrusive rocks, minor intermediate to felsic pyroclastic rocks, some intermediate hypabyssal intrusive rocks, and fine to coarse clastic metasedimentary rocks. These rocks have been deformed and contact metamorphosed by the contact strain aureoles of the late-Archaean Dotted Lake Batholith, the Musher Lake Pluton, and the Spruce Bay Pluton (HCI term) situated north, northwest, and southeast of the property, respectively. AU rock-types are crosscut by north-northeast-trending diabase dikes, possibly of the Marathon swarm (Osmani 1991).

The supracrustal rocks observed within the Spruce Bay and the adjacent White Lake Property are informally subdivided into two main sequences:

1. An older ^2.77 to 2.70 Ga, Corfu and Muir 1989) Keewatin-age volcanic sequence, that is further subdivided into lower (LVG) and upper (UVG) volcanic groups,

11

and is located north and south of an east-southeast-trending line roughly defined by the centre of Spruce Bay of White Lake. The UVG is dominated by tholeiitic to calc-alkalic mafic and intermediate volcanic rocks, whereas the LVG is underlain by complexly folded, intercalated, komatiitic to tholeiitic metavolcanic rocks. There is no clear transition between the LVG and UVG, therefore, the groups are not differentiated on the accompanying geology map (see Map l, Back Pocket).

2. A younger ^2.70 Ga), unconformably (?) overlying, coarse clastic metasedimentary sequence, composed predominantly of conglomerate. This sequence dominates the western portion of the property. It may be coeval with the Timiskaming- age Matawin Sequence of the Shebandowan Greenstone Belt (Osmani 1997, Rogers and Berger 1994).

The sequences and groups were defined on the basis of field relationships; stratigraphic facing directions; architecture of flow units; limited U-Pb age data on correlative units in the Hemlo area; and lithogeochemical signatures (see Appendix III). It should be noted that younging directions and structural facing were often difficult to impossible to obtain due to the obliteration of primary textures and structures by deformation and metamorphism.

Ultramafic to Mafic Metavolcanic Rocks:

Most of the ultramafic to mafic metavolcanic rocks occur southwest of Spruce Bay within the central portion of the property. The rocks are predominantly komatiites, locally grading into basaltic komatiites, and contain between 14 and 32.7 wt.% MgO (20.18 wt.% MgO average, see Appendix EI). They consist of generally non-magnetic, spinifex-textured, pillowed to massive, polysutured flows, associated breccias, and derived schists (tremolite/actinolite-serpentine- carbonate magnetite muscovite/phlogopite schist). The flow sequences are intruded by numerous, sill-like, moderately to strongly magnetic peridotite, pyroxenite, and gabbro bodies, up to 100 m in thickness, that usually display sharp, subconcordant to discordant contacts with the komatiitic flows. The ultramafic intrusions are generally medium- to fine-grained, massive, and occasionally display polygonal jointing. Relatively undeformed flows, with the exception of some spinifex-textured units exhibiting 1-5 cm olivine/pyroxene blades, are generally fine- to medium- grained and display characteristic primary textures and structures. Within high strain zones the flows are much more strongly deformed (strongly foliated to schistose) than their intrusive counterparts.

The ultramafic flow sequences generally consist of several individual flows between l and 5 metres in width, that are traceable, albeit discontinuously, for hundreds of metres along strike. The best example of the various flow features was observed within a single outcrop at L2+50W, 13+50N. Here a l m thick flow exhibited a well-developed spinifex-textured core, a narrow, chilled, flow-top breccia, and was in contact with an underlying massive, polysutured ultramafic flow. This flow is overlain by l m thick, spinifex-bearing, pillowed to massive flows exhibiting chilled or contorted flow contacts.

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The ultramafic flows rarely display contacts with the mafic metavolcanic rocks. In most cases contacts are obscured by the high metamorphic grade and the poorly exposed/lichen covered nature of the outcrops. However, some well-preserved ultramafic flows are observed to grade into transitional, less ultramafic, basaltic komatiite to high-MgO tholeiitic basalt, and then into more typical, tholeiitic, mafic metavolcanic rocks. Compositional grading is usually marked by changes in primary textures and relative differences in hardness and colour. For example, the ultramafic flows are generally soft, weather emerald green to rusty brown, and exhibit greyish- green to grey fresh surfaces. The mafic metavolcanic rocks are harder and weather various shades of grey, green, or brown, with green to greenish-black fresh surfaces.

Mafic Metavolcanic Rocks:

The mafic metavolcanic rocks are the most abundant supracrustal rock-type observed within the property. They primarily consist of fine- to medium-grained, amphibolitized, locally variolitic, pillowed to locally massive flows and associated breccias, with minor medium- to coarse-grained flows and other fragmental rocks, such as tuffs and lapilli tuffs. The flows contain no amygdules, which suggests deep-water deposition. All units are variably deformed and range from moderately foliated to highly schistose to locally gneissic. Mafic metavolcanic rocks proximal to the Spruce Bay Pluton (SBP), are deformed and metamorphosed to the extent that primary mineralogy, textures, and structures are completely destroyed. These rocks display mm- to cm-scale, bands defined by dark green to black amphibole (hornblende?)-biotite-rich layers alternating with plagioclase-quartz epidote layers. The banded structures may represent highly deformed and metamorphosed pillows

Most pillowed flows, and their derived schists, are strongly flattened and are usually unsuitable for younging and structural facing determinations. However, a few, relatively well- preserved, locally overturned pillows, occurring within the central portion of the property, suggest the presence of tight to isoclinal, property-scale folding.

The mafic flows present within the central portion of the property are intercalated with ultramafic flows. Sharp contacts are rarely observed between the mafic and ultramafic volcanic units. Most mafic flow units display compositional grading, suggesting formation by fractionation of the ultramafic parental magma responsible for the komatiitic flows.

Intermediate Metavolcanic Rocks:

Few intermediate metavolcanic rocks occur on the property. When observed they form narrow, ash tuff, crystal tuff, and minor lapilli tuff units that occur throughout the property. The lapilli tuff usually consists of flattened, elongated, subround to subangular, intermediate, plagiophyric fragments, ^ mm to 5 cm in length, contained within a fine-grained, strongly foliated to schistose, aphyric to feldspar crystal-bearing, intermediate matrix of dacitic to andesitic composition. In most cases, stratigraphic top directions are indeterminant because original textures and structures are obscured or destroyed by deformation and metamorphism.

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The intermediate pyroclastic rocks occur as laminated to poorly sorted, lapilli tuff to tuff units interlayered with, or compositionally gradational into, mafic or felsic metavolcanic units. The fragmental rocks occurring outside of the south central part of the property, are interlayered with, or gradational into, mafic metavolcanic and metasedimentary rocks, probably reflecting a distal, subaqueous environment. The intermediate pyroclastic rocks present within the south central portion of the property often grade into relatively thick felsic pyroclastic units. This gradational relationship suggests derivation by fractionation of intermediate and felsic members from the same parental magma in a subaerial environment. This association may represent a separate volcanic cycle for the intermediate to felsic pyroclastic sequences.

Felsic Metavolcanic Rocks:

Felsic metavolcanic rocks primarily occur within the south central portion of the property and seem to comprise two belts:

1. A northern felsic metavolcanic belt (NFB). The NFB occurs near the northern property boundary and forms a discontinuous belt, up to 60 m thick, extending eastward from L13+OOW to the southern arm of Spruce Bay, a distance of 2200 m. A sinistral, north-south-striking fault truncates the unit within the bay.

2. A southern felsic metavolcanic belt (SFB). The SFB occurs adjacent to the Spruce Bay pluton, near the southern property boundary, and forms an east- to northeast-striking, up to 400 m thick sequence, approximately 1700 m in length. Adjacent to the pluton the rocks are folded and rotated in an anticlockwise sense.

The felsic pyroclastic rocks of the NFB and SFB predominantly consists of lapilli tuff to crystal tuff. The lapilli tuff contains elongated, flattened, 3 mm to 6 cm, quartz- or feldspar-phyric felsic clasts within a quartz- or feldspar-phyric, felsic tuffaceous matrix. Since the clasts and matrix are similar in composition the unit is interpreted as a primary pyroclastic deposit. The presence of medium-grained units within the felsic belts also suggests reworking and a distal source for some of the rocks. Proximal to the Spruce Bay pluton (SBP) the rocks are highly deformed and strongly metamorphosed to schists and gneisses.

Chemical Metasedimentary Rocks:

Chemical metasedimentary rocks are rare and when observed occur mainly within the eastern portion of the property. They comprise banded oxide and silicate facies ironstones that generally contain *^1 to 5*^o disseminated, stringered, or blebby pyrite and pyrrhotite and may contain significant base metal mineralization. One magnetite ironstone exposed along the western shoreline of the southern arm of Spruce Bay (approximately L7+65E, 9+OON), contains 2 to S0A, disseminated and blebby pyrite, bornite, chalcopyrite, and sphalerite. This unit contained 8560 ppm zinc, 547 ppm copper, 297 ppm nickel, and 18 ppm molybdenum.

14

Clastic Metasedimentary Rocks:

Interflow clastic metasedimentary rocks occur throughout the property. They form narrow, cm-scale to 10 metre thick lenses of wacke, siltstone, pelite, arkose, arenite and derived schists, commonly intercalated with mafic and intermediate metavolcanic rocks.

Ultramafic Intrusive Rocks:

The ultramafic intrusive rocks consist of sills, dikes, and bodies of peridotite, pyroxenite, hornblendite, and derived serpentine-tremolite/actinolite-chlorite-talc carbonate magnetite schist, that predominantly occur within the northeastern half of the property. The largest intrusion underlies much of Spruce Bay and outcrops along the bay's southwestern shoreline. It is a west- northwest-trending, 50 m to greater than 300 m thick, 2.5 km long, sill-like body composed of medium- to coarse-grained, strongly magnetic, massive to polygonally-jointed peridotite exhibiting minor dunitic phases. The peridotite weathers rusty-brown to greyish-white with greyish or greenish-black fresh surfaces. Elsewhere the ultramafic intrusions occur as narrow, short strike-length dikes or sills rarely greater than 25 m thick and 300 m in length.

Most of the ultramafic intrusions are spatially associated with bodies of gabbro; however, within the central portion of the property ultramafic and associated mafic intrusions appear to have been emplaced at, or near, the contacts between komatiitic and tholeiitic volcanic rocks. The ultramafic to mafic intrusive bodies emplaced within ultramafic to mafic volcanic sequences are probably comagmatic with their extrusive counterparts.

Mafic Intrusive Rocks:

Sill-like, mafic intrusive bodies composed of massive, medium- to coarse-grained, occasionally pegmatitic, locally plagiophyre, hornblende gabbro, melagabbro, leucogabbro, and derived schists, occur throughout the property and range from less than 10 m to greater than 350 m in width. The majority of the sills are concordant with, or slightly oblique to, volcanic layering and earlier tectonic fabrics; however, on a property scale, some of the intrusions are folded, sheared, and altered, much like their metavolcanic host rocks. The largest intrusion observed strikes northwest-southeast across the northeastern hah0 of the property, varies between 75 and 350 m in width, and was emplaced within, and is crosscut by, the north and south branches of the Spruce Bay Shear Zone. The strong shearing observed suggests that sill emplacement predated much of the regional shearing event The intrusion roughly separates the predominantly tholeiitic to calc-alkalic volcanic sequence in the north (LVG) from the mixed komatiitic and tholeiitic sequence to the south (UVG).

Younger (Temiskaming-age?) Metasedimentary Rocks:

The southwestern portion of the property is dominated by a thick, folded sequence of coarse, poorly sorted, predominantly matrix-supported, polymictic conglomerate. The sequence

15

consists of flattened, subround to round, often subangular, cobble- to pebble-sized, occasionally boulder-sized, clasts of mafic and felsic metavolcanic rocks, gabbro, and granitic rocks within a matrix of poorly sorted intermediate to mafic wacke. The majority of the conglomerates are intermediate or felsic in composition; however, rare ultramafic to mafic conglomerate units were observed in two localities (L5+OOE, 2+95N and L7+90E, 2+50N) and consist of ultramafic, mafic, and feldspathic, intermediate clasts contained within a schistose ultramafic matrix. The presence of altered and deformed clasts, similar in appearance to nearby metavolcanic and intrusive rock-types, strongly suggests that the conglomerate is locally derived and may be considerably younger than its source rocks.

The conglomerates may be equivalent to the Timiskaming-age (2699 Ma to 2689 Ma) pyroclastic and clastic metasedimentary rocks of the Shebandowan greenstone belt (Osmani 1997, Rogers and Berger 1994). The metavolcanic rocks on the Spruce Bay Property are interpreted correlative with the 2777 Ma to 2700 Ma metavolcanics of the Hemlo area (Corfu and Muir 1989). The granitic rocks adjacent to the Spruce Bay Property have been dated at 2688 Ma to 2684 Ma (Corfu and Muir 1989), therefore, the presence of younger, very similar appearing granitic clasts within the conglomerates suggests a Timiskaming-age ^2684 Ma) for the unit.

Intermediate to Mafic Intrusive Rocks:

Volumetrically minor amounts of steeply dipping, foliated, intermediate to mafic dykes and sills, consisting of aphyric to porphyritic diorite to gabbro, occur throughout the property. The porphyritic varieties consist of 10 to 20*^6,2 to 4 mm, deformed plagioclase or hornblende phenocrysts within an intermediate to mafic groundmass.

A variety of field relationships and the relative ages between these intrusions and other rock-types present within, and adjacent to, the property suggest that the intermediate to mafic dykes or sills are younger than the Keewatin-age supracrustal and associated intrusive host-rocks and older than the possibly Timiskaming-age conglomerates. The minor intrusions crosscut all Keewatin-age rocks, but do not appear to crosscut the conglomerates which contain feldspar and hornblende-phyric, intermediate to mafic, intrusive clasts similar to the observed dykes and sills.

Intermediate to Felsic Hypabyssal Intrusive Rocks:

Massive to foliated, aphyric to feldspar and quartz-feldspar porphyritic hypabyssal intrusive rocks, and their altered equivalents, are not common on the property. They generally occur as moderately- to steeply-dipping dykes or sills containing 20 to SW/o, 2 to 5 mm, subhedral to anhedral, feldspar and subround quartz phenocrysts contained within a fine-grained to aphanitic, intermediate to felsic groundmass. Quartz phenocrysts tend to be smaller in size and subordinate in number to feldspar phenocrysts. Strongly foliated to schistose, altered porphyries are difficult to distinguish from intermediate crystal tuffs.

16

Late Archaean Felsic to Mafic Intrusive Rocks:

The composite, late Archaean Spruce Bay Pluton (SBP) underlies the southern and southeastern margins of the property. Numerous dykes and sills associated with the pluton occur throughout the property. The pluton and associated minor intrusions are composed of equigranular, rarely porphyritic, medium- to coarse-grained, massive to locally foliated and gneissic granodiorite, quartz monzodiorite, diorite, and minor tonalite, quartz diorite, granite, gabbro, and monzogabbro. The foliated and gneissic varieties are common near the SBP/supracrustal contact.

Proterozoic Mafic to Ultramafic Intrusive Rocks:

Proterozoic mafic and ultramafic intrusive rocks include diabase, gabbro, pyroxenite, hornblendite, and lamprophyre and occur throughout the property as dykes and plugs. The most abundant are north- to north-northeast-trending, medium- to coarse-grained, non-foliated, strongly magnetic, diabase dikes of the Marathon swarm (2.17 Ga, Osmani 1991). They range from less than 5 to 80 m in width and intrude all Archaean-age rock-types. A few gabbro, pyroxenite, and lamprophyre dikes occur locally and may be coeval with the Coldwell alkalic complex (1.1 Ga, Heaman and Machado 1987).

Metamorphism

Metamorphic grade ranges between lower- and mid-amphibolite facies with higher-grade rocks occurring within the contact-strain aureole of the Spruce Bay Pluton. Within the aureole mafic metavolcanic, and associated intrusive rocks, exhibit mm- to cm-scale, often garnetiferous, protogneissic layering consisting of alternating, diffuse, dark, hornblende biotite-rich and light, plagioclase-epidote-quartz-rich bands. Intermediate to felsic metavolcanic rocks within the aureole are reduced to plagioclase-muscovite-biotite hornblende quartz schist.

Supracrustal rocks occurring outside the contact-strain aureole exhibit assemblages consistent with lower-amphibolite facies metamorphism overprinted by a weak retrograde metamorphic event that approached mid- to upper-greenschist facies. Locally primary textures and structures, such as spinifex-texture and pillows within mafic and ultramafic metavolcanic rocks, are well-preserved within the north-central portion of the property. The mafic metavolcanic rocks in that area are moderately foliated and generally exhibit the assemblage actinolite-plagioclase carbonate. Ultramafic metavolcanic and associated intrusive rocks generally exhibit assemblages containing a variety of tremolite/actinolite-carbonate serpentine olivine magnetite chlorite biotite.

Structural Geology

Three generations of tectonic foliation (S,, S2 and S3) were observed within the property. The dominant Sj foliation generally conforms to bedding and is northwest- to west-striking, but

17

anticlockwise deflections are evident proximal to the Spruce Bay Pluton and the White Lake Fault. The S2 foliation usually deviates 10 to 150 clockwise from the S t foliation and is oblique to observed bedding and volcanic layering. A weak, north-northeast-striking S3 foliation was observed adjacent to late faults, shears, and diabase dikes.

Linear fabrics are defined by preferentially oriented prismatic to acicular metamorphic minerals, such as actinolite; the elongation/stretching of clasts within conglomerate; and the hinge lines of mesoscopic folds. With few exceptions, these linear fabrics plunge 500 to 850, west- northwest.

Pillow tops, graded bedding, and individual flow-unit architectures were used to define younging directions. Well preserved pillowed flows display a common variation of top directic between south and north and the repetitious nature of supracrustal units strongly suggests the

symmetry parasitic folds

Two of the most prominent, large-scale structures on the property are:

1. The Spruce Bay Shear Zone (SBSZ): This dextral, northwest-trending system transects the northeastern half of the property and partially defines the north and south shorelines of Spruce Bay. This shear system consists of three, subparallel, steeply dipping, linear structures referred to as the north, central, and south Spruce Bay shear zones on Map l (see Back Pocket). These zones, and their associated splays, are characterized by penetrative schistosity, discrete, anastomosing, outcrop-scale shear zones, linear topographic features (lineaments), and variably silicified and carbonatized host-rocks. These structures are partially discernible using ground magnetic data (Osmani et al. 1997b) and are characterized by long, linear zones of low to high magnetic intensity with magnetic anomaly trends parallel to tectonic foliation trajectories (Osmani et al. 1989).

2. The White River Fault (WRF): The sinistral, northeast-striking fault transects the southeastern portion of the map area, partially defines the contact between the Spruce Bay Pluton and the adjacent supracrustal rocks, and truncates the southeastern extension of the Spruce Bay Shear Zone.

Sampling Program

A total of 462 surface grab and channel samples were collected during the 1997 field season (see Map 2, Back Pocket). All samples were submitted to XRAL Laboratories, Rouyn- Noranda, Quebec, and were analysed for gold and base metals (see Appendices I and II). In addition, whole rock lithogeochemical analyses (major oxides and selected trace elements) were completed on 316 of the samples (see Appendix IV). The whole rock samples included both altered and least altered metavolcanic, metasedimentary, and intrusive rocks. The

18

lithogeochemical range between altered and least altered samples of specific rock-types and mean geochemical values for the least altered samples are presented in Appendix III. No rare earth elements (REE's) analyses were completed.

Lithogeochemistry

A detailed study involving the determination of elemental mobility/immobility and addition/subtraction to define specific alteration signatures is a time consuming process and was not attempted within this report. What is presented is a brief discussion of the lithogeochemistry of variably altered extrusive and intrusive rocks from the Spruce Bay property. Most of the diagrams described below (see Appendix V) were designed for use with unaltered, relatively unmetamorphosed rocks and should be used and interpreted with caution when applied to strongly deformed and metamorphosed Archaean-age rocks.

Figures 5, 6, and 7 illustrate the subalkalic nature of the felsic to ultramafic metavolcanic, mafic and ultramafic intrusive, and felsic to intermediate intrusive rocks (granitoid and hypabyssal intrusions), respectively.

The granitoid and intermediate to felsic hypabyssal rocks all plot within, or near, the assigned lithogeochemical fields of the various plutonic rocks on the Q-P discriminant diagram of Debon and Le Fort (1983; see Figure 8). The hypabyssal intrusions (filled triangles) fall within, or very near, the tonalite and granodiorite fields (fields l and 2, respectively), whereas, samples taken from the Spruce Bay Pluton and its associated dikes and sills (half-filled circles) display a much wider lithgeochemical range and plot within the granodiorite, tonalite, quartz monzodiorite, monzogabbro, and gabbro fields (fields 3, 4, 7, 8, and 12, respectively).

All selected metavolcanic samples were plotted on Jensen Cation (Jensen 1976) and AFM (Irvine and Baragar 1971) plots (see Figures 9 and 10, respectively). Although the data is scattered and diffused by metamorphism these plots still suggest the presence of both a calc- alkaline and a tholeiitic metavolcanic sequence within the Spruce Bay Property. Most of the samples appear to exhibit calc-alkaline affinities.

The lithogeochemistry of the various metavolcanic rocks is best illustrated on separate Jensen Cation Plots. The ultramafic to mafic flows exhibit a tight, linear cluster within the peridotitic and basaltic komatiite fields (see Figure 11). Most the mafic metavolcanic rocks form a large diffuse cluster straddling the high-iron tholeiite, high-magnesium tholeiite, calc-alkaline basalt, and tholeiitic andesite fields (see Figure 12). Most intermediate metavolcanic pyroclastic rocks plot within the calc-alkaline andesite and dacite fields (see Figure 13). All felsic pyroclastic samples form a very tight cluster within the calc-alkaline rhyolite field (see Figure 14).

The ultramafic and mafic intrusive rocks display lithogeochemical trends and ranges similar to their extrusive counterparts on the Jensen Cation and AFM plots (see Figures 15 and 16, respectively).

19

Diabase dykes fall within, and adjacent to, the high-magnesium tholeiitic basalt field on the Jensen Cation Plot (see Figure 17).

Tectonic Environment:

/. Mafic Volcanic and Intrusive Rocks: An attempt is made here to determine the tectonic environment for the Spruce Bay mafic metavolcanic rocks, and their synvolcanic intrusive counterparts, by employing Mn-Ti-P ternary discrimination plots (see Appendix V) developed by Mullen (1983). This method is generally applied to mafic volcanic rocks; however, mafic intrusive rocks have been included here because they are considered by the authors to be synvolcanic in origin. The Mn-Ti-P ternary plot was originally developed for unaltered, modern volcanic rocks and should be used and interpreted with caution when applied to metamorphosed Archaean rocks. Figure 18 shows that a majority of the mafic metavolcanic rocks plot within the island arc tholeiite (IAT) and calc-alkalic basalt (CAB) fields, with a small cluster plotting within the mid-oceanic ridge basalt (MORB) field. With the exception of one sample, all mafic intrusive rocks (see Figure 19) concentrate within the IAT field, suggesting that their emplacement was related to island arc-type volcanism and that they may be genetically related to the IAT basalts observed within the property. The sample scatter observed on both figures is probably due to metamorphism.

2. Granitoid Rocks: The tectonic environment during the emplacement of the Spruce Bay Pluton, related minor intrusions, and intermediate to felsic hypabyssal dykes and sills was determined by the use of Rb/Y+Nb and Nb/Y discrimination diagrams (see Appendix V) developed by Pearce et al.(1984). All samples plot within the volcanic arc granite (VAG) field of Figure 20 and the VAG/syn-collisional granites field of Figure 21. These plots support the premise that most of the volcanic rocks present within the property were formed in an island arc environment (see Figures 18 and 19).

Gold and Base Metals Mineralization

As previously mentioned a total of 462 grab and channel samples were collected during the 1997 field season. Sample locations are presented on Map 2 (see Back Pocket), sample descriptions and gold analyses are listed in Appendix I, selected base metal analyses are presented in Appendix II, and a complete list of analyses are presented in Appendix III.

No significant gold mineralization was observed within the Spruce Bay property and all samples analysed for gold fall into the following categories:

1. ^ ppb Au: 32.907o;2. l to lOppbAu: 63.207o;3. 11 to 20 ppb Au: 2.807o; and4. 21 to 152 ppb Au: I.l 07o.

20

All samples were also analysed for base metals. Approximately 30"^ of the samples yielded more than an arbitrarily assigned background value of 200 ppm for Cu, Zn, and Pb. Any Mo value above 10 ppm is considered to be anomalous for the area. Any sample, yielding at least one anomalous base metal value, is presented in Appendix II.

Anomalous base metals values are generally associated with pyrite, sphalerite, and minor molybdenum, bornite, chalcopyrite, and pyrrhotite mineralization and comprises three styles of mineralization on the property:

1. Cyprus-type: This stratabound/stratiform mineralization style occurs within rusty, silicified, sometimes sheared, pillowed, mafic to ultramafic metavolcanic flows or interflow clastic metasedimentary rocks in close association with ultramafic and mafic intrusions. Anomalous to low grade base and precious metals values were observed at three locations:

a) The Point Zone (L8+OOE, KH-50N to 11+OON; see Maps l and 2): This previously unknown zone occurs within mafic to ultramafic flows, and associated narrow, mafic and ultramafic dykes and sills, containing l to 507o disseminated pyrite, pyrrhotite, bornite, and chalcopyrite. Grab and channel sampling obtained values of up to: 3680 ppm Zn; 613 ppm Cu; 12 ppm Mo; and 152 ppb Au (grab samples SB 119238 to SB 119244 inclusive, and channel samples SBC85214 to SBC85240 inclusive; see Appendices I and II).

b) The Carol! Showing (L1+65W, 11+15N, see Maps l and 2): occurs within mafic to ultramafic, pillowed to massive flows containing l to S^/o, locally up to I W/o, disseminated and blebby pyrite, sphalerite, and pyrrhotite. Samples taken by Dan Carroll in 1990 and 1991 contained as high as 6850 ppb Au, 70 ppm Ag, 6730 ppm Zn, 54 ppm Mo. HCI sampling of the 7 known shallow trenches were very disappointing and did not exceed 1240 ppm Zn, 266 ppm Cu, 0.4 ppm Ag, 7 ppm Mo, and 14 ppb Au (Samples SB119218 to SB 119225). This showing is hosted by a similar lithologic package and contains a metal association similar to 'The Point Zone", described above, and is interpreted to occur within the same complexly folded, stratigraphic horizon.

c) L7+65E, 9+OON (see Maps l and 2): At this location, up to 8560 ppm Zn, 547 ppm Cu, and 10 ppb Au were obtained from magnetite ironstone intercalated with ferruginous siltstone containing 2 to 5Vo pyrite, bornite, and sphalerite (sample SB 119248).

The above base and precious metal occurrences exhibit similar lithologies, alteration, and mineralization styles and may all occur within a single, stratigraphic horizon that has been affected by at least two periods of folding, the first of which was tightly isoclinal. The style of mineralization and its host-rocks suggests a setting and metal association similar to Cyprus-type sulphide mineralization. Cyprus-type mineralization is known to occur exclusively within mafic interflow metasedimentary rocks (Rogers et al. 1995) with mafic and ultramafic intrusions providing a heat source and possibly a source of sulphides (Osmani 1996).

21

2. Shear/quartz vein-hosted: Sulphide-bearing to sulphide-rich shear zones, often containing quartz and quartz carbonate albite veins and stringers, in close association with aphyric to porphyritic, intermediate to felsic dykes, is the most commonly observed mineralization on the property. Host rocks include mafic flows and intermediate to felsic pyroclastic rocks. Molybdenum is the most abundant base metal observed and is occasionally accompanied by geochemically anomalous Au. The highest Mo value (241 ppm) was obtained from a rusty quartz vein (sample SB85302, L5+90W, 5+OON) occurring within mafic flows in close proximity to a narrow, northeast-trending shear zone. Anomalous Mo was also encountered along the northwestern shore of the south arm of Spruce Bay, adjacent to the southern branch of the Spruce Bay Shear Zone and many east and northeast-trending shears and faults adjacent to the Spruce Bay pluton (see Appendix I and II). Mo Au mineralization appears to be spatially, possibly temporally, associated with regional shearing and faulting and late-Archaean, granitic intrusions in the White Lake area.

Apparently anomalous values of up to 1780 ppm Cr and 863 ppm Ni within the ultramafic to mafic flows and intrusive rocks represent Cr and Ni contained within primary olivine grains, not within sulphides. These analyses are not anomalous and represent normal background values for the ultramafic host-rocks. This is supported by Middlemost (1985) who states that high- magnesium basalts can contain up to 750 ppm Cr and 150 ppm Ni and peridotitic komatiites up to 2530 ppm Cr and 1380 ppm Ni.

Conclusions and Recommendations

Bedrock mapping (1:5000 scale) and detailed lithogeochemical grab and channel sampling (462 samples) were completed during the summer of 1997. No significant gold mineralization was encountered on the property. It is recommended that no further work be completed by HCI and the option on the property be dropped.

It should be noted that several, previously unknown, low-grade zones of Zn and Cu mineralization were discovered during the mapping and sampling program. Some of these occurrences may have the potential of hosting economic Zn-Cu mineralization. Homestake Canada Inc. is not in the business of exploring for base metals if there is no significant accompanying gold mineralization; however, it would be remiss of the authors if we did not recommend that the owners of the property follow-up on the base metals potential.

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Certificate of Qualifications

I, Ikram (Ike) A. Osmani of 2640 South Lane Road, Sudbury, Ontario, do hereby certify that:

1) I am a graduate of University of Lucknow, Lucknow, India, with a Batchelor of Science Degree in geology (1971).

2) I hold a Master of Science Degree in geology from Aligarh Muslim University, Aligarh, India (l973).

3) I hold a Master of Science Degree in geophysics from University of Windsor, Windsor, Ontario (1982).

4) I have been practising my profession in Ontario since 1981.

5) I have been employed by the University of Windsor, MPH Consulting Ltd., Citadel Gold Mines, the Ontario Geological Survey, and am currently employed by Homestake Canada Inc. as a Project Geologist.

6) I am a member of the Sudbury Geological Discussion Group and Prospectors and Developers Association of Canada.

7) The information contained in this report and accompanying maps is based onpersonal observations and direct supervision of the field work, published data, and assessment data contained in the files of the Resident Geologist's Office, Thunder Bay.

8) I do not have directly or indirectly, nor do I expect to receive, any interest in the subject property.

Dated this 24th day of October, 1997 at Thunder Bay, Ontario

Ikram (Ike) A. Osmani, M. Se. (Geology), M. Se. (Geophysics). Project Geologist

23

Certificate of Qualifications

I, Zlatko Durdevic of 6990 David D'Angers, Montreal, Quebec, do hereby certify that:

1)1 hold a Bachelor of Science (specialization) degree in Geology (1997) from Concordia University, Montreal, Quebec.

2) I have been practising my profession in Ontario, Quebec, and the Northwest Territories since 1996.

3) I have worked for Concordia University and Phelps Dodge Corporation of Canada Ltd, and am currently employed by Homestake Canada Inc. as a geologist.

4) I do not have directly or indirectly, nor do I expect to receive any interest in the subject property.

Dated this 24th day of October, 1997 at Thunder Bay, Ontario.

Zlatko Durdevic, B.Se. (Geology) Geologist

24

Certificate of Qualifications

I, Allan D. MacTavish of 548 McMaster St., Thunder Bay, Ontario, do hereby certify that:

1.) I hold a Bachelor of Science (Honours) Degree in Geology (1977) from Laurentian University, Sudbury, Ontario.

2.) I hold a Master of Science Degree in Geology (1992) from Lakehead University, Thunder Bay, Ontario.

3.) I am a Fellow, in good standing, of the Geological Association of Canada.

4.) I have been practising my profession in Ontario, the Northwest Territories, and Manitoba since 1975.

5.) I have been employed directly by Noranda Exploration Company Limited,Canadian Superior Exploration Co. Ltd., Amax Minerals Inc., Kerr Addison Mines Ltd., St. Joe Canada Inc./Bond Gold Canada Inc./LAC Minerals Ltd., the Ontario Geological Survey, Falconbridge Limited, and am currently employed by Homestake Canada Inc. as a Senior Project Geologist.

6.) I hold no interest, directly or indirectly, in this property, nor do I expect to receive any interest or considerations from the same.

Dated this 24th day of October, 1997 at Thunder Bay, Ontario.

Allan D. MacTavish, M. Se. (Geology), FGAC Senior Project Geologist

25

References

Corfu, F. and Muir, T.L1989: The Hemlo-Heron Bay greenstone belt and the Hemlo Au-Mo deposit, Superior Province, Ontario, Canada: l. Sequence of igneous activity determined by zircon U-Pb geochronology; Chemical Geology, v.79, p. 183-200.

Debon, F. and Le Fort, P.1983: A Chemical-Mineralogical Classification of Common Plutonic Rocks and Associations; Transaction of the Royal Society of Edinburgh: Earth Sciences, v. 73, p. 135-149.

Heaman, L.M. and Machado, H.1987: Isotope Geochemistry of the Coldwell Alkaline Complex I - U-Pb studies on accessory minerals; in Program with Abstracts, Joint Annual Meeting, Geological Association of Canada - Mineralogical Association of Canada, v. 12, p. 54.

Irvine, T.N. and Baragar, W.R.A.1971: A Guide to the Chemical Classification of the Common Volcanic Rocks; Canadian Journal of Earth Sciences, v. 8, p. 523-548.

Jensen, L. S.1976: A New Cation Plot for Classifying Subalkalic Volcanic Rocks; Ontario Division of Mines, Miscellaneous Paper 66,22p.

Middlemost, Eric A.K.1985: Magmas and Magmatic Rocks, An Introduction to Igneous Petrology; Longman Group Limited, New York. 266p.

Mullen, E.D.1983: MnO7TiO27P2O5: Minor Element Discriminant for Basaltic Rocks of Oceanic Environment and its Implications for Petrogenesis; Earth and Planetary Science Letters, v. 62, p. 52-62.

Osmani, LA.1997: Geology and Mineral Potential: Greenwater Lake Area, West-Central Shebandowan Greenstone Belt, Ontario Geological Survey, Report 296, 135p.

Osmani, I.A., Samson, J. and MacTavish, AD.1997a: Geological Report on Rous Lake Property, Hemlo Area, Northern Ontario, Homestake Canada Inc., Unpublished Report.

26

Osmani, LA., MacTavish, A.D. and Samson, J.1997b: Ground Magnetic Survey Report, White Lake Property, White Lake Area (north part) Thunder Bay Mining Division, Ontario; Homestake Canada Inc., Unpublished Report, 16p.

Osmani, LA1996: Geology and Mineral potential of the Upper and Middle Shebandowan Lakes Area, West-central Shebandowan Greenstone Belt; Ontario Geological Survey, Open File Report 5938, 82p.

Osmani, LA.1991: Proterozoic Mafic Dike Swarms in the Superior Province of Ontario; in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part l, p.661-681.

Osmani, LA., Stott, G.M., Sanborn-Barrie, M., and Williams, H.R.1989: Recognition of Regional Shear zones in South-central and Northwestern Superior Province of Ontario and their Economic Significance; in Mineralization and Shear Zones, Editor: J.T. Bursnall, Geological Association of Canada, Short Course Notes, Volume 6, p. 199-218.

Rogers, M.C., Thurston, P.C., Fyon, J.A., Kelly, R.I. and Breaks, F.W.1995: Descriptive Mineral Deposit Models of Metallic and Industrial Deposit Types and Related Mineral Assessment Criteria; Ontario Geological Survey, Open File Report 5916, 241 p.

Rogers, M.C. and Berger, B.1994: Geology of Adrian, Marks, Sackville, Aldina and Duckworth townships, District of Thunder Bay; Ontario Geological Survey, Open File Report 5896, 102p.

Williams, H.R., Stott, G.M., Heather, K.B., Muir, T.L., and Sage, R.P.1991: Wawa Subprovince; in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part l, p.485-539.

27

Appendix l

Spruce Bay Property

1997 Sample Descriptions and Gold Analyses

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119005

SB119009

SB119013

SB119014

SB119015

SB119018

SB119019

SB1 19020

SB119021

SB119026

SB119027

SB119028

SB119029

SB119030

SB119031

SB119032

SB119033

SB119034

SB1 19035

SB119036

SB119037

SB119038

SB119039

LOCATION

L11+OOE, 16+60N

L12+15E, 16+05N

L23+10E, 14+35N

L22+90E, 14+75N

L23+OOE, 15+50N

L21+33E, 16+12N

L21+13E, 14+OON

L21+10E, 12+80N

L19+33E, 17+54N

L13+82E, 16+07N

L13+75E, 16+92N

L14+33E, 18+18N

L1S+OOE, 9+60N

L15+10E, 9+50N

L15+OOE, 8+92N

L15+OOE, 8+28N

L15+20E, 7+45N

L15+OOE, 7+23N

L15+OOE, 7+20N

L15+10E, 6+36N

L15+OOE, 5+77N

N of L15+OOE, island in lake

L12+OOE, 10+90N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whote Rock

Whole Rock

Whole Rock

Whote Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Whote Rock

Assay

Whole Rock

Assay

Whole Rock

Assay

DESCRIPTION

- fine grained mafic volcanic schist

- ultramafic metavolcanic schist, magnetic, weakly carbonatized, rusty on schistosity planes, fine-grained, highly schistose to sheared- wacke to siltstone, interbedded with ferruginous material [magnetite, chert ?]

- gabbro, coarse-grained, recrystallized/amphibolitized, N-S dominant trend of fractures and shears, epidote observed in some fractures (chiefly qtz 8* feldspar)- intermediate tuff to lapilli tuff, light grey on fresh surface, weathers whitish-grey

- mafic to intermediate volcanic schist (tuff to lapilli tuff?), silicified

- mafic pillowed flow, fine-grained, foliated to schistose, weakly silicified, carbonatized, epidotized

- peridotite, fine to medium-grained, greyish-green on fresh 8. weathered surfaces, moderately to highly magnetic, weakly serpentinized- silicified mafic metavolcanic schist, fine-grained, banded, foliated, grey on fresh surface, weathers greenish-grey

- mafic volcanic schist, fine-grained, greenish-black to dark grey on fresh surface, weathers grey, weakly silicified by qtz stringers along foliation planes- gabbro, strongly foliated to schistose, medium to coarse-grained

- gabbro, coarse-grained, foliated, ^ 'ft disseminated sulfides, minor qtz stringers

- wacke with minor mafic fragments, ^ "ft medium-grained pyrite

- mafic volcanic schist, silicified, carbonatized and contains numerous quartz-carbonate veinlets parallel to foliation, no visible sulphides- mafic flow with minor qtz vein fragments, massive, fine-grained, dark green on fresh 8, weathered surfaces, qtz veinlets emplaced along schistosity- mafic volcanic schist, qtz veinlets along foliation planes S, selvedges, rusty along qtz veinlets S foliation

- mafic volcanic schist, fine-grained, qtz+7-albite veinlets, massive to possibly pillowed

- monzodiorite to monzogabbro ?, medium-grained, weakly foliated

- mafic volcanic with 10*36 to semi-massive pyrite+Apyrrhotite

- wacke, schistose, rusty along schistosity planes, medium to dark grey on fresh surface, weathers greyish-white, finely bedded to laminated- banded chert-magnetite ironstone, strongly oxidized, no visible sulfides

- peridotite, coarse-grained, massive (some polygonal jointing), dark grey to black on fresh surface, weathers greyish-brown

- massive mafic flow, fine-grained, schistose, dark green on fresh surface, weathers greyish-green, numerous albite+qtz+carbonate strinoers and veinlets. ^ * sulfides

Auppb

*:1

•el

-:1

6

•el

8

10

4

6

2

1

2

2

"!1

19

6

2

1

4

6

16

1

1

Page 1 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119040

SB119041

SB119042

SB1 19043

SB119044

SB11904S

SB119046

SB119047

SB119048

SB119055

SB119058

SB119072

SB119073

SB1 19074

SB119075

SB119101

SB119102

SB119134

SB119135

SB119136

SB119137

SB119138

SB119143

LOCATION

L12+OOE, 1O45N

L12+OOE.8-I-32N

L12+OOE, 7+40N

L11*95E,6*60N

L11+90E.6+20N

L12*OOE,5*70N

L12*OOE,4*25N

L12+10E.3+40N

L12+OOE, 2+35N

L8+OOE, 18+35N

L7-KXJE, 18+10N

L2+50W, 13+50N

L2+50E, 13+50N

L1+25W, 13+40N

L2+QOW, 14+OON

L1+OOW, 13+52N

L1+15W, 14+53N

18+40E, 18+15N

L18+33E, 18+02N

L18+33E, 17+83N

15+32E, 17+O2N

L15+33E, 17+10N

L16+33E, 18+27N

SAMPLE TYPEAssay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whote Rock

Assay

Whole Rock

Whole Rock

Whote Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- highly rusty mafic volcanic, fine to medium-grained, strongly foliated to schistose, albite+qtz+carbonate stringers which contain -M* pyrite- mafic volcanic, fine-grained, massive, trace sulfides, knobby weathering

- mafic volcanic schist (possibly pillowed), fine-grained, dark grey on fresh surface, weathers brownish-grey, qtz stringers along fracture planes- quartz monzodiorite, medium-grained, massive, strongly lineated along fracture planes, pyrite cubes 8* carbonate occur along fracture planes- mafic to intermediate lapilli tuff, consists of highly flattened felsic +A mafic clasts which are set in an intermediate to mafic clastic matrix, carbonatized in places, trace sulfides- silicate facies ironstone, amphibote-rich, schistose, rusty, garnetiferous, contains disseminated and blebs of pyrite*pyhrrotite*Achalcopvrite- weakly silicified, +I- carbonatized mafic pillowed flow with biotite * some qtz veinlets within the selvedges

- ultramafic flow, fine to medium-grained, non-magnetic, massive, greenish-grey on fresh surface, weathers light brown, -d 'ft disseminated sulfides- felsic to intermediate lapilli tuff, no visible sulfides

- schistose gabbro, approx. 0.5m wide exposed shear zone, sheared gabbro is strongly silicified, sericitized and moderately to strongly carbonatized, minor quartz-albite veinlets, no visible sulphide mineralization- gabbro, coarse-grained, schistose, strongly lineated, amphibolrtized, no visible sulphides

- ultramafic to mafic (komatiitic) pillowed flow, weathers emerald green, greyish-green on fresh surface, soft and silky texture, minor quartz and epidote along fracture planes, no visible sulphides- ultramafic to mafic flow top breccia (komatiitic) 5 to 6 cm wide unit, quartz-feldspar stringers, other properties similar to WL119073- ultramafic to mafic (komatiitic) pillowed flow, fine-grained, weathers brownish-green, greyish-green on fresh surface, spinifex- textured, up to 5 cm long oltvine+A-pyroxene blades- massive mafic flow, fine-grained, weakly carbonatized, no visible sulphide mineralization

- fine-grained, dark green-grey on fresh surface, massive ultramafic volcanic

- fine-grained, strongly foliated/schistose, light grey-buff on fresh surface, aplite dike, muscovite on cleavage planes

- Mafic intrusive (schistose gabbro ?), SCflk hbld, plag and qtz, fine to medium-grained, trace to ] ah pyrite in blebs

- mafic to intermediate volcanic schist, strong banding, fine-grained, epidote alteration

- Mafic volcanic schist, fine-grained

- Gabbro, schistose, medium to coarse-grained

- Hornblende-garnet-quartz-biotite schist, fine-grained, 10*96 garnet, magnetic (silicate facies ironstone ?)

- Gabbro, locally schistose, coarse-grained

Auppb

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•si

*1

<1

5

8

5

<1

3

12

^

<1

<1

<1

^

<1

1

2

5

<1

1

2

2

Page 2 of 21

Appendix

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119144

SB1 19145

SB119146

SB119147

SB119148

SB119149

SB119150

SB119151

SB119152

SB119153

SB119154

SB119155

SB119156

SB119157

SB119168

SB119159

SB119160

SB119162

SB119163

SB119169

SB119170

SB119171

SB119172

LOCATION

L16+33E, 18+OON

L16+33E, 16+63N

L25+OOE, 10+OON

L23+26E, 9*85N

L16+OOE, 8+8ON

L15+96E, 8+60N

L15+97E, 8+45N

L15+80E, 8+45N

L15+8SE, 7+85N

L16+25E, 7+25N

L16+OOE, 4+90N

L15+96E, 4+72N

L16+O2E, 4+30N

L16*OOE,3*77N

L13+OOE, 16+52N

L13E+OO, 16+80N

L13+OOE, 18+26N

L10+OSE, 17+86N

L10+10E, 16+90N

L8+98E, 2+40N

L8+OOE, 7+02N

L8+OOE, 7+40N

L8+OOE, 8+23N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- intermediate lapilli tuff, banded, fine-grained

- Gabbro, fine to medium-grained, very weak foliation

- Granodiorite, weak foliation, trace fine pyrite, 2CHi biotite, 1CWfe hornblende, weakly magnetic, pinkish

- Granodiorite, biotite S hornblende aligned, coarse-grained, pinkish

- mafic lapilli tuff, very fine-grained, schistose, weak epidote alteration, few clasts

- Brecciated flow, mafic, epidote, clasts, remnant pillows?

- Brecciated flow, mafic, epidote, clasts, remnant pillows?

- intermediate tuff, fine-grained, banded (1 -3 cm wide)

- Mafic volcanic, fine-grained, moderate foliation, banded

- Mafic volcanic schist with pods, moderately to strongly foliated

- mafic volcanic

- Metawacke, 1 -2 cm banding

- ultramafic to mafic volcanic (pillows?), fine-grained, trace pyrite

- felsic volcanic, fine-grained, granular, weak epidote alteration

- Mafic volcanic, fine-grained, trace pyrite, weak foliation

- Hornblendite, medium to coarse-grained, locally foliated

- Hornblendite, medium to coarse-grained, locally foliated

- Hornblendite, medium to coarse-grained, locally foliated

- Mafic volcanic, fine-grained, schistose

- mafic to intermediate banded schist, trace to 5ft pyrite A pyrrhotite+ACpy, moderate epidote alteration

- Muscovite-epidote-biotite-quartz schist, ID-20% muse, 2-10* epidote in clots S. blebs, 1-3* biotite

- Mafic volcanic schist, fine-grained, weak epidote alteration 8, in cross-cutting veinlets, trace sulphides

- ultramafic metavolcanic schist, fine-grained, greenish-grey on weathered surface

Auppb

1

•el

2

2

1

1

4

3

4

3

3

2

3

1

1

1

2

5

4

7

1

4

•el

Page 3 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB1 19173

SB119174

SB119175

SB119176

SB1 19177

SB1 19178

SB119179

SB119180

SB119181

SB119182

SB119183

SB119184

SB1 19185

SB119186

SB119187

SB119188

SB1 19196

SB119197

SB119207

SB1 19208

SB119209

SB119210

SB119212

LOCATION

L8+OOE, 8+75N

L8+OOE, 8+85N

L7+50E, 9+OON

L7+50E, 9+25N

L7+97E, 6+40N

L7+96E, 6+40N

L7+31E, 11+80N

L7+03E, 11+30N

L7+03E, 1H-30N

L7+03E, 11+OON

L6+91E, 10+23N

L7+OOE, 8+33N

L6+79E, 8+33N

L6+40, TL7+OON

L6+OOE, 8+70N

L5+96E, 1H75N

L6+75E, 14+80N

L6+75E, 14+80N

L1+OOW, 11+87N

LO+96W, 12+65N

LO*85W, 13+15N

L2+OOW, 13+15N

L2+90W, 10+37N

SAMPLE TYPE

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- altered ultramafic flow?, talc schist, possible molybdenite (3*)fe), trace pyrite

- Mafic volcanic schist, fine-grained

- Highly altered tremolite-muscovite schist of probable ultramafic metavolcanic protolith, rusty, strong foliation

- Granodiorite, coarse to medium-grained, plag phyric (2-5mm), ~10*Xi biotite, very weak foliation

- diabase dike, medium to coarse-grained, unfoliated, trace pyrite

- intermediate schist (tuff ?), very fine-grained, unfoliated, S-15% epidote clots, 1-5"* pyrite, locally rusty

- serpentine-tremolite*7-carbonate schist, shear zone, rusty along shear planes, ^ % disseminated, very fine-grained sulfides

- brown-green, rusty ultramafic schist (flow breccia), soft, no visible sulfides

- dark green to black ultramafic fragment from flow breccia ?, highly altered, dense, soft, rusty, no visible sulfides

- altered ultramafic or mafic intrusion ?, moderately oxidized, very fine-grained disseminated 8, chunks of pyrite, minor bornite, ^-chalcopyrite, magnetic, fine to medium-grained- ultramafic volcanic, massive and pillowed flow, fine-grained, weathers dark grey, dark green on fresh surface, weakly foliated

- ultramafic to mafic volcanic, rusty, massive A pillowed flow,

- altered ultramafic intrusion/flow ?, fibrous, rusty, no visible sulfides

- Intermediate tuff with abundant qtz stringers, no visible sulfides

- massive to pillowed ultramafic schist, fine-grained, weathers grey-green, light green on fresh surface

- ultramafic pillowed flow

- massive, weakly altered mafic volcanic flow, fine-grained, strongly foliated

- feldspar porphyry, ,25-.5m wide, 2-3mm phenos of feldspar ( 20-40* )

- mafic pillowed flow, strongly foliated to schistose, very fine-grained, minor qtz stringers, grayish black on fresh surface, weathers grey- ultramafic flow, fine-grained, slightly spinifex texture and schistose, weathers emerald green-grayish, dark green on fresh surface- peridotite, fine-grained, massive,

- qtz monzodiorite to granodiorite, massive, medium to coarse-grained, weathers white to beige, hW+bio+felds (plag - k- spar?)*qtz- mafic volcanic schist, fine-grained, moderately silicified

Auppb

4

1

*!1

<1

<1

1

1

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5

4

3

6

4

•:1

3

3

2

•:1

<1

2

•et

<1

75

Page 4 of 21

Appendix l

SAMPLE NUMBERSB119213

SB119214

SB119215

SB119216

SB119217

SB119218

SB119219

SB119220

SB119221

SB119222

SB119223

SB1 19224

SB119225

SB1 19226

SB119227

SB1 19232

SB1 19233

SB1 19234

SB1 19235

SB119236

SB119237

SB1 19238

SB119239

LOCATION

L3+OOW, 11+10N

L3+OOW, 11+25N

L2+98E, 11+75N

L3+OOW, 12+76N

L3+OOW, 13+36N

L2+COW, 11+50N

L2+OOW, 11+65N

L1+75W, 11+20N

L1+65W, 11+15N

L1+60W, 11+20N

L1+50W, 11+30N

L1+45W, 11+36N

L1+35W, 11+30N

L3+OJW, 14+25N

L2+92W, 14+36N

L10+35E, 7+OON

L10+02E, 6*96N

L10+OOE, 5+OON

L10+OOE, 5+OON

L7+90E, 11+55N

L10+OOE, 5+80N

L7+90E, 11+10N

L8+OOE, 1H-10N

SAMPLE TYPE

Whole Rock

Whole Rock

Assay

Whole Rock

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Spruce Bay Property: 1997 Sample Descriptions

DESCRIPTION

- mafic volcanic, fine-grained, strongly foliated

- possibly ultramafic or high MgO basalt, fine-grained, weathers emerald green

- mafic volcanic, fine-grained, light grey on fresh surface, silicified, ^ 'to pyrite

- mafic volcanic, fine-grained, massive, light grey on fresh surface

- ultramafic flow, fine-grained, massive, foliated to schistose

- silicified mafic volcanic, up to 2* pyrite

- mafic volcanic, fine-grained, rusty, up to 5*96 disseminated pyrite

- silicified mafic volcanic -i- qtz vein, trace sulfides

- silicified mafic volcanic with qtz vein * qtz-alb stringers, up to It?*, pyrite as chunks and disseminated

- silicified rusty mafic volcanic with qtz vein, <1 % pyrite

- rusty, siliceous, metasediment ?, trace sulfides

- siliceous/cherty - metasediment, rusty, 2-5% fine-grained sulfides

- rusty mafic volcanic schist with minor qtz veinlets, 1 'to disseminated pyrite

- spinifex-textured ultramafic to mafic flow (komatiite), massive to weak foliation, greenish-black on fresh surface, weathers grey green, qtz stringers along fractures- ultramafic volcanic, pillowed ?, highly silicified * oxidized (gossan), ^ to 2% disseminated sulfides

- banded mafic schist, fine to medium-grained, amphibole rich, thin plag rich bands, disseminated 1 'K pyrite+Apyrrhotite

- intermediate tuff to lapilli tuff, intercalated/interbedded with mafic schist ( pillow * tuff) and wacke, grey on fresh surface, weathers white-brown, strongly foliated,- polymictic conglomerate, mafic matrix, at least 2 types of felsic clasts, minor mafic clasts, clasts range from lapilli to bomb size, ovoid to subangular, moderately to highly flattened- monzodiorite dike, hombtende-phyric

- serpentine-tremolite-carbonate*Malc schist (massive flow to flow breccia), highly sheared, trace sulfides within narrow shears

- mafic volcanic schist & feldspar porphyry dike fragment

- serp-tremolrte-carb schist (massive to spinifex), fine-grained, highly sheared

- ultramafic to mafic schist, friable, rusty, ^ % sulfides along shear planes

Auppb

4

1

1

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<1

2

<1

5

12

2

3

14

•O

1

4

1

5

•:1

1

4

2

10

Page 5 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB1 19240

SB119241

SB119242

SB119243

SB119244

SB119245

SB119246

SB119247

SB119248

SB119249

SB119250

SB119278

SB119279

SB119280

SB119281

SB1 19282

SB119283

SB119284

SB119285

SB119286

SB119287

SB119288

SB119289

LOCATION

L8+OOE, 1O90N

L8+06E, 1O80N

L8+05E, 1CH75N

L8+OOE, 1O70N

L8+OOE, 1O60N

L7+80E, 8+96N

L8+35E, 9+05N

L8+30E, 8+60N

L7+65E, 9+OON

L7+80E, 8+96N

L7+OOE, 11+78N

L28+OOE, 18+75N

L28+OOE, 18+75N

L27+OOE, 19+15N

L26+OOE, 17+10N

L24+90E, 18+70N

L25+20E, 18+25N

L24+75E, 15+eON

L24+75E, 15+60N

L25+OOE, 14+75N

L24+05E, 14+50N

L23+80E, 15+75N

L23+95E, 16+78N

SAMPLE TYPEAssay

Assay

Assay

Assay

Assay

Whole Rock

Assay

Assay

Assay

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- altered ultramafic extrusive/intrusive contact zone (gossanous), mineralized with a-3% pyrite*bornrte*7-chalcopyritet/- sphaterite , pyrite occurs disseminated, bornite ^/-chalcopyrite occurs as chunks- similar to SB1 19240 - same zone

- sheared, very rusty, silicified metasediments, fine-grained, very fine-grained trace disseminated sultides

- qtz vein t host rock (altered mafic 1 intermediate), within 1 m wide shear zone, qtz vein is irregular, 2-3'fc disseminated moly+pyrite, minor bomite+sphalerite+pvrrhotite- ultramafic intrusion (1 .5m wide) along the sheared contact with the altered mafic/intermediate volcanic, highly oxidized and silicified, shear zone is .5-.75m wide (anastomosing shears), 2-396 disseminated very fine-grained sulfides- mafic volcanic, fine-grained, massive to pillowed ? flow, strongly foliated, qtz stringers

- gossan zone within altered mafic metavolcanic, highly oxidized, *1 % disseminated pyrite-i-bomite*7-sphalerite, weakly to strongly magnetic- mafic volcanic, fine-grained, massive to pillowed ? flow, strongly foliated to schistose, qtz stringers, trace sulfides

- magnetite ironstone, intercalated with siltstone, 2-5"* pyrtte*bomite*Achalcopyrite*;-sphalerite, occurs disseminated, as chunks 8* massive blebs- intermediate to felsic hypabyssal intrusive, fine-grained to aphanitic, contains 2-3*ft very fine-grained sulphides

- qtz-carb vein within ultramafic schist (serpentine-tremolite-carb 7), trace to no sulfides

- Pillowed mafic flow, moderately altered Z foliated

- diorite dike wtthin mafic flow

- Moderately to strongly foliated, medium to coarse-grained, micaceous, mafic schist

- Moderately foliated, micaceous mafic schist

- Fine to medium-grained, micaceous, moderately to strongly foliated, banded mafic schist

- Banded, medium-grained, micaceous mafic schist

- Moderately foliated, gabbro

- monzodiorite, trace pyrite wtthin minor quartz veining

- intermediate to felsic intrusive (granodiorite), xenolithic

- mafic schist, fine to medium-grained, muscovite bearing, fine quartz veinlets randomly orientated

- Moderately to strongly foliated, mafic lapilli tuff, lapilli sized clasts are muscovite rich and mafic in composition

- Steel blue coloured, muscovite rich, strongly foliated, mafic (and intermixed sedimentary?) schist

Auppb

16

1

7

1

1

2

2

1

10

6

•el

•M

^

•ei

2

•!1

2

3

1

8

1

1

2

Page 6 of 21

Appendix l

SAMPLE NUMBERSB119290

SB119291

SB1 19292

SB119293

SB119294

SB119295

SB119296

SB119297

SB119298

SB119299

SB119300

SB119301

SB1 19302

SB119303

SB119312

SB119313

SB119314

SB119315

SB119316

SB119317

SB119318

SB119319

SB119320

LOCATION

L24+10, 18+OON

L23+90E, 18+60N

L23+96E, 19+25N

L22+OOE, 18+OON

L22+OOE, 18+OON

L22+OOE, 16+75N

L22+OOE, 16+55N

L22+20E, 16+15N

L22+25E, 14+75N

L22+OOE, 13+30N

L20+28E, 15+30N

L20+28E, 15+30N

L20+43E, 16+10N

L20+23E, 17+50N

L17+33E, 18+60N

L17+33E, 18+55N

L17+33E, 18+55N

L17+10E, 17+90N

L17+28E, 16+77N

L17+33E, 14+O5N

L17+43E, 13+10N

L17+28E, 12+60N

L18+85E, 6+15N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Spruce Bay Property: 1997 Sample DescriptionsDESCRIPTION

- Green-grey, fine to medium-grained, moderately foliated mafic schist

- coarse-grained, non-magnetic, moderately to strongly foliated gabbro with quartz clots

- Fine to medium-grained, muscovite rich, moderately foliated, banded mafic schist

- fine-grained, strongly foliated, mafic flow, thick quartz veins parallel to foliation

- Light yellow-tan, felsite dike/sill parallel to foliation within mafic schist, moderately foliated, amphiboles aligned with foliation

- fine-grained mafic flow to coarse-grained gabbro or coarse mafic flow, non-magnetic

- Grey to green-grey, intermediate tuff to crystal lapilli tuff

- Medium green, coarse-grained, moderately foliated gabbro

- Medium green, coarse-grained, foliated gabbro

- Steel grey to creamy white, mafic to intermediate lapilli tuff, well developed foliation

- Green, muscovite rich, moderately foliated, banded, mafic schist

- medium-grained, moderately foliated, hornblende phyric dtorite/gabbro, hornblende crystals parallel to foliation, pyrite specks disseminated throughout- mafic volcanic schist, non-magnetic, moderately foliated, banded

- Green-grey, moderately foliated, mafic volcanic schist, fragmental texture, altered

- Diabase dike, unfoliated, ophitic texture, magnetic

- Fine to medium-grained, unfoliated, massive, dark grey, non-magnetic, diabase chilled margin

- Light to medium green, moderately foliated, silicified, fine to medium-grained mafic (and sedimentary?) schist,

- Banded light to dark green, intermediate tuff, moderate foliation

- Medium to coarse-grained, ophitic, magnetic diabase dike

- coarse-grained, green grey, very weakly foliated peridotite

- Dark grey green, coarse-grained, massive peridotite

- Dark grey green, coarse-grained, massive peridotite

- fine-grained, possibly pillowed, foliated, mafic schist

Auppb

•el

•tt

*:1

•0

•el

1

9

6

4

4

2

1

1

1

2

3

2

1

2

3

6

7

3

Page 7 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB1 19321

SB1 19322

SB1 19323

SB1 19324

SB119326

SB1 19326

SB1 19327

SB1 19328

SB119329

SB1 19330

SB1 19331

SB1 19332

SB1 19333

SB119334

SB1 19335

SB1 19336

SB1 19337

SB1 19338

SB119339

SB1 19340

SB119341

SB1 19342

SB119343

LOCATION

L18+75E, 6+ODN

L18+OOE, 7+25N

L18+OOE, 6+OON

L16+85E.5+23N

L17*OOE,5*63N

L16*97E,5*80N

L17+OOE.6+50N

L16+9BE.8+50N

L14+05, 10+05N

L14+OOE.9+45N

L14+10E.8+88N

L13*75E,8*2SN

L13+75E, 7+25N

L13+95E, 6+05N

L14+OOE.4+75N

L13+OOE, 1O50N

L13*10E,9*85N

L13+OOE.9+OON

L12*90E,8*50N

L12+93E.8+O8N

L13+40E, 7+OON

L13+OOE, 6+77N

L13+OOE, 5+69N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- GranodioriteAonalite, weakly foliated, intruding mafic schist, fine to medium-grained-chilled margin

- fine-grained, dark green, mafic schist, silicified, possible pillow selvedges or interflow sediments

- fine-grained mafic schist, moderately foliated, bands of metasediments and granitoid intrusives

- fine-grained, strongly foliated, green-grey, mafic metavolcanic

- Green-blue, coarse-grained, olivine phyric, moderately foliated, non-magnetic gabbro

- strongly foliated diorite to gabbro, hornblende phyric

- Fine to medium-grained, moderate green grey, fragmental mafic flow, with interflow sediments

- fine-grained, moderately foliated mafic metavolcanic, pillowed or fragmental

- Mafic volcanic schist (fragmental) containing 5-1 Ocm long mafic fragments flattened by foliation, weakly magnetic ironstone layers- mafic volcanic schist with qtz-stringers or granitic fragments

- Green, fine to medium-grained, foliated, mafic metavolcanic

- Fine to medium-grained, mafic flow with intercalated sediments?, moderate foliation

- mafic volcanic schist

- Green grey, fine to medium-grained, moderately foliated mafic metavolcanic

- Green grey, fine to medium-grained, moderately foliated mafic to ultramafic metavolcanic

- Blue-grey, fine-grained, Moderately foliated, aphyric mafic metavolcanic

- Grey-green, fine to medium-grained, moderately foliated mafic flow

- Foliated flow or banded mafic metavolcanic, light and dark blue green colour, strongly foliated 8, boudinaged

- 20cm wide rusty zone parallel to foliation in mafic metavolcanic rock, purple hematitic zone on the margin of the thicker limonitic zone, strong shearing, grey quartz vetoing, no sulphides- fine-grained, moderately foliated, muscovite rich, mafic metavolcanic

- Mafic volcanic schist, micaceous interiayers of sedimentary or intermediate lapilli tuff units

- Fine to medium-grained, moderately foliated mafic flow with either interflow sediments or pillow selvedges

- Light steel grey, fine to medium-grained, mafic volcanic schist

Auppb

2

2

5

4

2

1.5

4

3

1

1

4

1

2

2

6

10

8

1

2

1

1

1

2

Page 8 of 21

Appendix t

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119344

SB11934S

SB119346

SB119347

SB1 19348

SB119349

SB119350

SB119351

SB119352

SB1 19363

SB119354

SB119355

SB119356

SB1 19357

SB119358

SB119359

SB1 19360

SB119361

SB119362

SB119363

SB119364

SB11936S

SB119366

LOCATION

L13+COE, 4+93N

L13+OOE, 4+60N

L11+O5E, 11+20N

L11+30E, 11+15N

L11+15E, 10+75N

L10+90E, 10+45N

L11+50E, 11+OON

L11+15E, 10+O5N

L10+95E, 9+1 2N

L11+15E, 8+15N

L11+06E, 7+40N

L11+06E, 7+40N

L10+90E, 6+90N

L11+OOE, 6+07N

L11+12E, 4+90N

L11+OOE, 4+25N

L11+OOE.3+70N

L11+15E.3+OON

L4+S6E.11+80N

L5+OOE, 11+50N

L4+85E, 11+20N

L4+85E, 11+20N

L5+OOE, 10+77N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

DESCRIPTION

- Fine to medium-grained, moderately foliated, micaceous mafic volcanic schist, pillow selvedges?

- Intermediate lapilli tuff to sediment, black lapilli up to 4cm long, pale grey fine micaceous matrix

- diabase dike, medium-grained, ophitic texture, massive, magnetic

- mafic metavolcanic, weakly to moderately foliated to schistose

- mafic to ultramafic volcanic schist (pillows ?), fine-grained, weakly carbonated

- altered ultramafic intrusion, medium to coarse-grained, light blue-green, weakly magnetic, soft

- brecciated (primary or tectonic) mafic metavolcanic schist, epidotized fragments

- mafic volcanic schist, moderately foliated, fine-grained, light green-grey

- mafic volcanic flow, moderately foliated, blue-grey to green-grey, green-tan coloured fine-grained felsic clasts (10cm long)

-similar to SB1 19352

- mafic volcanic schist? with intercalated sediments?, fine-grained, moderately to weakly foliated, gritty/sugary texture, rusty, green A purple-brown- band/dike/sill of rusty yellow colour, medium to coarse-grained granular biotite+quartz porphyry,

- intermediate to mafic crystal tuff, fine-grained, moderately foliated, micaceous, light green-grey

- mafic metavolcanic, fine-grained, moderately foliated, blue-green in colour, silicified

- mafic to intermediate volcanic (tuff to crystal tuff ?), banded, fine to medium-grained, moderately foliated, green to light tan in colour, k-feldspar rich patches- qtz porphyry, coarse-grained, granitoid intrusive ?, slightly rusty on weathered surface, very weakly foliated to massive

- ultramafic intrusive/Mow ?, strongly magnetic, fine to medium-grained, moderately foliated, light blue-green colour

- mafic volcanic schist, banded, fine-grained, moderately foliated, dark to medium green in colour

- ultramafic to mafic schist, fine to medium-grained, weathers dark greenish-beige, dark grey on fresh surface, massive appearance, trace sulfides- spinifex textured ultramafic flow, fine-grained, weathers dark beige-green, grey on fresh, trace sulfides, possibly pillowed, qtz- alb stringers- rusty ultramafic volcanic schist, fine-grained, magnetic, dark grey on fresh surface, trace sulfides

- spinifex textured ultramafic flow, fine to medium-grained, greyish-black on fresh surface, weathers greenish-light brown, talc- bearing- mafic volcanic schist, fine-grained, grey on fresh surface, weathers greyish-black, strongly foliated to schistose, silicified

Auppb

3

2

1

3

4

3

7.5

3

6

5

•el

1

•:1

•:1

•:1

^

•el

^

1

•:1

•*1

*1

•*1

Page 9 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB1 19367

SB1 19368

SB1 19369

SB1 19370

SB1 19389

SB1 19392

SB119394

SB1 19395

SB1 19396

SB119397

SB1 19398

SB1 19399

SB119400

SB119412

SB119416

SB119425

SB118426

SB119427

SB1 19428

SB1 19429

SB119430

SB1 19431

SB1 19432

LOCATION

L5+OOE, 10+04N

L5+05E, 8+80N

L5+OOE, 8+30N

L5+OOE, 7+65N

LO+02W, 7+45N

L2+OOW, 7+37N

L9+OOW, 2+15N

L9+OOW, 1+50N

L1+04W, 6+79N

UH70W,5*50N

L1+OOW.3+90N

L1+05W, 2+95N

LI+OOW.O+SON

L4+06W, 14+30N

L4+OOW, 11+65N

L6+80E.6+90N

L6+99E, 5+96N

L7+OOE, 6+20N

L6+85E, 5+40N

L7+83E, 4+40N

L7+01 E, 3+45N

L8+ODE, 5+49N

L8+OOE, 4*10N

SAMPLE TYPE

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- mafic to ultramafic metavolcanic, fine-grained, foliated, black on fresh surface , weathers dark green-grey, schistose appearance on fresh surface, no visible sulfides- mafic volcanic schist, rusty-beige on weathered surface, siliceous, appears finely laminated, qtz stringers/veinlets along foliation planes- mafic metavolcanic, fine-grained, massive, silicified, weathers dark grey-brown, grey on fresh surface, no visible sulfides

- mafic metavolcanic, massive to slightly foliated, silicified - qtz veins/stringers, fine-grained, dark grey-green on fresh surface, weathers grayish white- mafic metavdcanics, massive, fine-grained, small rusty zones, grey on the fresh surface, trace very fine-grained sulfides

- mafic metavotcanic, foliated, grey-green on the fresh surface, weathers light S, dark grey, silicified - qtz veins/stringers along foliation planes, non-magnetic- mafic metavolcanic, dark green-black on the weathered surface, grey on fresh, fine-grained, no visible sulfides, foliated

-same as SB1 19394

- diorite to gabbro, fine to medium-grained, schistose, grey-black on fresh surface, weathers brownish-black, contains plag-hbl- bio- mafic (pillowed 7) volcanic, fine-grained, schistose, soft, grey on the fresh surface, weathers greenish-brown, trace sulfides

- mafic metavdcanics, deformed pillows, fine-grained, silicified, foliated, schistose, dark grey on the fresh surface, weathers greenish black- mafic flow, massive, aphanitic to fine-grained, grey on fresh surface, weathers black

- massive mafic metavolcanic, fine-grained, silicified, small rusty areas/spots, grey on the fresh surface, weathers greyish- white, trace sulfides- ultramafic to mafic flow, massive, fine-grained, non-magnetic, weathers emerald green, dark grey-green on fresh surface, weakly to moderately foliated, rusty patches along foliation S fracture planes- massive mafic volcanic St derived schist, fine-grained, moderately silicified, albite stringers, no visible sulfides

- mafic lapilli tuff , intermediate to felsic clasts in a mafic volcaniclastic matrix, clasts are generally lapilli size

- mafic volcanic (amphibolitized), weathers rusty brown, greyish-black on fresh surface, very fine-grained to aphanitic, S-4% medium-grained disseminated pyrite, may contain garnet -i- epidote along fractures- mafic schist, beige on weathered surface, grey on fresh surface, l -ZK disseminated pyrite

- mafic lapilli tuff Z derived schist, highly flattened felsic (pink to beige) and minor mafic clasts set in a mafic matrix, calc- silicate layers * epidote (mm to cm scale), up to A1*) disseminated pyrite * stringers- highly silicified mafic metavolcanic ?, fine-grained, strongly oxidized, 2-316 disseminated fine-grained pyrite cubes

- intermediate to felsic feldspar porphyry, emplaced concordantty to mafic metavolcanic layering/foliation, highly deformed, trace pyrite- muscovite-biotite-feldspar-qtz schist (felsic to intermediate tuff ?), fine-grained, bedded, rusty on cleaved (bedding) surfaces, trace sulfides- highly altered intermediate tuff/lapilli tuff ?, strongly foliated, muscovite, weathered surface is strongly rusty to grey, light grey on fresh surface. 2-3")t disseminated sulfides

Auppb

2

18

9

7

6

*:1

1

10

1

•:1

1

9

1

3

5

2

6

•el

•d

1

5

2

3

Page 10 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119433

SB119434

SB119435

SB119436

SB119437

SB119438

SB119439

SB1 19440

SB119441

SB119442

SB119443

SB1 19444

SB119445

SB11944S

SB1 19447

SB1 19448

SB119449

SB1 19450

SB1 19461

SB119452

SB1 19453

SB1 19454

SB119455

LOCATION

L8+OOE.3+06N

L7+90E, 2+50N

L4+OOE.4+05S

L4+OOE, 1+OOS

L4+03E, 1+90S

L5+OOE, 1+82S

L5+Q2E.3+03S

L5+OOE, 1+OON

L4+97E, 2+63N

L5+OOE, 2+96N

L4+S6E, 4+1 2N

L5+06E, TL7+OON

L3+OOE, 6+05N

L3+OOE.4+50N

L3+OOE, 4+07N

L3+COE, 2+95N

L3+OOE, 0+24N

L3+OOE.2+96S

L5+80E, 6+40N

L5+SOE, 6+20N

L6*OOE,5*OON

L6+OOE, 4+12.5N

L6+10E, 2+10N

SAMPLE TYPEAssay

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- highly oxidized ultramafic flow (pillowed ?), no visible sulfides

- mafic to ultramafic conglomerate, mafic * ultramafic * felsic clasts set in a mafic to ultramafic matrix, .5m oxidized zone, 1- 2'* sulfides- intermediate lapilli tuff, felsic lapilli clasts are set in a biotite-feldspar-qtz matrix, clasts are ovoid to ribbon-shaped

- felsic lapilli tuff, felsic clasts and matrix are both qtz-feldspar phyric, weathers beige-white, light grey on fresh surface

- mafic metavolcanic, fine-grained, amphibolitized, foliated to schistose, rusty, trace pyrite

- felsic lapilli tuff, intensely flooded by hematite along clast boundaries 8, fractures

- felsic to intermediate lapilli tuff, small highly oxidized zone (chunks * disseminated pyrite - 2%)

- mafic pillowed flow, fine-grained, amphibolitized, pillows are strongly deformed, greyish-black on fresh surface, small highly oxidized zone (gossan - up to Sib disseminated, Webs, and chunks of pyrite)- mafic metavolcanic (garnetiferous pillow breccia or lapilli tuff ?), fine to medium-grained, amphibolite schist, moderately silicified, trace sulfides- ultramafic to mafic conglomerate, epidotized, felsic lapilli clasts set in a serpentinized ultramafic matrix, clasts are subangular to rounded and range in size from 2mm to 6cm, ultramafic matrix is silicified 8, strongly carbonatized- ultramafic flow, polysutured, fine-grained, soft on weathered surface (talcose) 4 rusty, grey-green on fresh surface, minor qtz stringers- mafic pillowed flow (high MgO basalt), fine-grained, silicified, moderate qtz-alb stringers Z veinlets, strongly foliated to schistose, no visible sulfides- intermediate to felsic tuff to lapilli tuff, light grayish beige-white on the fresh surface, weathers rusty beige, fine-grained matrix, rare lapilli size clasts of darker color are set in a light grey to beige matrix- polymictic conglomerate, mafic S felsic clasts (elliptical to rounded), matrix is intermediate to mafic St siliceous, qtz stringers/veintets parallel to foliation- ultramafic flow, fine-grained, schistose, intensely carbonatized 8, silicified, no visible sulfides

- Similar to SB1 19446 but oxidized

- mafic (pillowed ?) flow, garnet-bearing, fine-grained, foliated, amphibolitized, dark green-black on the fresh surface, weathers rusty color on surface S along foliation, moderate qtz stringers- intermediate lapilli tuff, light grey on the fresh surface, weathers rusty color, hornblende-bearing

- mafic metavolcanic, flow-top breccia, vesicular, variolitic, dark grey-green, micro-pillows, pillow breccia, trace sulphide

- massive to pillowed mafic metavolcanic, numerous quartz stringers, tension gashes parallel to foliation

- mafic schist, platy alignment of amphiboles parallel to schistosity, trace pyrite

- intermediate (andesite), fine to medium-grained, massive texture, t-2% disseminated pyrite, muscovite on Joint surfaces, rusted oxidized surface- silicified mafic to intermediate flow, T-2% disseminated pyrite

Auppb

•el

3

1

•d

^

•el

1

2

2

4

14

1

1

1

•el

•:1

1

*:1

•:1

2

4

4

•el

Page 11 of 21

Appendix

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119466

SB1194S7

SB119458

SB119459

SB119460

SB119461

SB119462

SB119463

SB119464

SB119465

SB119466

SB119467

SB119468

SB119469

SB1 19470

SB119471

SB119472

SB119473

SB119474

SB119475

SB119476

SB119477

SB119478

LOCATION

L6+OOE, 1+50N

L6+OOE, 1+30N

L7+OOE, 1+25N

L7+OOE, 0+37S

L6+OOE, 1+OOS

L4+25E, BLO

L4+OOE, 2+87N

L4K30E, 6+60N

L3+90E, 6+OON

L4+OOE, 3+75N

L2+50E.4+50N

L2+OOE, 2+50N

L2+OOE.3+50S

L2+OOE, 1+25N

L2+OOE, BLO

L2+OOE.4K10N

LO+00, 3+25S

LO+00, 1+37N

LO+00, 7+OON

LO+00, 6+25N

LOHOW, 5+50N

LO+13E.5+OON

LO+00, 2+50N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

DESCRIPTION

- feldspar porphyry, siliceous, massive, trace sulphides

- mafic metavolcanic, fine-grained, dark grey to black, massive, numerous quartz-epidote stringers oblique to fabric, rusted/oxidized staining, 1-21* disseminated pyrite- feldspar-phyric felsic metavolcanic, trace sulphide

- quartz-crystal tuff, fine-grained, massive, siliceous rhyolitic protolith with gneissic metamorphism, rusted/oxidized joint surfaces, slightly potassic and sericitic alteration, 0.5-1 "56 finely disseminated pyrite- feldspar-phyric crystal tuff, rhyolitic protolith metamorphosed to gneissic texture, orthoclase and albite rich, trace sulphide

- amphibolitized mafic metavolcanic, fine-grained, aphanitic with platy alignment of amphibole crystals parallel to fabric, unit possesses oxidized/rusted weathering and slightly contorted feldspar dikes parallel to fabric- mafic volcanic schist, rusted jointed surfaces and bedding planes, 1 -2*K finely disseminated pyrite

- mafic volcanic schist, fine to medium-grained, dark grey, oxidized and hematitic alteration on bedding planes, trace pyrite

- Tine to medium-grained, amphibolitized mafic volcanic schist

- ultramafic massive How, dark grey-green, fine-grained, aphanitic, massive, trace sulphide

- polymictic conglomerate, felsic and cherty dasts, granodiorite and diorite ellipsoid clasts up to 15 cm in length stretched parallel to fabric within a fine-grained mafic to intermediate matrix, trace sulphide- amphibolitized medium-grained mafic volcanic, dark grey to black, trace sulphide

- amphibolitized medium-grained mafic volcanic, dark grey to black, trace sulphide

- mafic metavolcanic

- highly altered mafic volcanic, fine-grained, rusted, oxidized bedding surfaces, trace pyrite

- medium-grained diorite, trace sulphide

- intermediate to felsic, siliceous, feldspar-phyric, trace pyrite

- mafic metavolcanic, fine-grained, light grey, oxidized surface, trace sulphide

- intermediate to mafic tuff, fine-grained siliceous, light grey, rusted oxidized weathered surfaces, 1 -2'* finely disseminated pyrite- mafic metavolcanic, massive to tuffaceous, oxidized weathered surface, 2-3'ft disseminated pyrite

- intermediate to felsic lapilli tuff, feldspar-phyric, siliceous, massive gneissic layers in contact with diabase, trace pyrite

- intermediate tuff, siliceous with scattered biotite-amphibole flakes oriented parallel to fabric, 1-21* finely disseminated pyrite

- barren milky white quartz vein hosted within serpentinized komatiitic ultramafic flow, flow is massive but possesses remnant Dorvsuturina. trace sulphides

Auppb

•:1

g•el

1

•el

•el

2

•M

1

•el

1

2

3

1

2

1

7

1

1

2

*1

^

1

Page 12 of 21

Appendix

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB119479

SB1 19480

SB119481

SB119482

SB1 19483

SB119484

SB1 19485

SB1 19486

SB119487

SB1 19488

SB1 19489

SB1 19490

SB1 19496

SB119497

SB1 19498

SB1 19499

SB119600

SB85001

SB86002

SB86003

SB85004

SB85005

SB85006

LOCATION

L1+OOE, 1+OOS

L1+50W, 7+OON

L2+OOW, 7+OON

L1+90W.5+85N

L2+OOW.5+25N

L2+50W, 7+OON

L3+OOW.6+50N

L8+OOW, BLO

L8+OOW.O+13N

LB+OOW.O+SON

L8+10W, 4+75N

L8+10W, 5+25N

L6+-25W, 1+50N

L6+OOW, 2+50N

L6+10W, 3+25N

L6+OOW.3+75N

L6+ODW, 4+25N

L1+OOW.O+25S

L1+OOW, 1+OOS

L13+97W, BLO

L10+OOW, 2+15N

L10+ODW, 2+85N

L10+OOW, 4+35N

SAMPLE TYPE

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whote Rock

Whole Rock

Whote Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whote Rock

Whole Rock

Whote Rock

Whole Rock

DESCRIPTION

- felsic lapilli tuff, protolith rhyolitic with gneissic grade metamorphism, quartz-phyric, trace sulphide

- intermediate to mafic dike (lamprophyre ?), coarse-grained, hombtende-phyric, hornblende aligned parallel to fabric, fine grained groundmass comprised of interstitial plagioclase-pyroxene, trace sulphides- maHc flow, fine-grained, moderately foliated, light green, slightly talcose, possible flow-top breccia and hyaloclastite, trace sulphide- altered mafic metavolcanic, fine-grained, aphanitic, moderately foliated, light green, massive, trace sulphide, oxidized weathered surfaces- gossan stained and hematitic quartz vein within oxidized rusted and hematite intermediate or altered mafic ? volcanic, no sulphide noted but strong potassic and hematitic alteration- intermediate crystal lapilli tuff or conglomerate, unit strongly metamorphosed with segregated mafic and felsic lapilli clasts stretched parallel to fabric, fine-grained and recrystallized matrix- polymictic conglomerate, clasts of varying composition, dioritic to mafic and ellipsoid stretched parallel to fabric, numerous feldspar porphyry dikes, trace sulphide- gneissic, intermediate lapilli tuff, strongly folded, intruded by feldspar porphyry dikes, trace pyrite

- mafic metavolcanic, dark grey to black, fine-grained, aphanitic, oxidized, hematitic weathered surface, massive, trace pyrite

- amphibolitized massive mafic metavolcanic, oxidized surface, trace pyrite

- felsic metavolcanic, tuffaceous, extremely siliceous, quartz-phyric, trace pyrite

- polymictic amphibolitized conglomerate with felsic, granodiorite and mafic clasts stretched parallel to fabric, oxidized surfaces, trace pyrite- mafic metavolcanic, light green, massive, fine-grained, aphanitic, oxidized surface, trace pyrite

- mafic metavolcanic (amphibolitized), biotite rich segregated layers, fine-grained to aphanitic, dark grey-green, massive, oxidized/rusted surface, trace pyrite- mafic lapilli tuff, lapilli clasts weathered out on surface

- altered ultramafic flow/intrusion, emerald green colour, possibly fuschitic or vanadium alteration, carbonatized, oxidized weathered surface, trace pyrite- mafic massive flow, trace sulphide

- mafic metavolcanic, massive, fine-grained, grey on the fresh surface, weathers grey-brown, no visible sulfides

- mafic metavolcanic, fine-grained, foliated, silicified, rusty in small areas/spots, no visible sulfides

- polymictic conglomerate, qtz-feldspar matrix, mafic St felsic pebble size clasts, banded in areas

- polymictic conglomerate, matrix supported, flattened mafic Z felsic clasts

- mafic metavolcanic, overturned pillows, fine-grained, foliated-schistose, dark grey on the fresh surface, weathers brownish- flrey- felsic lapilli tuff, blue-grey on the fresh surface, weathers beige-light brown, fektepar-phyric, felsic clasts, matrix is fine to medium-grained, trace sulfides

Auppb

^

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^

5

2

•:1

4

5

-:1

•*1

•:1

•el

4

<1

<1

2

•:1

<1

<1

<1

*1

<1

<1

Page 13 of 21

Appendix l

SAMPLE NUMBERSB85007

SB8S008

SB86009

SB85010

SB8S011

SB8S012

SB86013

SB85014

SB85015

SB85021

SB85022

SB85023

SB85024

SB85025

SB85026

SB85027

SB85028

SB85029

SB85030

SB85031

SB85032

SB85033

SB85034

LOCATION

L9+85W, 4+60N

L&KXJW.5+23N

L9+OOW, 4+47N

L9+OOW, 3+27N

L7+OOW, 0+55N

L7+OOW, H12N

L7+OOW, 2+72N

L7+OOW, 4+02N

L7+15W, 4+90N

L5+OOW, 0+15N

L5+OOW, 3+50N

L5+OOW, 4+06N

L&KX3W, 4+30N

L11*OOW,3*40N

L1O96W, 3+99N

L12+OOW, 2+85N

L8+OOW, 6+90N

LS+85W, 6+85N

L11+OOW, 6+55N

L12+OOW, 4+25N

L12+OOW, 1+50N

L9+OOE.9+24N

L9+OOE, 4+74N

SAMPLE TYPE

Whole Rock

Whole Rock

Assay

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Assay

Assay

Whole Rock

Whole Rock

Assay

Assay

Whole Rock

Assay

Whole Rock

Assay

Spruce Bay Property: 1997 Sample DescriptionsDESCRIPTION

- felsic to intermediate lapilli tuff, felsic clasts, quartz-phyric

- mafic sediments ?, fine-grained, banded appearance, grey on the fresh surface, weathers rusty-brown, trace sulfides

- intermediate lapilli tuff, rusty, fine-grained, schistose, no visible sulfides

- mafic metavolcanic, fine-grained, schistose, grey on fresh surface, weathers rusty-brown, oxidized, 1* sulfides - py+cpy+bo

- greenish to grey-brown on the fresh surface, grey on fresh surface, fine-grained, foliated, mafic volcanic schist, deformed pillows, silicified - qtz * qtz/carb veinlets/strinoers- mafic volcanic schist, (pillowed ?), fine-grained, foliated, grey-brown-black on the weathered surface, dark grey on fresh, silicified, rusty in fracture planes- mafic metavolcanic, fine-grained, schistose, amphibolKized, small rusty areas/spots, trace sulfides, dark grey on fresh surface, weathers brownish grey- mafic volcanic schist, dark grey on the fresh surface, weathers rusty brown, fine-grained, trace to 1 'K pyrite, hematite present in fracture planes- intermediate to felsic lapilli tuff, banded appearance, trace sulfides, beige-rusty on the weathered surface, grey on the fresh surface- mafic metavolcanic, fine-grained, schistose, moderately silicified, deformed pillows 7, very fine-grained sulfides

- mafic metavolcanics, fine-grained, schistose, silicified/rusty along foliation S fracture planes, deformed pillows, grey on the fresh surface, weathers pale grey-brown- mafic metavolcanic, fine-grained, schistose, silicified- qtz veins/stringers , very fine-grained sulfides

- rusty/oxidized zone in mafic metavolcanics, no visible sulfides

- mafic metavolcanics, foliated, fine-grained, silicified - qtz veins/stringers, small rusty zone, grey on the fresh surface, weathers grey-white- small (.5m) rusty zone in silicified mafic volcanics?, foliated, magnetite bands, trace bornite

- diorite to quartz-diorite, fine to medium-grained, plag * k-spar bearing, epidote stringers

- mafic pillowed flow, schistose, fine-grained, no visible sulfides

- mafic volcanic schist, silicified, small oxidized zone, rusty in fracture planes

- oxidized/gossan in feldspar porphyry, weak hematite alteration, no visible sulfides

- intermediate tuff, fine-grained, epidote bearing, trace sulfides, schistose

- plagioclase-phyric diorite, fine to medium-grained, epidote bearing, in contact with granodiorite

- mafic volcanic, fine-grained, schistose, silicified along foliation planes, amphibole needles, biotite, trace sulfides, dark grey on the fresh surface, weathers light grey- mafic to ultramafic flow, fine-grained, foliated, 1-2* pyrite, in contact with porphyry dike

Auppb

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4

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2

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•:1

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^

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•:1

3

3

4

3

2

3

4

Page14of21

Appendix

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB8603S

SB85036

SB85037

SB85038

SB85039

SB85040

SB85041

SB86042

SB8B043

SB85044

SBC8604S

SBC85046

SBC8S047

SBC8S048A

SBC8S048B

SBC85049

SBC86050

SBC8S051

SBC86062

SBC86053

SBC85064

SB85201

SB85202

LOCATION

L9+OOE, 4+25N

L9+OOE.3+74N

L9+OOE, 3+74N

L9+OOE, 3+74N

L9+OOE.3+60N

L9+25E, 2+90N

L9+OOE, 1+85N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+65N

LO+90E, 7+460N

LO+90E, 7+460N

LCHSOE, 7+460N

LD+90E, 7+460N

LO+90E, 7+460N

UH-90E, 7+460N

LO+90E, 7+460N

LO+90E, 7+460N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 1O50N

L1+OOE.5+52N

L1+OOE.4+15N

SAMPLE TYPE

Whole Rock

Assay

Assay

Assay

Assay

Whole Rock

Whole Rock

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Whole Rock

Assay

Assay

Assay

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

DESCRIPTION

- mafic flow, pillowed ?, fine-grained, foliated, grey-green on the fresh surface, weathers brown-green, no visible sulfides

- contact between siltstone and diorite, coarse-grained garnet 8, hematite staining, 2-516 pyrite * bornite

- contact between siltstone and diorite, coarse-grained garnet S, hematite staining, 2-516 pyrite * bornite

- contact between siltstone and diorite, coarse-grained garnet Z hematite staining, 2-516 pyrite * bornite

- conglomerate, large ultramafic clasts, amphibolitized, schistose-foliated, gamet+bio, ^ St sulfides - py+bo

- ultramafic flow, actinolite/tremolite bearing, fine-grained, foliated, dark green on the weathered surface

- mafic metavolcanic, fine-grained, foliated, amphibolitized, garnet * epidote crystals, possibry pillowed, rusty in some fracture planes- wide gossan/oxidized zone in mafic metavolcanics, thin massive pyrite seams, 1 16 disseminated pyrite, bornite, trace chalcopyrite, foliated- wide gossan/oxidized zone in mafic metavolcanics, thin massive pyrite seams, 1 16 disseminated pyrite, bornite, trace chalcopyrite, foliated- wide gossan/oxidized zone in mafic metavolcanics, thin massive pyrite seams, 1 16 disseminated pyrite, bornite, trace chalcopyrite, foliated- mafic volcanic, strongly silicified, fine-grained, magnetic, disseminated Po, up to 2016 seams/blebs/stringers/diss Py

-similar to SBC85045

- similar to SBC85045

- feldspar porphyry dike, trace sulphides

- mafic volcanic, silicified, fine-grained, magnetic, disseminated Po, up to 1516 disseminated Py

-similar to SBC85048B

-similar to SBC85048B

-similar to SBC85048B

- mafic volcanic, fine-grained, non-magnetic, trace disseminated sulphides

- mafic/ultramafic, fine-grained, locally magnetic, trace disseminated sulphides

- mafic volcanic, fine-grained, locally magnetic, trace to 116 btebs/diss Py

- mafic to ultramafic flow top breccia, felsic and mafic clasts within mafic matrix - conglomerate or lapilli tuff ?

- mafic (pillowed 7) flow, fine-grained, amphibolitized, qtz-alb stringers along selvedges 8, fractures

Auppb

5

3

3

4

4

6

5

8

5

7

3

3

7

4.5

4

4

4

3

6

16

5

•:1

1

Page 15 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB85203

SB85204

SB85205

SB86206

SB86207

SB85208

SB85213

SBC85214

SBC8521S

SBC85216

SBC85217

SBC85218

SBC85219

SBC85220

SBC85221

SBC8S222

SBC86223

SBC85224

SBC85225

SBC8S226

SBC85227

SBC85228

SBC85229

LOCATION

L1+OOE.3+40N

L1+06E.3+50N

L1+O3E.O+65S

L11+25E.2+26N

L8+90E, 6+40N

L10+80E, 4+OOS

L9+OOE.5+50N

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+ODE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (LB+OOE, 10+50 to 11+OON)

Point Zone (LB+OOE, 10+50 to 11+OON)

Point Zone (LB+OOE, 10+50 to 11+OON)

SAMPLE TYPE

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Assay

Whole Rock

Whole Rock

Assay

Whole Rock

Assay

Assay

Whole Rock

Assay

Whole Rock

Assay

DESCRIPTION

- highly deformed ultramafic (pillowed ?) schist, fine-grained, foliated, abundant qtz-alb stringers, minor carbonate stringers

- ultramafic pillow + flow top breccia * pillows, fragments range in size from a few mm's to several em's, fragments are subangular to ovoid, fragment boundaries are filled with musc-qtz-alb stringers- quartz-phyric felsic flow/autobreccia, very fine-grained matrix with 1-2mm qtz phenocrysts (5'K), highly oxidized, trace pyrite near qtz veins- felsic lapilli tuff, light grey on fresh surface, weathers beige-white, lapilli clasts (2mm-1cm long) are highly nattened and quartz phyric, finely banded unit, ^ "X, disseminated sulfides- felsic ash tuff to crystal tuff, light grey on fresh surface, weathers greyish-white to rusty-grey, ash tuff is well bedded with silty pelite beds, trace pyrite- granodiorite to granite, medium to coarse-grained, pink on fresh surface, weathers light pink to white, massive

- gossan zone (2m wide), highly oxidized zone mineralized with 1 -2"* disseminated pyrite

- altered mafic volcanic, schistose, micaceous, no visible sulfides

altered mafic to ultramafic dike or sill, moderately magnetic

- feldspar porphyry, massive, no visible sulfides

- feldspar porphyry, massive, rusty, no visible sulfides

- contact zone - rusty ultramafic intrusion and feldspar porphyry (10 'K), no visible sulfides

- gossan zone (ultramafic intrusion), 2** disseminated/stringers to semi-massive Py-Bo-Cpy

- mafic flow, weakly foliated, moderately magnetic, up to ZX, very fine-grained sulfides

-similar to 85220

- gossan zone, similar to 85219 ( .6m apart across the host rock trend)

- mafic volcanic, schistose, non-magnetic, trace disseminated pyrite

- mafic volcanic, schistose, siljcified-qtz veins/veinlets, locally magnetic, sulfides occur in Webs, stringers, and disseminated, Py+Po, trace to "l**- mafic volcanic, schistose, qtz stringers, magnetic, 1 to 5'ft sulfides - Py+Po-disseminated/stringers/blebs, thin massive pyrite seams- mafic volcanic, schistose, qtz stringers, non-magnetic, trace pyrite

- mainly feldspar porphyry, minor mafic volcanic, non-magnetic, amphibole needles, schistose, trace disseminated sulfides

- ultramafic dike/sill, magnetic, trace sulfides, hbl needles, actinolite, trace pyrite

- contact between ultramafic dike S mafic volcanic, schistose, rusty/oxidized areas, both rocks are magnetic, trace to 3"* sulfides-Pv-Po-Molv - btebs/disseminated/strinoers

Auppb

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5

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7

4

3

5

4

49

3

5

152

18.5

32

15

4

3

2

10

Page 16 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSBC85230

SBC85231

SBC85232

SBC85233

SBC8S234

SBC85235

SBC85236

SBC85237

SBC85238

SBC85239

SBC86240

SBC85241

SBC85242

SBC85243

SBC85244

SBC85245

SBC8S246

SBC85247

SBC85248

SBC85249

SBC85260

SBC8S251

SBC85252

LOCATION

Point Zone (LS+OOE, 10+50 to 11+OON)

Point Zone (LS+OOE, 10+50 to 11+OON)

Point Zone (L8+ODE, 1O+5D to 11+OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (L8+OOE, 1O+50 to 11+OON)

Point Zone (LB+OOE, 10+50 to 11+OON)

Point Zone (LS+OOE, 1O*50to11*OON)

Point Zone (L8+OOE, 10+50 to 11+OON)

Point Zone (LS+OOE, 10+50 to 11+OON)

Point Zone (LS+OOE, 1O+50 to 11+OON)

Point Zone (LS+OOE, 10+50 to 11+OON)L8+50E, 9+15N

L8+50E, 9+15N

L8+50E.9+15N

L8+50E, 9+15N

L8+50E, 9+15N

L8+50E, 9+15N

L8+50E, 9+15N

L8+50E, 9+15N

L8+50E, 9+15N

L8+50E, 9+15N

L8+8OE, 5+50N

LS+SOE.S+SON

SAMPLE TYPE

Whole Rock

Assay

Assay

Whole Rock

Assay

Assay

Assay

Assay

Assay

Whole Rock

Assay

Assay

Assay

Whole Rock

Assay

Whole Rock

Assay

Assay

Assay

Assay

Assay

Assay

Assay

DESCRIPTION

- mafic volcanic, schistose, sulfides occur as blebs/disseminated, 1 to 516 Py

- qtz-vein S mafic flow, magnetic, trace to 2"* Py+Po, trace Po - disseminated/blebs

- adjacent to qtz-vein, intermediate/felsic hypabyssal intrusion, non-magnetic, trace to 1 16 Py

- silicified mafic volcanic, schistose, slightly oxidized, qtz stringers, trace sulfides

- ultramafic to mafic intrusion/volcanic, magnetic, actinolite+fuchstte bearing, schistose, Py+Po occur disseminated/blebs/stringers- mafic to ultramafic volcanic, non-magnetic, schistose, fine-grained sulfides, weakly oxidized in areas

- mafic to ultramafic volcanic, qtz veins/veintets, magnetic, amphibole needles, Po occurs disseminated/blebs - trace to 1 16

- ultramafic volcanic, fine-grained, schistose, amphibole needles, magnetic, rusty/oxidized, trace to 5"*) Py+Po, trace Bo+Cpy

- ultramafic volcanic 8* gossan, stringers and blebs of Py - up to 10% l disseminated Po, qtz stringers

- mafic volcanic, gossan/oxidized, magnetic, moderately silicified, Py stringers/blebs - up to ID'%, trace to 1 'X, Po, trace Bo+Cpv, hematite staining- ultramafic to mafic volcanic, fine-grained, magnetic, pyrite occurs in blebs/stringers - up to 2-3*96 Py, trace disseminated PO+ Bo+Cpv- gossan zone, oxidized/rusty, mafic to ultramafic volcanic, schistose, trace sulfides

- mafic volcanic, schistose, rusty, magnetic, epidote S hematite (stringers * patches), trace to W Py+Po+Bo+Cpy - disseminated- mafic volcanic, fine-grained, biotite rich, schistose, trace pyrite, qtz stringers

- mafic volcanic, fine-grained, schistose, magnetic, Py - disseminated/stringers, Po - disseminated, trace Bo+Cpy - disseminated- mafic metavdcanic, variolitic ?, qtz stringers, locally magnetic, schistose, fine-grained, trace Py+Po+Bo+Cpy

- mafic to ultramafic volcanic, chiefly magnetic, fine-grained, schistose, trace to W Py+Bo+Cpy+Po

- mafic to ultramafic, silicified, fine-grained, schistose, magnetic, trace to 116 Py+Po

- mafic to ultramafic volcanic, fine-grained, schistose, qtz veinlets/stringers, locally magnetic, trace to 216 Py+Po

- mafic to ultramafic, variolitic ?, fine-grained, schistose, epidote, qtz veinlets/stringers, weakly to strongly magnetic, trace to 316 PY+PO, trace Bo+Cpy- mafic to ultramafic volcanic , fine-grained, schistose, silicified, moderately magnetic in areas, epidote bearing, trace Pv+Po+Bo- sediments (siltstone-6b,c), alternating mafic A felsic bands, very fine-grained to fine-grained, trace to 316 pyrite - disseminated/seams/blebs- sediments (pelftes-6u,c) , alternating mafic ft felsic bands, qtz stringers, hematite, trace to 316 Py, trace Bo+Cpy - disseminated/biebs/strinaers

Auppb

19

5

2

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6

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Page17of21

Appendix l

SAMPLE NUMBERSBC85253

SBC8S2S4

SBC85255

SBC86266

SBC86257

SBC85258

SBC85269

SBC85260

SBC85261

SBC85262

SBC86263

SBC85264

SBC85265

SBC85266

SBC85267

SBC85268

SBC85269

SBC86270

SBC86271

SBC85272

SBC85273

SBC85274

SBC85275

LOCATION

L8+80E, 5+50N

L8+80E, 5+50N

L8+80E, 5+50N

L8+80E, 5+50N

L8+80E, 5+50N

L8+80E, 5+50N

L8+80E, 5+50N

L9+OOE.3+75N

L9+OOE, 3+75N

L9+OOE.3+75N

L9400E,3*75N

L9+OOE, 3+75N

L9+OOE, 1+6SN

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+50N

L9+OOE, 1+51N

L9+OOE, 1+52N

L9+OOE, 1+53N

L9+OOE, 1+54N

SAMPLE TYPEAssay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Whole Rock

Assay

Assay

Assay

Assay

Spruce Bay Property: 1997 Sample DescriptionsDESCRIPTION

- sediments (6u,c), banded, very fine-grained to fine-grained, rusty/oxidized, Py - up to to 2%-seams

- mafic volcanic schist, alternating light Z dark bands, fine-grained, silicified, trace disseminated pyrite

- mafic volcanic schist, alternating light & dark bands, * felsite dike or sill, ^ %Py- seams/stringers

- sediments (siltstone-6b,c), alternating mafic a felsic bands, very fine-grained to fine-grained, pyrite - stringers/seams/blebs, * felsite dike or sill- sediments (6r), fine to medium-grained, banded, rusty, trace to^Vb pyrite seams/stringers

- sediments (6u,c), banded, fine to medium-grained, rusty, trace to •el * Py seams/stringers/blebs, qtz veinlets/stringers

- mafic volcanic schist t felsite dike or sill, fine to medium-grained, rusty/oxidized, qtz veins/stringers, 1 'fc Py seams/strinqers/disseminated- diorite to intermediate/felsic intrusive, garnet * biotite rich zones, fine to medium-grained, qtz vein/veinlets, non-magnetic, trace to 1 "fc disseminated Py, Bo+Cpy- diorite/gabbro, garnet, fine to medium-grained, weakly to moderately magnetic, trace disseminated Po+Py

- diorite/gabbro, garnet * biotite rich, hornblende crystals, trace disseminated Py, weakly magnetic - Po ?

- diorite/gabbro, gamet+btotite+chlorite? rich zones, locally magnetic, trace to ^ Py+Po (sulfides occur in or on the border of the garnet rich zones)- diorite/gabbro, gamet+biotite rich zones, locally magnetic, trace disseminated Po, trace to 1 'ft Py, hematite staining

- rusty/oxidized, mafic volcanic, fine-grained, weakly magnetic, trace Py+Po+Bo+Cpy

- rusty/oxidized, mafic volcanic, fine-grained, weakly magnetic, trace Py+Po+Bo+Cpy

- rusty/oxidized, mafic volcanic, fine-grained, locally magnetic, trace to 1 "X. Py - stringers/blebs/disseminated, trace disseminated Po+Bo+Cpv- mafic volcanic, rusty/oxidized, fine-grained, magnetic, up to 8% Py+Po - diss/blebs/stringers

- gossan zone, sheared, magnetic, trace Py+Po, too rusty to determine protolith - probably mafic volcanic

- rusty/oxidized zone, sheared, mafic volcanic, magnetic, fine-grained, up to 10"* Py - diss/blebs/stringers, trace to 1 'ft disseminated Po, trace Bo+Sph+Mo?, hematite staining- intermediate volcanic, fine-grained, locally weakly to moderately magnetic, trace to 3")fc Py - diss/blebs/stringers, trace disseminated Po- intermediate volcanic, minor feldspar porphyry unit, locally magnetic, trace Bo+Po, Py seams/diss/btebs/stringers - up to 1CWfc

- intermediate volcanic, fine-grained, weakly to strongly magnetic, trace disseminated Po+Cpy+Mo, trace to 1 "* disseminated Bo+Sph, up to 7* Py - diss/stringers/seams/blebs- intermediate volcanic, very weakly magnetic, trace Po, trace to -:1 % Bo+Sph, up to 7"fc Py - diss/stringers/blebs/seams, minor feldspar porphyry unit- chiefly intermediate volcanic, fine-grained, qtz veins/stringers, locally magnetic, trace to <2% disseminated/patches Sph+Bo, trace Po+Cov. UD to 8"X. Pv - seams/diss/btebs/strinaers

Auppb

^

<1

<1

<1

<1

1

10

t1

4

<1

<1

<1

<1

<1

<1

•M

1

<1

1

2

•:1

2

2

Page 18 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSBC85276

SBC85277

SBC85278

SBC85279

SBC86280

SBC85281

SBC85282

SBC85283

SBC85284

SBC85285

SBC86286

SBC85287

SBC85288

SBC85289

SBC85290

SBC85291

SBC85292

SBC85293

SBC8S294

SBC85295

SBC85296

SBC86297

SBC85298

LOCATION

L9+OOE, 1+55N

L9+OOE, 1+56N

L9+OOE, 1+57N

L9+OOE, 1+58N

L9+OOE, 1+59N

L9+OOE.1+61N

L9+OOE, 1+62N

L9+OOE, 1+63N

L9+OOE, 1+64N

L9+12E, 1+64N

L&H2E, 1+65N

L9+15E, 1+66N

L9+15E, 1+67N

L9+15E, 1+68N

L9+15E, 1+69N

L9+15E, 1+70N

L9+02E, 1+50N

L9*02E, 1+50N

L9+02E, 1+51N

LO+90E, 7+60N

LO+90E, 7+60N

LO90E, 7+eON

L090E, 7+60N

SAMPLE TYPE

Whole Rock

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

Assay

DESCRIPTION

- mafic volcanic, silicified, locally weakly to strongly magnetic, Py+Po+Sph+Bo

- chiefly mafic volcanic between minor feldspar porphyry unit, locally magnetic, trace Po, up to 4'ft seams/stringers/diss Py

- mainly mafic volcanic, minor feldspar unit, locally magnetic, rusty, trace Po+Sph+Bo, up to 3*96 stringers/blebs/diss Py

- mafic volcanic, silicified, fine-grained, magnetic, trace to 1 'k patches/disseminated Bo+Po+Sph, up to 6St Py - seams/blebs/stringers/diss- mafic volcanic, silicified, fine-grained, magnetic, trace Py+Po+Bo+ACpy

- mafic volcanic, fine-grained, magnetic, silicified - qtz veins, trace to 1 "fa Po+Bo+Cpy+Aarsenopyrite, up to 5% blebs/stringers/diss Py- mafic volcanic, silicified, magnetic, fine-grained, trace to 1 'K Po+Bo+Cpy, up to Tk blebs/stringers/diss Py

- mafic volcanic, silicified, fine-grained, magnetic, trace to 1 * Po, Bo+Cpy+Mo, up to to 4Vi blebs/stringers/diss Py

- mafic volcanic, silicified, fine-grained, magnetic, trace Po+Bo, 1 to A1*! seams/stringers/btebs/diss Py

- mafic volcanic, banded, silicified, fine-grained, magnetic, trace Bo+Sph+Cpy, trace to 1 "fc Po, up to 4"*! seams, stringers, diss PY- mafic volcanic, strongly silicified, fine-grained, magnetb, trace to \ *h Po+Bo+Sph+Cpy, up to 10*36 seams/stringers/btebs/diss Pv-similar to SBC85286

- mafic/ultramafic volcanic, silicified, fine-grained, magnetic, trace to 1* Po+Bo+Sph+Cpy, up to 15% disseminated Py

-similar to SBC85288

-similar to SBC85288

- similar to SBC85288

- intermediate/mafic volcanic, silicified, rusty/gossanous, non-magnetic, up to 1CWi stringers/diss Py, trace to 1 Vb Bo+ASph

- intermediate/mafic volcanic, silicified, fine-grained, locally magnetic, trace disseminated Po, up to 10*36 disseminated Py

- similar to SBC85293

- mafic volcanic, fine-grained, magnetic, silicified - qtz stringers, 1 "ft disseminated Po, up to B1h disseminated Py

- mafic volcanic, fine to medium-grained, locally magnetic, actinolite needles, coarse plagioclase+qtz alteration, up to 25'* semi massive+disseminated coarse pyrite, Po blebs- mafic volcanic, silicified - qtz stringers/veinlets, fine-grained, magnetic, trace disseminated Po+ASph, up to Id1* stringers/blebs/diss Py- mafic volcanic, silicified, fine to medium-grained, magnetic, Z1*! disseminated Po, up to 2OTfe btebs/stringers/seams/diss Py

Auppb

3.5

•el

<1

*1

4

2

1

3

2

2

6

3

3

4

t1

•el

4

3

3

8

2

1

1

Page 19 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSBC85299

SBC85300

SB85301

SB85302

SB85303

SB853M

SB8S30S

SB85306

SB85307

SB85308

SB85309

SB85310

SB85311

SB8S312

SB85313

SB85314

SB85315

SB8S316

SB85317A

SB85317B

SB86318

SB86319

SB85321

LOCATION

LO+90E, 7+60N

LO+90E, 7+60N

L6+30W, 2+OON

L5+90W, 5+OON

L6+10W, 0+25N

L6+QOW, 2+60S

L6400W, 3+75S

L4+OOW, 0+50S

L4+OOW, 5+ODN

L3*OOW,Ot75S

L3+OOW.3+50S

L3*15W,0*75N

L3+OOW.3+OON

L1+OOW, 1+75S

L1*90W,Of25S

L2+OOW, 1+50S

L1+85W.2+25S

L2+OOW, 1+QON

L2+ODW, 2+30N

L10+OOE, 7+OON

L10+OOE.8+10N

L10+OOE, 10+35N

L4+OOW, 6+25N

SAMPLE TYPEAssay

Assay

Assay

Assay

Whole Rock

Whole Rock

Whole Rock

Assay

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Whole Rock

Assay

Assay

Whole Rock

Assay

Whole Rock

Whole Rock

Whole Rock

Whole Rock

DESCRIPTION

- similar to SBC85296, sulphides in qtz vein

- mafic volcanic, silicified, fine-grained, magnetic, 1* Po, up to 20*36 disseminated Py

- mafic metavolcanic, massive, silicified, fine-grained, dark green, aphanitic, rusted/oxidized surface, trace pyrite

- potassic and hematitic stained quartz vein within massive mafic metavolcanic, trace sulphide

- heterolithic and polymictic conglomerate with predominantly granodiorite ellipsoidal clasts stretched parallel to fabric, intermediate matrix and slightly gneissic, trace pyrite- heterolithic (polymictic) conglomerate with intermediate gneissic matrix with predominantly ellipsoidal granodiorite clasts stretched parallel to fabric, trace pyrite- pyroxentte/homblendite, possible proterozoic unaltered xenolith rafted within granitic pluton, massive, dark green, extremely coarse-grained, insertal crystals, trace pyrite- polymictic conglomerate with potassic and hematitic altered quartz vein, trace sulphide

- intermediate lapilli tuff, light grey on the fresh 8. weathered surface, trace sulphide

- mafic metavolcanic, dark green to grey, massive, fine-grained, aphanitic, amphibolitized, rusted/oxidized surface, trace pyrite

- xenolithic granitoid, coarse-grained, aphanitic, amphibolitized xenolKhs rafted within gneiss, trace pyrite

- deformed mafic pillowed flow, t-2% finely disseminated pyrite

- mafic volcanic, fine-grained, massive, trace sulphide

- polymictic conglomerate with ellipsoidal granodioritic clasts stretched parallel to fabric, trace pyrite

- mafic metavolcanic, light green to dark grey, fine-grained, aphanitic, massive, amphibolitized, north-south trending granodioritic dikes, trace pyrite- amphibolitized mafic metavolcanic, fine-grained, aphanitic, slightly hematitic with gossanous, limonitic alteration, trace pyrite

- felsic lapilli tuff, extremely siliceous, feldspathic, light buff and banded, tuffaceous texture, pitted weathered surface, OS-1% finely disseminated pyrite- mafic pillowed flow, fine-grained, aphanitic, deformed pillows with tops to north, trace sulphide

- mafic volcanic, light green, slightly sheared, fine-grained, rusted/oxidized with 0.5-1 "it finely disseminated pyrite

- schistose mafic metavolcanic, fine-grained, light grey to buff weathered surface, fine lineations comprising fabric, trace pyrite

- schistose mafic metavolcanic, fine-grained, aphanitic, well developed tuffaceous bedding, trace sulphide

- gabbro, coarse-grained, roughly equal proportions of pyroxene/plagioclase, massive, 2-3*ft disseminated pyrite

- gneissic, intermediate to mafic tuff, slight potassic alteration, 0.5-1 1b disseminated pyrite

Auppb

1

1

•:1

•el

*:1

1

•ci

22.5

3

6

5

6

9

6

1

2

3

3

2

3

3

4

5

Page 20 of 21

Appendix l

Spruce Bay Property: 1997 Sample DescriptionsSAMPLE NUMBERSB86322

SB85324

SB85325

LOCATION

L4+OOW, 5+66N

L6+15E, 2+10N

L7+OOE, 2+65N

SAMPLE TYPEAssay

Whole Rock

Whole Rock

DESCRIPTION

- polymictic conglomerate, clasts predominantly granodiorttic and ellipsoidal stretched parallel to fabric, hematitic alteration, trace sulphide- silicified mane to intermediate flow, 1 -2* disseminated pyrite

- strongly silicified mafic flow, trace epidote, 1 -2"* disseminated pyrite

Auppb

3

1

5

Page 21 of 21

Appendix II

Spruce Bay Property

Selected 1997 Base Metals Analyses

APPENDIX II

SPRUCE BAY PROPERTY: 1997 SELECTED BASE METAL RESULTS

Sample Number

SB119035

SB119043

SB119150

SB119152

SB119154

S B1 191 81

SB119221

SB 11 9224

SB119225

SB119240

SB119241

SB119244

SB119248

SB119249

SB119286

SB119300

SB119429

SB1 19432

SB119437

SB119440

SB 11 9442

SB 11 9449

SB119450

SB1 19461

SB1 19475

SB1 19483

SB85008

SB85009

SB85036

SB85037

SB85038

SB85042

SB85043

SB85044

SBC85053

Location

L15+OOE, 7+20N

L11+95E, 6+60N

L15+97N.8+45N

L15+85E, 7+85N

L16+OOE.4+90N

L7+03E, 11+30E

L1+65W, 11+15N

L1+45W, 11+35N

L1+35W, 11+30N

L8+OOE, 10+90N

L8+05E, 10+80N

L8+OOE, 10+60N

L7+65E, 9+OON

L7+80E, 8+95N

L25+OOE, 14+75N

L20+28E, 15+30N

L7+83E, 4+40N

L8+OOE, 4+1 ON

L4+03E, 1+90S

L5+OOE, 1+OON

L5+OOE, 2+95N

L3+OOE, 0+24N

L3+OOE, 2+95S

L4+25E, BLO

LO+00, 6+25N

L2+OOW, 5+25N

L9+OOW, 5+23N

L9+OOW, 4+47N

L9+OOE, 3+74N

L9+OOE, 3+74N

L9+OOE, 3+74N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+65N

L8+OOE, 10+50N

Cu ppm329

49.5

80.7

95.3

356

18.8

236

229

266

287

132

271

547

23.5

231

231

53

203

54.3

88

5.4

50

23

61.4

282

8.4

19.3

40.1

105

68.4

114

151

66.4

56

688

Zn ppm23.2

55.7

17.4

36.8

27.5

263

1240

258

17.2

1750

316

226

8560

329

1450

78.4

74.5

75.3

254

127

98.2

92.3

55.1

270

269

31.1

97.3

223

14.7

36.5

40.6

406

206

298

1620

Ni ppm

---------

103

90

187

297

15-

-

-

-

-

320-

-

-

-

-

17-

11

37

31

44

65

42

34

137

Pb ppm

7

^

^

^

5

22

5

6

4

37

15

32

41

16

12

10

7

3^^3

16

10

^

^

15

17

20

28

35

41

30

30

23

4

Gr ppm

--------.-

312

872

794

82

132-

-

-

-

-

435-

-

-

-

-

238-

100

265

283

406

121

97

73

306

MO ppmO

45

10

16

2

1

7

2

3

3

4

4

18

8

12

3

14

10

2

5

48

17

10*:1

1

14

16

18

11

11

10

^

3

10

13

Page 1 of 3

APPENDIX

SPRUCE BAY PROPERTY: 1997 SELECTED BASE METAL RESULTS

Sample NumberSB85213

SBC85215

SBC85218

SBC85219

SBC85222

SBC85224SBC8S225SBC8S228SBC8S229SBC85236

SBC85237

SBC85238

SBC85239

SBC8S240

SBC85242

SBC85251

SBC85252

SBC85253

SBC85254

SBC85256

SBC85257

SBC85258

SBC852S9

SBC85260

SBC85261

SBC85262

SBC85263

SBC8S264

SBC85265

SBC85266

SBC85267

SBC85272

SBC85274

SBC85280

SBC85281

Location

L9+15N, 4+35N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50NL8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L8+OOE, 10+50N

L9+50E, 9+1 5N

L9+OOE, 5+50NL9+OOE, 5+50N

L9+OOE, 5+50N

L9+OOE, 5+50N

L9+OOE, 5+50N

L9+OOE, 5+50N

L9+OOE, 5+50N

L9+OOE, 5+50N

L9+OOE, 3+75N

L9+OOE, 3+75N

L9+OOE, 3+75N

L9+OOE, 3+75N

L9+OOE, 3+75N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+65N

L9+OOE, 1+51 N

L9+OOE, 1+63N

L9+OOE, 1+59N

L9+OOE, 1+61 N

Cu ppm50.1

92.2

134

610

613

56.5

227

85.2

394

30.6

342

304

328

235

148

156

42.2

115

72.8

124

69.5

92.7

75.4

187

171

81.8

148

157

65

69.7

72.7

48

53.6

109

74.3

Zn ppm355

59.2

218

3680

1270

126

546

240

2910

252

666

1060

420

163

130

466

309

331

309

452

293

410

271

47

21.9

34.9

13.6

30.7

260

191

217

57.7

82.1

207

220

Ni ppm

19

300

91

309

445

50

117

587

257

57

338

221

211

181

79

62

27

45

40

32

22

27

31

63

58

54

45

58

29

35

37

47

37

56

49

Pb ppm

10

22

24

33

35

20

19

12

27

35

31

36

27

29

22

24

17

24

20

30

23

20

21

33

20

25

21

24

19

19

20

3

3

^

^

Cr ppm97

647

604

463

768

110

154

1670

659

207

1110

612

490

1050

216

96

90

73

127

88

73

109

89

211

159

279

264

183

69

67

60

106

114

77

61

Mo ppm

10

3

7

8

5

12

5

3

8

5

3

9

4

3

11

8

4

4

7

4

4

7

5

29

15

11

10

10

5

58

5

10

23

6

7

Page 2 of 3

APPENDIX

SPRUCE BAY PROPERTY: 1997 SELECTED BASE METAL RESULTS

Sample Number

SBC85282

SBC8S283

SBC85284

SBC85288

SBC85289

SBC85290

SBC85291

SBC85296

SB85302

SB85303

SB85304

SB85306

SB85310

Location

L9+OOE, 1+62NL9+OOE, 1+63N

L9+OOE, 1+64N

L9+15E, 1+67N

L9+15E, 1+68N

L9+15E, 1+69N

L9+15E, 1+70N

LO+90E, 7+60N

L5+90W, 5+OON

L6+10W, 0+25N

L6+OOW, 2+60S

L4+OOW, 0+50S

L3+15W, 0+75N

Cu ppm64.6

84.2

95.3

81.4

170

113

148

135

11.5

34.1

20.4

38

277

Zn ppm206248284

343

291

327

266

91.4

6.2

92.9

131

70.2

95.6

Ni ppm

515146

50

67

46

69

37-

-

-

-

91

Pb ppm^^^^^3

<2

^<2

15

15

17

23

Cr ppm

8510081

11198

100

99

75-

-

-

-

204

Mo ppm

3344

3

5

4

14

241

12

12

14

4

Page 3 of 3

Appendix III

Selected Lithogeochemical Ranges

and

Mean Values for Least Altered Samples

Appendix III

White Lake and Spruce Bay Properties

Selected Lithogeochemical Ranges (Most Altered and Least Altered) A Mean Values For Least Altered Samples -1997

Ultramafic VolcanicLeast Altered

Most Altered

Arithmetic MeanMafic Volcanic

Least Altered

Most Altered

Arithmetic MeanIntermediate Volcanic

Least Altered

Most Altered

Arithmetic MeanFelsic Volcanic

Least Altered

Most Altered

Arithmetic MeanPeridotiteLeast Altered Most Altered

Arithmetic MeanHornblendite/Py rozenite

Least Altered Most Altered

Arithmetic MeanGabbro

Least Altered Most Altered

Arithmetic MeanDiabase

Least Altered

Most Altered

Arithmetic Mean

SI02•A

35.9 49.716.5

43.4 62

51.5

55.6 71.263.96

68.6 78

71.23

30.8 47.839.3

3852.445.2

46.7 55.150.9

48.2 50.148.15

A12O3 /o

2.95 16.89.2

5.78 20.714.04

10.6 16.715.37

11.5 15.714.45

0.69 9.955.32

3.61 19.111.35

13.1 17.915.5

13.1 16.614.85

MgO /o

6.832.720.18

2.29 12.57.39

1.215.32.9

0.51 1.790.85

14.2 43.829

9.18 18.313.74

5.8 11.68.7

5.17 8.887.02

T102 /o

0.15 0.910.5

0.28 2.651.28

0.28 1.260.92

0.17 0.510.39

0.4 0.620.33

0.254 0.950.6

0.5 1.30.9

0.59 2.491.54

CaO /o

1.67 19.69.46

3.67 19.510.52

2.8 9.635.46

1.47 6.063.27

0.37 10.85.58

9.63 14.712.16

8.06 12.910.48

8.43 12.110.26

Na20 /o

0.05 3.161.01

0.72 5.772.58

1.09 6.784.2

1.52 5.954.31

0.05 1.6

0.82

0.72 2.121.42

1.323.52.41

1.63 2.882.25

K2OV,

O.01 2.450.46

0.05 2.040.48

0.19 6.841.89

0.02 5.181.88

0.01 0.120.06

0.11 1.130.62

0.1 1.260.68

0.23 1.030.63

Fe203"/O

8.14 16.311.44

7.34 22.213.37

2.96 10.45.41

1.29 6.893.45

8.49 12.913.4

7.46 14

10.73

8.3 16.212.25

9.29 17.513.4

Ni ppm

124 863

-

15 320

-

14 101

-

26 30-

-

-

.

58 68

-

-

-

Cr ppm

261 1780

-

68 640

-

44 168.

75 256

-

-

-

.

177 190

.

-

-

NOTE: White Lake Property - 200 Whole Rock Sauries

Spruce Bay Property -315 Whole Rock Samples

Page 1 of 1

Appendix IV

Spruce Bay Property

1997 Analytical Results

Pa c. j e i

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE / A DIVISION OF SGS CANADA INC

129 AVE. REAL CAOUETTE - C.R 2283 - ROUYN-NORANDA - QUEBEC J9X 6A9 TO... (819) 784-9108 FAX: (819) 76*4673

CEP.TiFlCAT D'ANALYSE/CERTIFICATE GF ANALYSIS

Noin de la Compagnie-Company: Homes Cake ExplorationBen de Commanda No/ P.O. No:Projet/ Project No : 90763Date Scumis/ Submitted : Jun 23, 199"Attention : IKS Osmani

R12057

Jun 26, 199'

Mo. D'Echantiilon AU Sample No. PFB

AU CHK

SB119026 SB119027 SB119023 SB119029 SB119030 SB119031 SB119032 SB119033 SB119034 SB119035 SB119036 SB119037 SB119038 3B119039 SB119040 SB119041

212

i^O

2 '

ci

SB119137SB119138

-^(JWiliidjy*dL-5B119140VOL5B119141VJUSB119142~ SB119143

SB119144 SB119145

- SB119146SB119147SB119148SB119149SB119150SB119151SB119152

- SB119153SB119154SB119155SB119156

~ SB119157SB119158SB119159

IN2 \i \ jSfe**asg*S^ t-v?liA"t5 L^J/P " ~" \ ^^0D9ip'BwlS^9Mlf v ^* V\A^VL xi^*tJC^^.1 \ P

< l \

*1 \

21

2211434

2 ^^^~ O ~ ~" ' ^yn)VUjUi^ t^^u-\^"^ I ^ \

O

33 ; 22 l3 li1 1i y

Certifie par X Certified bvMembre du Grouiw SGS (Sociita Generate de Surveillance)

Fag;

XRAL LES LABORATOIRES XRAL LABORATORIESLINE DIVISION OE l A DIVISION Of SGS CANADA INC.

129 AVE. REAL CAOUETTE - C P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 TEL.: (818) 764-9108 FAX. (819) 764-4673

CEPTTFICAT D'ANALYSE.'CERTIFICATE OF ANALYSIS

BonPro jet/ Project NoDate Sounds/ SubmittedAttention

: 9076'1- jun 7 -J 1007i I ke Bsn^ '

R12C5

Jun 26,

No. D'EchantillonSample No.

5B119150— SB119162 ———————^ SB119163UIUSB119308JIL-5S119309Ju5fill9310VJU5B119311— sBiiyji2 ————

SB119313SB119314

^ SB119315SB119315SB119317SB119316

- SBI19319SB119320SB119321SB119322SB11S323SB1193243B119325

- SB119326SB119327SB119328SB119329

~~ SB119330SB119331SB119332

-. SB119333SB115334SB119335SB119336 v

- SB119337SB119338SB119341SB119342SB119343SB119344

AU AU CHKFPB FFB

2 X *^p**uc- Qz*\2. ViOVUiti Ladi* ——— ———— " ————— — ____ -

4 - *^pvwcjC^ f&a-^ "" — - —— r2 ' , ~~. — ———— —————————— - ——— -i-; x vOUA^^ WLP2 3 ^l f

3', ^j?^^ 6*V\2 / li V]1' ^•5 X

i x5 ';'3 x2^2^ 2^5^4 X2 Xlx 2/4'3'1'1'i'i'2'?-"i/10^oxi/ <i/i"i^2'3 '

Mambr. du Croupe SCS (SocKtte G^nAnte de Surraitonc*)

XRALPage 3

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OP SGS CANADA INC.

129 AVE. BCAL CAOUETTE - C.P 22M - ROUYN-NORANOA - QUCBCC J9X SA9 T6L: (819) 764-9106 FAX: (81B) 764-4873

CERTIFICAT D'ANALYSE'CERTIFICATE OF ANALYSIS

R12057Nom de la Compagnie/Company: Homestake Exploration Bon de Commande No/ P.O. No: Projet/ Project No : 90753Date Sounds/ Submitted : Jun 23, 1997 Jun 26 1997 Attention : ike Osmani

NO. P'Echantillon AUAU CHK" Sample No. PFB PPB

SB119345 2' ^S-PVTMUL. /Wl ,SB119346 lf i iSB119347 V sSB119348 4 'SB119349 3^-SB119339 2 ySE119340 l x

Membre du Groups SGS (Societi Generate de Surveillance)

Page l

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE / A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Norn de la Compagnie/Company: Bon de Commande No/ P.O. No: .Projet/ Project No : Date Soumis/ Submitted : Attention :

Homestake Exploration

90763/90764 Aug 01, 1997 Ike Osmani

R12465

Aug 05, 1997

-No. D'Echantillon AU AU CHK Sample No. PPB PPB

SB119445SB119446 SB119447-SB119448SB119449SB119450SB85201SB85202SB85203SB85204-SB85205'SB85206SB85207.SB852083^.85209 —————

11 •ci<l1<l<l1<l<l•ci<l<l5^T

^r D^^^ ^

<l

1 "NI'Hi i^*.Lr — ———— 'X,J3*85210

SB119400.SB119478 SB119479SB119480SB119481-SB119482SB119483SB119484-SB119485SB119486SB119487SB119488"SB119489

^IL9ftll9491 vvU- 6119492 W .^fi!19493* -9^119494W-^B11^406 ————

-1

<l-ci52^45•ci 1<l

____ l i

3<l<l

Isfwwx-B*^ —— '^ ^

i^Uk^

-Certifie par /' Certified bdu Groupe SGS (Societe Ginerale de Surveillance)

XRAL

Page 2

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE / A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 * ROUYN-NORANDA - QUEBEC J9X 5A9 TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

R12465Norn de la Compagnie/Company: Homestake Exploration Bon de Commands No/ P.O. No:

-Projet/ Project No : 90763/90764Date Soumis./ Submitted : Aug 01, 1997 Aug 05, 1997 Attention . : Ike Osmani

No. D'Echantillon AUAU CHK Sample No. PPB PPB

SB119497 *cl ^ •^pvvvcc J^A^XSB119498 ^ ' ^J

^SB119499 2SB119500 <lSB85001 <lSB85002 *:1

- SB85003 <lSB85004 <lSB85005 <l

- SB85006 -ciSB85007 <l <lSB85008 <lSB85009 <l

- SB85010 -ciSB85011 -ciSB85012 5

^ SB85013 4SB85014 -ciSB85015__________5! ___________________________ ^^----—^^

z l

V -9B85018 <:

WL5B85020- SBSb021

SB85022SB85023

- SB85024SB85025SB85026SB85027SB85301SB85302SB85303

- SB85304SB85305SB85306

. SB85307

<l ^^jOV\vX^, O^A^\

<l s<l<l<l<l <l<l<l<l1.ci^4 21

3

Membre du Groupe SGS (Societe Generate de Surveillance)

XRAL

Page l

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE 7 A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 . TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Norn de la Compagnie/Company: Homestake ExplorationBon de Commanda No/ P.O. No:Projet/ Project No : 90763/90764T)ate Soumis/ Submitted : Aug 11, 1997Attention : Ike Osmani

No. D'Echantillon AUAU CHKSample No. PPB PPB

R12562

Aug 15, 1997

-SBC85214 3BC85215 SBC85216

3BC85218 3BC85219 SBC85220

3BC85222 SBC85223 .SBC85224 5BC85225 3BC85226 SBC85227

3BC85229 SBC85242

7435449351522132154321064

4 3 5- 857

656o

33

16

3B85321 SB85322

^-^6.85323 3B85042 SB85043,SB85044 3B85308 3B85309 SB85310^685311 3B85312 SB85313 SB85314 3B85315 3B85316 SB85317"3B85317B 3B85318

*lLSfiB5028-SB85029

Certi fie par l Certified bybre du Groupc SGS (Societe Generate de Surveillance)

XRAL

Page 2

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

R12562Nom de la Compagnie/Company: Homestake Exploration Bon de Commande No/ P.O. No: Projet/ Project No : 90763/90764'Date Soumis/ Submitted : Aug 11, 1997 Aug 15, 1997 Attention : Ike Osmani

No. D'Echantillon AUAU CHK Sample No. PPB PPB

-SB85030 4 4SB85031 3SB85032 2^SB85033 3SB85034 4SB85035 5SB85036 3-SB85037 3SB85038 4SB85039 6JSB85040 7 5SB85041 5

Membre du Groups SGS (Societe Generate de Surveillance)

, \

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE f A DIVISION OP SGS CANADA INC129 AVE. REAL CAOUETTE - C .P 2283 - ROUYN-NORANDA - QUEBEC J9X 5AS

TEL : (819) 764-9108 FAX: (819) 764-4673

CFPTTFT.;-.-.T D' AMAT,Y:SE,'CERTIFICATE OF ANALYSIS

Norn de la CompAgnis "r/rrip.iny: Homs.rt-.3kft Exploration Bon de Commands Ne F-. O . Me :Pro jet/ Project Me : 90~:;.:; ? 07 S 4Date Soumis ' Submir.t.s-ri : Jul IT, 12?"Attention : Ike Osmani

R12261

Jul 16., 199"

No. D'Echantd l L on aU .~J.j CHK Sample No. FFE FPB

SB11S179 SB119180 SB1191S1 SE11S182 SB119183 SE119184 SB119185 SB119186 SB119187 SB119188

WL119191•WK119192-WL119193 WL119194 WL119195

-vail 92 00-WT.1 1Q401-WL119402-1-JL119403-VJL119404-WL119405-WL119406

-WL119408-/JL119409-WL119410 WT.1 1941 1

SB119363 SB119364 SB119365 SB119366

264

J 4 3 2 1 1 -,- 1 1-l

•:: 1

--.i

Certifie par l Certified byMcmbre du Groups SGS (Socitte Gen*r*(e de Surveillance)

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE / A DIVISION Of SGS CANADA INC.129 AVE. RSAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL.: (819) 764-9108 FAX: (fl19) 764-4673

CEPTT-iCAT D'ANALYSE/CERTIFICATE OF ANALYSIS

.Norn de la Compagnis Company Bon de Commanda No. P.7.. Mo Pro jet 7 Project. Ne pace Suuiuis/ Submit - e d

-At tent i on

HcmH:it.ake Exploration

5QT63.-90764 Jul 11, 1027 ike Osrrani

"261

Jul 15, 199-

No. D'Echanr.ilion AU AU CHK Sample No. PFE F PH

SB119367 -SB119368

SB119369,5B1193"7Q

"•WL119371

WL1193V3WL119374-WL119375

T

f]

Membre du Group* SGS {Societe G*n*rai* d* Surveillance)

Page l

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION OE l A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C. P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Norn de la Compagnie/Company: Homestake Exploration Bon de Commands No/ P.O. No: Projet/ Project No : 90763/90764 -Date Sounds./ Submitted : Jul 24, 1997 Attention : Ike Osami

R12389

Jul 29, 199'

,JSTo. D'Echantillon AU AU CHKSample No.

--WL119378WL1193.79WL119380

•WL119381WL119382/JL119383 WL119384

-WL119385,VL119386

-1A/L119387^WL119388

/tfL119389' ,VL119392 "~~-WL119393•-WL119412

tfL119413

-WL119415VL119416VL119417

-WL119418-WL119419

VL119420-VJL119421-WL119422

•7L1194237L119424SB119390

3B119394 SB119395

^SB119396" 5B119397JB119398SB119399

--5B1194245B119425

SB119426-SB119427

PPB PPB

* V^OKV^^, kcoUfi—^651

Ai5*j * \ '

53 ,6<l V "•3 . f-l5 . 6

452

.1•ci54 51346t ^~pv^ti— rSd-A^*10 -^ J -1<l1oN/ST

O ^^^--. .

paribre du Groupe SGS (Societe Generate de Surveillance)

Page

XRALLES LABORATOIRES KRAL LABORATORIES

UNE DIVISION DE l A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

tom de la Compagnie/Company: Homestake Exploration 3on de Cornmande No/ P.O. No: Projet/ Project No : 90763/90764

-Oate Soumis/ Submitted : Jul 24, 1997 \ttention : Ike Osami

R12389

Jul 29, 199'

JsTo. D'Echantillon AU AU CHK Sample No'. PFB PPB

-SB119428 5B119429 SB119430JB119431 IB119432 ;B119433SB119434

IB119436oB119437JB119438.B119439;B119440SB119441•-^6119442B119443 iB119444 ^6119451B119452B119453

SB119454 CB119455B119456

SB119458B119459B119460

SB1194610B119462B119463

5B119464SB119465B119466

..B119467SB119468"B119469B119470

SB119471S3119472

•cil5Oi.*

3•ci2l

122414l

44

•*^H/

Membre du Groupe SGS (Societe Generate de Surveillance)

XRAL

Page 3

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE / A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D' ANALYSE /CERTIFICATE OF ANALYSIS

R12389Nforn de la Compagnie/Company : Homestake Exploration Bon de Commande No/ P.O. No: Projet/ Project No : 90763/90764-Date Sounds/ Submitted : Jul 24, 1997 Jul 29, 1997 Attention : Ike Osami

Jto. D'Echantillon AU AU CHK Sample No. PPB PPB

-SB119473 l3B119474 l3B119475 2

J3B119476 <l3B119477 <l

cvf \ ^

Membre du Groupe SGS (Societe Generate de Surveillance)

Page l

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE l A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

"Mom de la Compagnie/Company: Homestake Exploration3on de Cornmande No/ P.O. No:Projet/ Project No : 90763/90764

--Date Soumis/ Submitted : Jun 17, 1997Attention : Ike Osmani

R1201'

Jun 21, 199'

No. D'Echantillon AU "Sample No. PPB

AU CHK AU CHK AU CHK PPB G./T G/T

•.-WL1190017L119002.JL119003

•WL119004•r~?L-119005"- JL119006

- WL119007--WL119008

FL119009-.JL119010-WL119011--1,119012- 'L119013-WL119014-WL119015- L119016- ..L119017(J?KJ 119018

6 L119020BNL119021

- L119023- wL119024WL119025"L119116

L119117VJL119118M.L119119

L119120•V.L119121WL119122

1.119123L119124

WL119125-"^119126

.119127WL119128WL119129

in ^7 *A t \^\ ^" \ ii u ' \x/ IvCtfi. Lft-ici2^^7313 ^ fr^.f-6 _ T^CA^^

2 tOlCcXft Ljk.\dL- ~~<l-3 212'715*765^000' 12.89 12.4527"y ^^^. pj — —— .

4 0 ^ * 06

•^l \A)VvC\ji LjJuj^ '5 48'1•ci1<l26-a<l<li<l"i 3 ^^57

Cert i fie par /' Certified hvre du Groupe SGS (Societe Generate de Surveillance)

Page 2

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE l A DIVISION OF SGS CANADA INC129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL.: (819) 764-9108 FAX: (819) 76-M673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Norn de la Compagnie/Company: Homestake ExplorationBon de Commande No/ P.O. No:Pro jet. X Project No : 90763/90764Date Soumis./ Submitted : Jun 17, 1997Attention : Ike Osmani

R1201"

Jun 21, 1997

No. D'Echantillon AU Sample No. PPB

AU CHK AU CHK AU CHK PPB G/T G/T

WL119130•WL119131 WL119132

-WL119133 JWL119134

-S6WL119135

- iWL119278 U-WL119279 S&WL119280 OWL119281 : .WL119282 S&WL119283 ce,VJL119284 : WL119285 SoWL119286 SfeWLH9287 .~;WL119288 '- WL119289•5BWL119290 SaWL119291 t WL119292

SEWL119294 T-WL119295 5 WL119296 S&WL119297 vfi,WL119298 •WL119299

'WE119303 WLlI?3M"

WL119306 xWL119307

4< l'

<l•

2 ' <l' 2 s

8'l" l/ 2'

6s4'

'

-

U

Membre du Groupe SGS (Sociite Ginirale de Surveillance)

XRALPage l

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SG5 CANADA INC

12ft AVE. R6AL CAOUETTE - C.P 2283 - ROUYN-NORANDA - QUEBEC J8X 5A9 TEL: (819)764-9108 FAX (819) 76*-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Nom de la Compagnie/Company: Homestake ExplorationEon de Commande No/ P.O. No:Projet/ Project No : 90764Date Soumis/ Submitted : Jun 11, 1997Attention : ike Osmani

R11901

Jun 17, 199.7

No. D'Echantillon AU AU CHK Sample No. PPE PFB

WL119051 WL119052 WL119053 WL119054 (3X119055

WL11S059 WL119060 WL119061 WL119052

WL119064 WL119065 'WL119066 -WL119067 WL119068 WL119069 WL119070 WL119071

S&WL119075

WL119077 WL119078 WL119079 WL119080 WL119081 WL119082 WL119083 WL119084 WL119085 WL119086 WL119087 WL119038 WL119089

4'

r

l< < l

l/K l"

' W W^-•o

lertifie par y Certified byMembre du Graupe S68 (Socictt O*n*nl* d* Survcillanc*}

Page l

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE / A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

lioin de la Compagnie Company Eon de Commande No P.O. No Projet/ Project No -Tat e Soumi s ' Submi 11 e d Attention

Homes take Exploration

90753 Jul 0 1997Ike Osmani

R12146

Jul 04, 1997

J-Jo. D'Echantillon AU AU CHK "Sample No. PPB PPB

-3B119238 3B119239 3B119240 3B119241"3B119242 SB119243 SB119244-3B119245 JB119246 3B119247 3B119248"3B119249

1016l

ll

l

106 \

Certi fie par ,/ Certified by :ire du Groupe SGS (Societe Centrale de Surveillance)

Page l

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE i A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C.P. 2283 * ROUYN-NORANDA - QUEBEC J9X 5A9

TEL.: (819) 764-9108 FAX: (819) 764-4673

:ERTIFICAT D'ANALYSExCERTIFICATE OF ANALYSIS

Horn de la Compagnie Company: Eon de Commande No' P.O. No: Projet f Project No : 'Late Soumis/ Submitted : Attention :

Homestake Exploration

# 90763Jun 2 6, 1 997Ike Osmani

R12107

Jul 03, 199"

Mo. D'Echantillon Sample No.

SE1190423B1190433B1190443B119045SB1190463B119047SB1190483B1191693B1191703B1191713E119172SB119173SB119174SB1191753B119178SB119207SB119208.SB1192093B1192103B119212SB1192133B1192143B11921533119216.SB1192173B1192183B1192195B119220SB1 19221SB1192223B119223.3B1192243B119225SB11923233119233'3B1192343B1192353B119236.3B119237

AU -AU CHK PPB PPB

<l<l58 ,, -5^ - . \ V 2 \ -,, } '7 ^. \14.-l5 3i j.

^.11^.12<l<l75 74411•ci<l•- 1 - -r- .9 ' r';,-. ~ —~j s

^1 -,v5 i ; ' " '12 16 ; ^ ' ~t -' - 1^ J j - i9 i" * o i14 /'415<l14 ^^9^

^ertifie par l Certified bydu Groupe SGS (Sociite G^nerale de Surveillance)

XRAL

Page 2

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE / A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

R12107'lorn de la Compagni e- Company: Homestake Exploration Eon de Commande No/ P.O. No: Frojet/ Project No : s 90763"Late Sounds/ Submitted : Jun 26, 1997 Jul 03, 1997 Attention : Ike Osmani

.Mo. D'Echantillon AU AU CHK Sample No. PPB PPB

-3B119350 93B119351 33B119352 6.33119353 5SB119354 -ci3B119355 lSB119356 <l-33119357 <l3B119358 <l3B119359 <l-SB119360 <l3B119361 <l

Membre du Groupe SGS (Societe Generate de Surveillance)

XRAL

pageLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE l A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

R12582Norn de la Compagnie/Company: Homestake Exploration Bon de Commande No/ P.O. No: Projet/ Project No : 90763 '90764Date Soumis/ Submitted : Aug 13, 1997 Aug 19, 1997 Attention : Ike Osmani

No. D'Echantillon AUAU CHK Sample No. PPB PPB

SBC85230 19SBC85231 5SBC85232 2SBC85233 lSBC85234 -ciSBC85235 -ciSBC85236 16SBC85237 -ciSBC85238 .ciSBC85239 -ci -ciSBC85240 ^SBC85241 6

Certifie par f Certifieddu Groupe SGS (Societe G^nerale de Surveillance)

i^~P v\ u) Page l

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE l A DIVISION OF SGS CANADA INC.129 AVE. REAL CAOUETTE - C. P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9

TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

.a Compagnie/Company: Bon de Commanda No/ P.O. No: Projet/ Project No : Date Soumis/ Submitted : Attention :

Homestake Exploration

90^63 '90^64 Aug 14, 1997 Ike Osmani

R12592

Aug 20, 1997

No. D'Echantillon AU AU CHK Sample No. PPB PPB

SBC85243 SBC85244 SBC85245 SBC85246 SBC85247 SBC85248 SBC85249 3BC85250 3BC85251 SBC85252 5BC85253 SBC85254 SBC85255 SBC85256 SBC85257 SBC85258 SBC85259.SBC85260 SBC85261 SBC85262 3BC85263'5BC85264 3BC85265 SBC8B266.SBC85267 3BC85268 SBC85269 SBC85270 SB85324 SB85325

l•ci ^•ci ^•ci•ci•ci

•cil10<l4•ci•ci

-ci•cil <ll5

•ci

<l

rertifie par ,/ Certified bymbre du Groupe SGS (Societe Generate de Surveillance)

XRAL

-s. Page l

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Norn de la Compagnie/Company: Homestake ExplorationBon de Commande No/ P.O. No:Projet/ Project No : 90763-'90764Date Soumis/ Submitted : Aug I B, 1 997Attention : Ike Osmani

R12609

Aug 20, 1997

No. D'Echantillon AU AU CHK Sample No. PPB PPB

SBC85271 SBC85272 SBC85273 SBC85274 SBC85275 SBC85276 SBC85277 SBC85278 SBC85279 SBC85280.SBC85281 SBC85282 SBC85283 SBC85284'SBC85285 SBC85286 SBC85287.SBC85288 SBC85289 SBC85290 SBC85291'SBC85292 SBC85293 SBC85294.SBC85295 SBC85296 SBC85297 SBC85298'SBC85299 SBC85300 SBC85045-SBC85046 SBC85047 SBC85048 SBC85048B"SBC85049 SBC85050 SBC85051.SBC85052

224-ci <l•ci42l3226334

4 3 2 8 2 l l l l 3 3 7 4 4 4 4 3 6

5

3

Certifie par l Certified byMembre du Groupe SGS (Societe G6nerale de Surveillance)

XRAL

Page 2

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. REAL CAOUETTE - C.P. 2283 - ROUYN-NORANDA - QUEBEC J9X 5A9 TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

R12609Norn de la Compagnie/'Company: Homestake Exploration Bon de Commande No/ P.O. No: Projet/ Project No : 90763/90764Date Sounds/ Submitted : Aug 18, 1997 Aug 20, 1997 Attention : Ike Osmani

No. D'Echantillon AUAU CHK Sample No. PPB PPB

SBC85053 16 SBC85054 5 5

Membre du Groupe SGS (Societe Centrale de Surveillance)

SEP-U2-97 TUE 06:52 PH KRAL LABORATORIES

FAX NO. 4164454152

P. 02/07

ZS

K

Z

Z

ZZ

gg

S*

8*

-to•s

^2

0352

* ssj s

f S2& 151^5 55B5 55511 131^5 liW

IZ

Z002

22200

ii**s^ssa

" **^i 55S22

J2SSS 555S5 325

1^

20

25

5—

55t

22

2

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22

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SS ISS

SEP-02-97 TUE 06:52 PH XRAL LABORATORIES

FAX NO, 4164454152P. 03/07

5GZ

Z

Z

Z

Z

Z

Z

Z

M

58S

Mo

3334.4

3

34.8

4

4*4

.34

. 4

3*4

3

3

' ''

'"

ojo

cs

00

02

2

00

2^

2

XRALWork Order: 016702

Element. Method. Det.Lim. Units.

SB 85028 SB 85029 SB 85030 SB 85031 SB 85032

SB 85093 SB 85034 SB 85035 SB 85036 SB 85037

SB 85038 SB 85039 SB 85040 SB 85041 SB 85042

SB 85043 SB 85044 SB 85308 SB 85309 SB 85310

SB 8531l SB 85312 SB 85313 SB 85314 SB 85315

SB 85316 SB 85317 SB 85317B SB 85318 SB 85319

XRAL LaboratoriesA Divfsion of SOS Canada Inc.

Date: 02/09/97 FINAL Pate 3 of

SrXRF?

2ppm139

N.A.N.A.

425N.A.

258N.A.

87N.A.N.A.N.A.N.A.

87124

N.A.N.A.N.A.N.A.

69477

127569189

N.A.N.A.

114N.A.

298111148

YXRF?

2ppm

15N.A.N.A.

8N.A.

25N.A.

10N.A.N.A.N.A.N.A.

528

N.A.N.A.N.A.N.A.

1415151015

N.A.N.A.

15N.A.

273317

ZrXRF7

3ppm

. 47N.A.N.A.

118N.A.

96N.A.

77N.A.N.A.

N.A.N.A.

38109

N.A.N.A.N.A.N.A.

9852

4613461

N.A.N.A.

52N.A.

11710271

NbXRF?

2Ppm^

N.A.N.A.

4N.A.

4N.A.

4N.A.N.A.N.A.N.A.

36

N.A.N.A.N.A.N.A.

63

4243

N.A.N.A.

42N.A.

42S

BsXRF?

20ppm229

N.A.N.A.

297N.A.

132N.A.

264N.A.N.A.N.A.N.A.<20327

N.A.N.A.N.A.N.A.

131139

45385564

N.A.N.A.

319N.A.

164115124

S CO2CHM112CHM114

0.01.*

0.04N.A.N.A.0.20

N.A.0.62

N.A.0.09N.A.N.A.N.A.N.A.0.030.05

N.A.N.A.N.A.N.A.0.020.390,090.080.03

N.A.N.A.0.07N.A.0.190.080.20

0.01*

0.25N.A.N.A.0.09N.A.0.03N.A.0.04N.A.N.A.N.A.N.A.0.170.01

N.A.N.A.N.A.N.A.0.020.020.580.030.07N.A.N.A.

0.02N.A.0.030.010.04

CrICP80

1ppm209151137140170

314[16241265283406201

1780100121977375

1272042202791967375

295272101152177

NlICP80

1ppm135415

10143

8934

1203731

4448

8636465423446

10391

10261

1065529

85115346568

CaICP80

0.5ppm67.338.947.440.6

8.244.444.0

101105

68.4

114115

26.529.9151

66.456.091.922.6277133

20.449.063.09.2

71.753.170.765.2142

ZnICP80

O.Sppm57.554.661.236.348.866.349.052.814.736.540.6164

58.995.5406206298125

78.795.662.472.785.0104

51.9

68.083.1107112

87.2

AsICP80

3ppmO

4o<3

3

O4

^.300

0

o22

74

^3O<3

9

54

<3O

44

OOO

Mo AcICP80 ICP80

1 0.2ppm ppm

6 ^.27 ^.22 -C0.24 *:0.25 *C0.23 ^.24 -C0.2

H -COJli *:0.210 -C 0.27 -C0.22 ^.24 ••C 0.2

3 -CO 210 (K34 -*:0.25 <0.24 2.25 -C0.23 ^24 *C0.26 ^.27 <0.22 ^.25 *CO,29 ^.24 *C0.2

CD

CD

enCO

co

g

MwrtMT of DM SOS Group (SodM Gfafota * SuwrtMw*)

XRALWork Order: 016702

Element. Mefbod. DetUnu Units,

SB 85320 SB 85321 SB 85322 SB 85323 SBC 85214SBC 85215 SBC 85216 SBC 85217 SBC 85218 SBC 85219

SBC 85220 SBC 85221 SBC 85222 SBC 85223 SBC 85224

SBC 85225 SBC 85226 SBC 85227 SBC 85228 SBC 85229

SBC 85242*Dop SB 85028*Dup SB 85040*Dup SB 85315*Dup SBC 85216

*Dup SBC 85228

XRAL LaboratoriesA DMiIon of SQS Canada Inc.

Bate: 02/09/97

CO-J

FINAL 4 of 6

Sr XRF?

2 ppm414 259

N.A. 57

244169 689 642

N.A. N.A.

118 116

N.A. 104

N.A.N.A.

107 N.A.

8 N.A.N.A.

137 86

N.A. 688

8

Y XRF?

2 ppm

18 21

N.A. 9 89

^ ^

N.A. N.A.

12 15

N.A. 12

N.A.N.A.

10 N.A.

5 N.A.

N.A. 15 6

N.A. ^

6

Zr XRF?

3 ppm

94 104

N.A. 38 9474

100 111

N.A. N.A.

52 55

N.A. 59

N.A.N.A.

54 N.A.

27 N.A.

N.A. 49 36

N.A. 10428

•ra

Nb XRF?

2 ppm

33

N.A. ^

23 3 3

N.A. N.A.

3 ^

N.A. 3

N.A.N.A.

2 N.A. O

N.A.

N.A. ^

2 N.A.

3^

! Mantel

Ba S CO2 XRF7CHM112CHM114

20 0.01 0.01 ppm tt fc411652

N.A. 31

23893

690 450

N.A, NJL

5554

N.A. 39

N.A.N.A, <20

N.A. <20

N.A.

N.A. 226

<•to N.A.

685^

rftiMSosa

0.07 0.31

N.A. 0.21 0.190.98 0.04 0.07 N.A. N.A.0.60 0.74

N.A. 0.44

N.A.RA. 0.22

N.A. 1.31

N.A.

N.A. 0.05 0.03

N.A. 0.041.34

mvttooU

0.01 ^.01 N.A. 0.01 0.07

0.01 0.02 0.01

N.A. N.A.

^.01 •CO.OI N.A. 0.01

N.A.N.A. 0.01

N.A. 0.01

N.A.

N.A, 0.27 0.16

N.A. 0.020.01

*0Mrited

Cr 1CP80

1 ppm

93 99 78

1130 266

647 65 68

604 463

182 152768 142 110154 142 207

1670 659216 184

1670 75 65

1470

tSurwWMo

NI ICF80

1ppm

41 38 34

444 154300

25 23 91

30961 62

445 71 50

117 53

135 587 257

79 130 895 30 26

553

•f

CuICP80

0.5 PPm13.3 48.0 62.8 23.4 26.892.2

7.1 6.6 134 610

94.7 105 613

91.6 56.5227

79.7 29.8 85.2 394148

62.4 25.6 9.8 8.2

81.4

Zn ICP80

0.5 ppm75.4 94.5 101

55.2 36.959.2 43.9 41.9 218

3680

152 158

1270 145 126546

87.5 100 240

2910

130 60.7 60.9 56.9 49.4

227

AsICP80

3 ppmOO

5 OO

6 3 7

O OO O Ooo

3 6

O O

8O O O

3 6

O

en CO

Mo A* -a ICP80 ICP8J5 a

1 0.2 W™ ppm g

5 *C0.2 r" S ^.2 ^ 4 *:o.2 S 1 *:0.2 g 3 K:o.2 -E53 *C0.2 2 5 *:0.2 E3 5 *C0.2 7 *C0.2 8 -C0.2

2 -C0.2 3 .C0.2 5 *:0.2 m 3 *C0.2 i

12 ^.2 ^5 <0.2 4 *C0.2 5 <0.2 3 <0.2 8 *C0.2

11 <0.2 6 ^.2 2 <0.2 6 <0.2 6 *:0.2

3 <0.2

P**.O3*i.J^enAk

S

r0C3enCD ^J

XRALWork Order: 016702

XRAL LaboratoriesA Division of SOS Canada fnc.

Date: 02/09/97

CO

Element. Method. Det.Lta. Units.

SB 85028 SB 85029 SB 85030 SB 85031 SB 85032

SB 85033 SB 85034 SB 85035 SB 85036 SB 85037

SB 85038 SB 85039 SB 85040 SB 85041 SB 85042

SB 85043 SB 85044 SB 85308 SB 85309 SB 85310

SB 85311 SB 85312 SB 85313 SB 85314 SB 85315

SB 85316 SB 85317 SB 85317B SB 85318 SB 85319

FINAL 5 tt 6

SbICP80

5ppm•CS^0O•C5

C5^^OOKS0•C5^<5^^<5<5^<5^^^O^<5<5<5

BaICP80

1ppm192168526317124102622190508

96336

4525

2332291589766

11210440

413473

6751226415712371

112

WICP80

10ppm•ao00•CIO^0•CIO

-CIO*cio*C10^0•CIO

•CIO*C10oo•cio00

00•cio•CIO•cio^0•CIO^00000*:io00•CIO•CIOXlOoo

PbICP80

2ppm

. 1717211520

1816152835

4129182530

3023252223

1619182617

1726222419

TeAAH3

0.1ppm

•CO.l0.10.1

*C0.1KiO.l*:0.1•CO.l•CO.l•co.i

0.1

0.10.20,1

CO.l0.10.1•co.i•co.i

•C0.10.2

•CO.!*:o.i<0.1co.i•C0.1

<0.1<O.I<0.1•co.i<0.1

en -a

OJ

O O3

Mwnter of KM SOS Group (Socttt* Gfetafa dt SumMm*)

SEP-02-97 TUE 06:54 PH XRAL LABORATORIES

FAX NO, 4164454152

P. 07/07

SB'ssel

fi gi—

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10*010*010 "o

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SEP-02-97 TUE 08:39 AH KRAL LABORATORIES

. -

*FAX NO.

4164454152P. 02/04

p* 2823 883 820

22®2

22

22

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S*

22220

12*o

022;o

2

222:2

0

sjfc'rf

22:22 2222

MS

52220

4432

2*

2

2222-

22-

02202 22220 22®

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2^

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2222

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XRALWork Order: 016781

XRAL LaboratoriesA Division of SOS Canada hw.

Date: 30/08/97 FINAL Pip 2 of 3

Element. Method. DetLlm. Unite.

SBC83230 SBC8S231 SBC85232 SBC83233 SBC85234

SBC85235 SBC85236 SBC85237 SBC83238 SBC85239

SBC8S240 SBC85241 *DupSBC85230

SrXRF?

2ppm105

N.A.N.A.

324N.A.

N.A.N.A.N.A.N.A.

192

N.A.N.A.

105

YXRF?

2ppm

12N.A,N.A.

11N.A.

N.A.N.A,N.A.N.A.

11

N.A.N.A.

12

ZrXRF?

3ppm

SIN.A.N.A.

104N.A.N.A.N.A.N.A.N.A.

83

N.A.N.A.

53

NbXRF?

2ppm

2NA.N.A.

4N.A.

N.A.N.A.N.A.N.A.

4

N.A.N.A.

3

BaXRF?

24ppm

39N.A.N.A.

45N.A.N.A.N.A.N.A.N.A,

188

N.A.N.A.

38

CrICP80

Ippm147150154215704374207

1110612490

1050428221

NiICP80

1ppm

61445857

15712257

3382212111819062

CuICP80

•.5ppm84.533.745.326.9182

63.330.6342304328235115

87.8

ZnICP80

0.5ppm101

82.7151

40.3156

66.5252666

1060420163

97.998.6

AsICP80

3ppmOOo0ooo0ooooo

MoICP80

1ppm

35S*:i4

25394

393

AaICP80

•.2ppm

•C0.2*C0.2<0.2<0.2<0.24C0.2<0.2<0.2<0^<0.2•COJ<0.2<0.2

SbICF80

5ppm<5<5<5^<5<5<5<5O^^^^

BaICP80

1ppm

7065

11250

3863972

10923218112011660

CO

CO CD

4^

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CO

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SEP-02-97 TUE 08:40 AM KRAL LABORATORIES

FAX NO, 4164454152

P. 04/04

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FAX NO, 4164454152

P, 02/07

i* 44m 444**

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44444 44444

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44444 44444

4443-2-ZZ 222ZZ 2222Z ZZ222 ZZZZ2 ZZZ--

9Z02J2 ZZZZZ ZZZZZ 2Z222 Z2222

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AUG-30-97 SAT 12:39 PH KRAL LABORATORIES

FAX NO, 4164454152

P. 03/07

•B" l -a

S

s g**

•sM3**

•g*

022

4*

!l!-

-22

1*01

* * *

XRALWork Order: 016811

Element. Method. Det.L(m. Units.

SBC85243 SBC85244 SBC8S24S SBC85246 SBC85247

SBC85248 SBC85249 SBC85250 SBC852S1 SBC852S2

SBC8S2S3 SBC8S254 SBC8525S SBC85256 SBC85257

SBC85258 5BC8S259 SBC85260 SBC85261 SBC85262

SBC8S263 SBC8S264 SBC85265 SBC85266 SBC85267

SBC85268SBC8S269SBC85270SB8S324SB85325

XRAL LaboratoriesA OivMon of SOS Canada Inc.

Date: 30/08/97 FINAL Page 3 of 6

Sr XRF?

2ppm

64N.A.

84N.A.N.A.RA.N.A.N.A.N.A.N.A.RA.N.A.N.A.RA.RA.N.A.N.A.N.A.N.A.N.A.N.A.RA.RA.RA.N.A.RA.RA.NA.

206144

Y XRF?

2PPm

22N.A.

22N.A.N.A.N.A.RA.RA.RA.N.A.RA.RA.N.A.N.A.N.A.N.A.N.A.N.A.RA.RA.N.A.N.A.RA.N.A.RA.NARA!RA.

1611

Zr XRF?

3ppm

81N.A.

83RA.N.A.N.A.N.A.NA.N.A.N.A.N.A.NA.RA.RA.RA.N.A.N.A.RA.RA.N.A,N.A.RA.N.A.N.A.RA.RA.N.A.N.A.

6050

NbXRF?

2ppm

4RA.

5RA.RA.

N.A.N.A.RA.N.A.N.A.

N.A.RA.N.A.NA.N.A.

N.A.RA.N.A.N.A.RA.

N.A.N.A.RA.RA.NA.

RA.RA.N.A.

33

Ba XRF?

20ppm269

RA.68

RA.N.A.N.A.N.A.RA.N.A.N.A.RA.N.A.N.A.N.A.RA.RA.N.A.RA.RA.RA.N.A.RA.RA.N.A.N.A.RA.RA.N.A.

180216

Cr ICP80

1ppm27929530337093

29528397969073

127808873

10989

211159279264183696760678564

183208

Nl ICP80

1ppm14114114912964

1351265762274540443222273163585445582935376528869696

Cu ICP80

0,5ppm54.067.064.191.297.298.238.078.5156

42.2115

72.857.1124

69.592.775.4187171

81.8148157

65.069.772.7

99116165

70.581.2

ZnICP80 1

0.5ppm101100120

90.0147

82.997.5

105466309331309166452293410271

47.021.934.913.630.7260191217157114127

67.267.8

As [CP80

3ppmO<300O

45

<37

OO<3O<311O

5<3O

4OO

40

O0oo

Ho ICF80

1ppm

54344

65484

4744475

29151110105

58545323

icm0.2

ypm^Q 2•C0.2•C0.2^.2•C0.2

"C0.2<0 2

0.2•C0.2*C0.2

OJ0.2<0.2•^.2•C0.2

0.3<0 2•C 0.2

*:o.2-C 0.2

^C0.2•C0.2*:o.24U2•S 0.2^2^2

Sb ICP80

5ppm^O^^^O^O^^O^^

^o^<5<5<5O^<5<5<5O

BaICP80

1ppm20525532020

256629

309147

203184362510163

15193

287321249

285362153109151

188139120149177

30-97 SAT 12

3

tn.c*

o J*.

MttMtar of KM SOS Group (Socttt* GMufo fr SuntOhnc^

AUG-30-97 SAT 12:40 PH XRAL LABORATORIES

FAX NO. 4164454152

P. 05/07

VV

V

g

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VV

vvv

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22

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22

5E2

22

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AUG-30-97 SAT 12:41 PH XRAL LABORATORIES

FAX NO. 4164454152

P. 06/07

•s

zzzzz zzzzz

zzzz'z zzzzz

l

. 02022 ZZ222 ZZ222 ZZZZZ ZZZZZ

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22222 22222 22222 22222 22222 22222

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vvvvv vvvvv vvvvv vvvvv

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XRALWort Order: 016811

XRAL LaboratoriesA Division of SOS CMMda Inc.

Date: 30/08/97 FINAL Fife 6 of

CO

TCD-J

CO

no

Element. Method. Drt.EJm. Units.

WICP80

10PJHB

*DnpSBC83243*DnpSBC85255*Dup SBC8S267

•cio

PbICP80

2ppm

172119

T* S C02AAH3 CHM112 CHM114

0.1 *.01 0.01

•co. i0.12 N.A. N.A.

0.02 N.A.N.A.

-n

en

en ro

MMibHT at A* 808 Qnoifx (SocMM Gonorate * SurnUwiMt

XRALWork Order: 015952

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 24/07/97 FINALElement. Method. Del.Lim. Units.

SB 119238 SB 119239 SB119240 SB11924I SB 11 9142

SB 119243 SB 119244 SB 119245 SBI19246 SBI19247

SB119-248 SB119249 *DupSBlI923S

Pige l of J

SI02 AI2O3 CaO XRF102 XRFI02 XRF102

0.01 0.01 9.01 Sum AbXRF102 XRF102

0.01 235.9n.a. n.a. n.a. n.a.

n.a. na

53.2 n.a.n.a.

n.a. 65.9 35.9

16 o.0.n. n.

n. n. 14. n.a n.a

n.aJ5.( 16.(

8 4.23 n.a. n.*. n.a. n.a.

o.a. n.a.

0 10.5D. a. n.a.

a. a J 1.75 * 4.22

18.5n.a. n.a. n.a. n.a.

a. a. n.A.

^335 n.a. n.a.

04.rsi?ig;5

0.75n.a. n.a. n.a. n.a.

n.a.n.a.

2.67 o.a. n.a.

n.a. 4.51 0.74

0.16 n.a. n.a. n.a. n.a.

n.a.n.a.

0.16n.a. n.A.n.a. 350 0.15

16.3 n.a. n.a. n.a. n.a.

n.a. n.a.11.5 n.a. n.a.

o. a. 3.78 16.4

0.19 n.a, n.a. n.a. n.a.n.a, aa.

0.27 n.a. n.a.

n.a. 0.05 0.19

0.73 n.a. n.a. n.a.n.a,n.a. n.a.

0.99 n.a. n.a.n.a.

0.52 0.72

0.09 n.a. n.a. n.a. n.a.n.a. n.a

0.10 n.a. n.a.n.a.

0.28 009

'V

0.08 n.a. n.a. n.a. n.a.

n.a.n.a. 0.09 n.a. n.a.n.a. 0.02 0.08

TIP

6.35 n.a. n.a. n.a.n.a.

o. a. n.a.

0.55 n.a. n.a.

n.a. 2.00 6.25

•*

1002 n.a. n.a.n.a. n.a.

n.a. n.a.

99.4 n.a. n.a.n.a.

99.7 100.1

ppm

16 oa. n.a. n.a.n.a.n.a. na.

7 n.a. n.a.

n.a. 109

15

ro.fc.iCO--J

CDon

:x

SlmCO

f*.COft. .c. tn.Ca.

tn

MWibW M (hi SOS Groiip (gfiflW Cerite

oro

XRALWork Order: 015952

XRAL LaboratoriesA Division o* SGS Canada Inc.

Date: 24/07/97 FINAL 2 at 3

i ro

ro

Element. Method. Del.Llm.fnlfj.

ST Y Zr Mb Ba CrXRF101 XRF102 X RF 102 XRFI02 XRF102 ICP80

l 2 2 2 20 lppm ppm ppm ppm ppm ppm

SB119238 "K SBI 19239 SBU9240 Vi SBI 1924 U SBI 19242 .

SBI 19243 r '. SB 119244 ";, SB 119245 SBI 19246 lo SBI 19247 ^

SBI 19248 SB H 9249 "Pup SB 119238

67 rt. a. n.a. n.t. n.a.

n.a. n.a. 113 n.a. n.a.

n.a.57266

16 n.a.n.a. n.a. n.a.

n.a. n.a. 31

n.a. n.a.

n.a.2517

122 Q.a. n.a. n.a. n.a.

n.a. n a.97

n.a. n.a.

n.a. 209 122

8 n.a.a.a. n.a, n.a.

n.a.n.a.

5n.a. D.a.

n.a.117

150 n.a.n.a. n.a. D.a.

n.a. n.a. 154 n.a. a.a.

n.a.1080157

2611030.312872271

159794313246299

82132257

NlICP80

1ppm

2021241039034

CMic wo • sppm

<05137287132

57.5

Zn ICP90

OSppm

12445.11750

VJI6122

Aaicrao3

ppmOOO<3O

Ma ICP80

1Ppm

26343

1CP80 0.2

npm

0.20.40.30.2

<0.2

Sb ICPSO

Sppm

<5<5

,;5<S

Ba ICP80

1ppm

14125115237

117

en-o rr

3C

ID?

1 ——

CD

3?

46 187- 162 38 94

51.6 271- 114

69.3 64.3

91.5 226

- 1 1 1— 65.2 94.6

AAAAA ww ww w

199 -C0.5 125

<3 O 8

3

0.2 0.3

•^0.2

<0.2

•c:o.2 <0.2 <0.2

<5 <5

^ <5

<S <5

1239194

103J92

471190103

mCO

CD

•C-en

tn ro

Mimbst a t the SOS Grcup ISocMtA G4n4r*I* tf* SurwUlancw)

CD to

XRALWork Order: 015952

XRAL LaboratoriesA Dlvidon of SGS Can tufa Inc.

Date: 24/07/97 FINAL hg* 3 of 3

Element. Method.rw.Lim.Ute.

SB 119238 SB) 192)9 SBI 19240 SBI 19241 SB 119242

SB 119243 SB 119244 SBI 19245 SB 119246 SB 119247

SB 119248 SBI 19249 •Dup SB 119238

wICP80

10ppm

CIO•CIO•cioCIO•C 10

CIO•CIO•CIO

17CIO

CIOCIO< 10

PbICPtO

2ppm

1714371514

1432121815

411612

T*AAH3

0.1pom

<0 10.4030.30.2

cO.I0.30.10.3O.I

0.90.2

•CO.l

S CO2CHM112CHM114

0.01*

C 0.01A. A.D. a.n.a.n.a.

n.a.n.a.

0.13n.a.n.a.

n.a.0.49

•CO.OI

0.01*

0.03n.a.n.a.n.a.n.a.

D. a.n.a.

0.05n.a.n.a.

a. a.0.130.02

iro .e-co

ro oCD-o

x?0x-

COo

oPO

o

anj^. en

en ro

McmtMr of Ih* SGS Group (JocltW G*n4rila tfa Survclliaoo)

XRALWork Order: 015881

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 22/07/97 FINAL Paje l of 6

Element Method. DetLlm. Units.

SB 119042 SB 119043 SB 119044 SB1190+5 SB119046

SB119047 SB 119048 SB119169 SBH9170 SB119171

SB119172 SB119173 SB119174 SB119175 SB119207

SB119208 SB 119209 SB119210 SB119212 SB119213

SB119214 SB119215 SB 119216 SB119217 SB 119218

SB119219 SB119220 SB119221 SB119222 SB119223

S1O2 AI2O3 CaO MgO Na2O K2O R2O3 MnO TfO2 P2O5 Cr2O3 LOI Sum Rb XRF102 XRF102 XRF102 XMT02 XRP102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102

0.01*53.765.960.849.850.9

42.269.857.966.552.9

45.547.154.4n.a.52.548.440.562.351.354.1

47.5n.a.51.0n.a.n.a.n.a.B. a.B.a.n.a.n.a.

0.01Ik

13.915.414.514.516.2

4.8314.515.615.413.9

8.379.0214.4n.a.16.6

7.554.6413.515.115.7

7.08n.a.14.5n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01tt

8.273.675.907.146.84

1.673.546.692.438.36

7.579.848.34n.a.11.7

10.12.452.7714.06.98

10.3n.a.13.1n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01tt

4.422.344.493.795.73

30.30.883.362.704.77

20.717.56.35n.a.

4.9218.132.07.725.596.2018.5n.a.6.60n.a.n.a.n.a.n.a.n.a.n.a.o. a.

0.01*

3.404.273.981.442.87

0.132.581.665.682.81

0.380.834. tOn.a.2.50

0.740.124.431.084.95

0.61n.a.1.21n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01tt

0.292.661.030.611.320.023.511.890.800.37

0.030.100.34n.a.0.150.09

<0 011.090.150.34

0.06n.a.

0.09n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01*

13.64.167.0520.112.8

10.42.389.633.8514.3

11.711.98.99n.a.

9.70

11.49.865.199.988.72

11.4n.a.11.3n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01tt

0.160.050.130.290.24

0.150.030.160.050.31

0.180.210.23n.a.0.22

0.190.140.070.250.23

0.20n.a.0.30n.a.n.a.a. a.n.a.n.a.n.a.n.a.

0.01tt

1.610.570.591.171.35

0.240.270.750.511.71

0,530.521.14n.a.

0.770.240.220.470.690.74

0.37n.a.0.62n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01tt

0.100.250.060.100.12

0.010.070.050.250.09

0.030.040.12n.a.0.05

0.010.010,150.040.05

0.02n.a.

0.04n.a.n.a.n.a.n.a.n.a.n.a.n.a.

0.01*

0.020.020.080.050.08

0.280.020.060.020.02

0.330.270.03n.a.0.06

0.210.290.070.060.06

0.37n.a.0.08n.a.n.a.n.a.n.a.n.an.a.n.a.

0.01fc

0.650.701.101.201.30

10.20.902.451.900.75

4.452.450.90n.a.0.50

2.1510.12.401.051.152.85n.a.0.80n.a.n.a.n.a.n.a.n.a.n.a.0.1.

0.01tt

100.1100.399.8

100.399.8

100.498.6

100.3100.3100.3

99.799.799.4n.a.99.799.1

100.3100.399.399.399.3n.a.99.7n.a.n.a.n.a.n.a.n.a.n.a.n.a.

2ppm

61012324532250643919

78

12n.a.

4

612667

14

4n.a.

8n.a.n.a.n.a.n.a.n.a.n.a.n.a.

FSCO

CO

CO

m to

CD.c*en -e*enro

M*nb*r of to SOS Group (Sod** CUnfc tk ft Swvelflmctl

ro.e-

XRALWork Order: 01S881

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 22/07/97 FINAL Kip 2 of fi

Element. Method. DetXltn. Units.

SB119224 SB 119225 SB119232 SB119233 SB119234SB 119235 SB119236 SB119237 SB119178 SB 119350SBH93S1 SB119352 SB 119353 SB 119354 SB119355SB119356 SB119357 SB 119358 SB119359 SB119360

SB119361*DupSBl 19042*DupSBl 19174*DapSBl 19218*DupSBl 19236*DupSBl 19359

CO

S102XRF102

0.01ftn.a.n.a.

49.563.961.762.545.251.371.049.152.354.551.356.472.7

62.159.448.874.444.349.153.854.5n.a.

45.1

AI2O3XRF102

0.01ftn.a.n.a.12.815.014.114.39.8114.612.812.114.513.715.114.014.514.514.020.714.36.3712.414.014.5n.a.9.88

CaOXRF102 J

0.01ft

n,a..n.a.8.743.196.074.238.4911.34.329.87

8.129.9212.56.481.634.576.749.390.999.159.948.248.35a.a.8.55

MgO[RF102

0.01ft

n.i.n.a.4.873.294.14

3.9418.33.831.319.74

7.105.637.104.300.284.295.904.360.3022.04.584.446.38n.a.18.4

Na2OXRF102

0.01ftn.a,n.a,1.676.784.65

4.520.960.795.952.71

3.602.701.103.424.464.213.951.874.750.312.133.404.09n.a.

0.98

K2OXRF102

0.01ft

n.a.n.a.0.170.440.672.120.101.470.020.69

0.070.190.210.273.56

2.940.851.823.450.06

1.020.290.36n.a.0.11

Fe2O3XRF102

0.01ft

n.a.n.a.19.55.416.065.2612.213.23.5812.711.211.510.411.91.825.227.549.751.1410.517.413.69.00n.a.12.3

MnOXRF102

0.01ft

n.a.n.a.

0.550.080.110.080.200.180.030.19

0.310.290.250.220.020.070.130.14

-CO.Ol0.16

0.430.160.23n.a.0.20

T10ZXRF102

0.01ft

n.a.n.a.1.470.570.51

0.600.581.230.290.881.271.000.721.630.200.580.500.690.11OJO

*

1.411.641.16n.a.0.57

P2OSXRF102

0.01ftn.a.n.a.0.090.330.05

0.360.050.130.070.320.150.120.050.120.060.360.050.040.030.020.100.110.12n.a.0.05

Cr2O3XJRF102

0.01ft

n.a.n.a.0.020.030.070.030.280.040.020.080.020.080.050.020.020.030.130.120.020.32

0.020.020.03n.a.

0.28

LO1XRF102

0.01ft

n.a.n.a.

0.451.301.151.553.452.000.851.650.450.550.751.300.850.800.752.050.456.300.850.550.90n.a.3.20

SumXRF102

0.01ft

n.a.n.a.

100.0100.499.399,799.7

100.2100.3100.299.2

100.299.4

100.2100.2

99.9100.199.9

100.199.899.4

100.399.7n.a.99.6

RbXRP102

2ppntn.i.n.a.

7161534114817^

2148

1158226689310

247

10n.a.

14

CO

COJ,.SE

sx:S?r-r~SoS—3

SS3

-n

g*.e*men.c*en ro

74.5 14.3 1.01 0.31 4.73 3.42 1.15 0.11 0.03 0.02 0.35 100.0 98

TJ

ro

SMunber of the SGS Group (SocUt* Gtnfato de SurwflteriMl

XRALWork Order; 015881

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 22/07/97 FINAL P*gB 3 of 6

Element. Method, Det.Llm. Units.

SB119042 SB119M3 SB119044 SB119M5 SB119046SB119047 SB 119048 SB119169 SB119170 SB119171SB119172 SB 119173 SB119174 SB119175 SB119207SB119208 SB119209 SB119210 SB119212 SB 119213SB119214 SBH9215 SB119216 SB 119217 SB119218SB119219 SB119220 SB119221 SB119222 SB119223

Sr Y Zr Nb Ba XRF102 XRF102 XRF101 XRF102 XRF102

2ppm

9398824410111440

2481724401442044

174B. a.130

1824

6861381S1

27B. a.110n.a.n.a.n.a.n.a.n.a.n.a.n.a.

2ppm

3618123529

173

221644

152226

n.a.22

104

192217

13n.a.

24n.a.n.a.n.a.n.a.n.a.n.a.n.a.

2ppm11417010476

126

3512675

192113

4748

121n.a.

693731

1475691

41n.a.

51n.a.a. a.B. a.n.a.a.a.B.a,B.a.

2ppm

38334

1374

106

574

n.a.579

1234

4n.a.

4n.a.n.a.n.a.n.a.n.a.n.a.n.a.

20ppm17287732119940373

424613251206

6776

174n.a.1725669

659109150

58n.a.

73o. a.n.a.n.a.n.a.n.a.n.a.n.a.

Cu ICP70

0.5ppm39.549.538.2110

22.943.63.21169.6

52.411.958.648.040.698.43.48.3

12.5131

42.4

40.980.280.520.2104176

32.0236

98.4124

Zn ICP70

0.5ppm12.455.742.625.540.527.232.333.537.220.213.111.010.919.65.4

12.110.442.412.26.8

10.327.810.923.633.012.911.1124025.869.2

As ICP70

3ppmOOooooooooooo0oo0oooo'oooooooo

MoICP701

ppm3

45552

<l3432

O•ci2121<l432

1•SI21232732

ICF7?0.2

ppm•C0.2*:0.2*:0.2

0.3*C0.2O.2O.20.2O.2^.2

O.20.2O.2

0.4O.2

0.20.2O.2O.2O.2O.2O.2O.20.2O.2

0.20.20.2

O.20.3

Sfa ICP70

5ppm^^^^^

O0^OOooo

^<5<5<S

^<5<5<5<5

^<5<5<5

^5

Ba ICP70

1ppm

18758132

1701215

2381814

39

1611

812

1849

101

149

2540219

238

21

Pb ICP70

2ppm

^^

4^^^^^^<2<2<2^

2<2<2<2

211^<2<2^<2<2<2<2

5^

4

W ICP70

10ppm

'^10

<10<10oo<10<10<10<10*ao<10

<10<10<10<10<10<10<10<10*no<10<10<10<10-CIO-CIO••cio•cio00

32•sio

Mwnbmr of DM SGS Group (SocUU atntote d* Swvaffimo*)

Kl5?ilLl XRAL Laboratories™*****—— A DivMon of S6S Canada Inc.

Work Order: 015881 Date: 22/07/97

Element.Method.Det.Llm.Units.

SB119224SB1 19225SB1 19232SB1 19233SB1 19234

SB1 19235SB1 19236SB119237SB1 19178SB1 19350

SB119351SB1 19352SB1 19353SB1 19354SB 119355

SB1 19356SB1 19357SB119358SB1 19359SB1 19360

SB1 19361*DupSBl 19042*DupSBl 19174*DupSBU9218*DupSBl 19236

Sr XRF102

2ppmn.a.o.a.

91260295

83653

172214310

1219389

164335

1050291198347

50

14794

170n.a.

56

Y XRF102

2ppmn.a.n.a.

312210181836

32928292734

3

2313155

14

393326

n.a.20

Zr XRF102

2ppmn.a.n.a.

84212106

1745193

153112

1169758

122119

1639364

13535

89114119n.a.

51

Nb XRF10Z

2ppm

n.a.n.a.

293

75376

33458

72477

433

n.a.6

FINAL

BMXRF102

20ppmn.a.n.a.123142290

101091

37667

417

153157126157486

108034272036660

265180170n.a.

85

Cu ICP70

0.5ppm229266

67.324.758.5

21.43.61228.3

62.8

53.951.586.233.68.0

7.015.418.22.4

60.8

61.037.847.11004.0

Zn ICP70

0.5ppm25817:230.841.717.4

31.316.548.49.2

32.5

9.48.05.5

17.010.0

38.019.820.710.818.9

33.713.111.433.720.2

As ICF70

3ppmOOo00oo0ooooooooo<3oo

oo<3<3O

Ho ICP70

1ppm

23324

4•c:!541

21136

3325

<l

2322

-Ci

ICPT!0.2

ppm0.40.3

<0.20.2

-C0.2

*C0.2<0 2

0.2•C0.2*C0.2

•C0.2•^0.2<0.2<0.2-C 0.2

•s: 0.2•C 0.2-C 0.2<02

0.2

^Q2^0.2<0.2<0.2^.2

Pip 4 of 6

Sb Ba ICP70 ICP70

5 1ppm ppm^ 12O 120 9^ 6^ 180 20^ 5O 1110 6^ 22

^ 4O 7O 20^ 320 38

O 55^ 117O 129^ 9^ 8

O 37^ 1 8^ 16O 39^ 6

Fb W ICP70 ICF70

2 10ppm ppm

6 < lO4 -CIO

O x: 104 *S10

^ -c 10^ ^0

8 < lQ<2 ^0

2 ^042 *;[()<2 <10<2 <lO<2 <10

6 *:10<2 <10<2 <10<2 <10

6 <102 < lO

6 < 10<2 <10<2 ^10<2 ^10<2 ^0

cc pr c

Pc

4

B

2e.fE

Eii-E

^^c

14C4C4

P

•DupSBl 19359 350 131 369 2.4 11.6 <3 <0.2

MwnlMr of theSGS Group (SocUtt Qtnintt da SunraDfane*}

XRALWork Order: 015881

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 22/07/97

Element. Method. Det.Um. Units.

SB119042 SB119043 SB119044 SB119045 SB119046

SB119047 SB119048 SB119169 SB119170 SB119171

SB119172 SB119173 SB119174 SB119175 SB119207

SB11920S SB119209 SB 119210 SB119212 5B119213

SB 119214 SB119215 SB119216 SB119217 SB119218

SB119219 SB119220 SB119221 SB119222 SB 119223

Te S CO2AAH3 CHM112 CHM114

0.1 0.01 0.01ppm % K

0.1

•CO. l

0.1

0.1

o!i<0.1 <0.1

0.7

Oil 0.3

0.066.330.130.190.02

0.21

*1.32 0.13 0.16

0.01 0.04 0.03 n.a. 0.04

O.OS 0.03 0.06 0.02

0.02 n.a. 0.03 n.a. n.a.n.a. n.a. n.a. n.a. n.a.

032 0.04 0.04

<0.01 0.04

2.020.010.200.010.02

0.02 0.02 0.02 n.a. 0.02

0.030.700.160.040.01

0.33 n.a.

0.10 n.a. n.a.n.a. o.a. n.a. o.a. n.a.

FINAL S of 6

ficc

cc

oJi .C O

rvJS

Mwnber of du SGS Group (SocUl* Qwtfote d* SurvaHhno*)

XRALWork Order: 015881

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 22/07/97 FINAL Fags 6 of 6

fiidtt col*Method,Det.Lim.Units.

SB 119224SB1 19225SB 119232SB1 19233SB 1192345B1 19235SB1 19236SB1 19237SB1 19178SB H 9350SB119351SB119352SB1 19353SB119354SB 11 9355SB1 19356SB 11 9357SB1193S8SB 119359SB1 19360SB1 19361*DupSBl 19042*Dup SB 119174*DupSBl 19218*Dup SB 119236

TeAAH3

0.1ppm0.10.1

<0.1<0 10.1O.Io!i<0 1oilO.IO.IiCO i<0.1<0.1<O.I<0.1<0.1<0.1<0 1<O.I

<01o!i<0.1o.iO.I

s CO2CHM112CHM114

0.01*n.a.n.a.0.110.160.090.05

<0.010.120.080.120.010.030.040.140.080.020.040.03

<0.010.130.120.060.03n.a.0.01

0.01%n.a.n.a.0.050.020.340.090.020.790.020.05

O 010!250.190.01

O.010.08

•O.Ol0.030.022.33

0.120.33

0.01n.a.

0.03*DupSBl 19359 O.I O.01 O.01

Mwnbw of th* SOS Group {SocUt* 6fetfrata 4* Sufwlflmctl

XRALWork Order: 016810

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL Pate l of 6

Element. Method. Det.Um. Units.

SBC85271 SBC85272 SBC8S273 SBC85274 SBC85275

SBC85276 SBC85277 SBC85278 SBC85279 SBC85280

SBC85281 SBC85282 SBC85283 SBC85284 SBC85285

SBC85286 SBC8S287 SBC85288 SBC8S289 SBC85290

SBC85291 SBC8S292 SBC85293 SBC85294 SBC8529S

SBC85296 SBC85297 SBC85298 SBC85299 SBC85300

SiO2 A12O3 CaO MgO Na2O K2O Fe2O3 MnO T1O2 P2O5 Cr2O3 LOI Sum XRF1QO XRF100 XRF100 XRF100 XRF100 XRF 100 XRF100 XRF100 XRF100 XRF100 XRF100 XRF100 XRF100

0.01ft

59.3N-A.N.A.N.A.N.A.

51.3N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.RA.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01*

16.0N.A.N.A.N.A.N.A.

12.9N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01.*.

3.49N.A.N.A.N.A.N.A.

6.00N.A.N.A.N.A.N.A.

N.A.N.A.N.A,N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01ft

2.52N.A.N.A.N.A.N.A.

3.81N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01ft

6.18N.A.N.A.N.A.N.A.

3.98N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01ft

0,84N.A.N.A.N.A.N.A.

0.97N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.RA.N.A.N.A.N.A.

0.01ft

8.46N.A.N.A.N.A.N.A.

15.8N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A,

0.01ft

0.11N.A.N.A.N.A.N.A.

0.21N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.001ft

1.049N.A.N.A.N.A.N.A.

1.478N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01ft

0.25N.A.N.A.N.A.N.A.

0.10N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.RA.RA.RA.

N.A.N.A.N.A.N.A.RA.

N.A.RA.N.A.N.A.N.A.

0.01ft

0.01N.A.N.A.N.A.N.A.

0.02N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

NA.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

O.Uft

1.85N.A.N.A.N.A.N.A.

3.75N.A.N.A.N.A.N.A.

N.A,N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.RA.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

0.01ft

100.0N.A.N.A.N.A.N.A.

1003N.A.N.A.N.A.RA.

N.A.RA.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

Rb XRF?

2W*

33N.A.N.A.N.A.N.A.

40N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.RA.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

RA.N.A.RA.N.A.N.A.

ro

x

mCO

-n

CD

tnx*.

MwnUr of Hw SOS Group (SooMM Gln4rafe d* SuivriHwM*}

XRALWork Order: 016810

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL P*g.e 2 of 6

Element. Method. Det.Um. Units.

SBC8SQ45 SBC85046 SBC85047 SBC85(48 SBC85048B

SBC85049 SBC85050 SBC85Q51 SBC850S2 SBC85Q53

SBC85054*Dup SBC85271*Dup SBC85283*DupSBC85295*DupSBC85050

7CD

ro

SI02 AI2O3 CaO MgO Na2O K2O Fc2O3 MnO T102 P2OS Cr2O3 LOI Sum XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO XRFIOO

0.01*.

N.A.N.A.N.A.61.7

N.A.

N.A.N.A.N.A.51.454.2

N.A.59.3

N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.15.9

N.A.

N.A.N.A.N.A.13.410.0

N.A.16.0

N.A.N.A.N.A.

0.01*

N.A.N.A.N.A.4.72

N.A.

N.A.N.A.N.A.9.779.36

N.A.3.50

N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.2.52N.A.

N.A.N.A.N.A.8.136.96

N.A.2.54N.A.N.A.N.A.

0.01*

N.A.N.A.N.A.4.98N.A.

N.A.N.A.N.A.1.931.10

N.A.6.16

N.A,N.A.N.A.

0.01ft

N.A.N.A.N.A.2.23

N.A.

N.A.N.A.N.A.0.110.11

N.A.0.83

N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.5.56

N.A.

N.A.N.A.N.A.13.014.3

N.A.8.48

N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.0.07

N.A.

N.A.N.A.N.A.0.150.11

N.A.0.11N.A.N.A.N.A.

0.001ft

N.A.N.A.N.A.0.674N.A.

N.A.N.A.N.A.

0.7800.549

N.A.1.043N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.0.26N.A.

N.A.N.A.N.A.0.060.05

N.A.0.25N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.0.02N.A.

N.A.N.A.N.A.0.030.06

N.A.0.01N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.0.55N.A.

N.A.N.A.N.A.0.853.50

N.A.2.00N.A.N.A.N.A.

0.01ft

N.A.N.A.N.A.99.2

N.A.

N.A.N.A.N.A.99.6

100.3

N.A.100.2N.A.N.A.N.A.

Rb XRF?

2ppm

N.A.N.A.N.A.

62N.A.

N.A.N.A.N.A.

35

N.A.35

N.A.N.A.N.A.

CO

rr

HI —r—EDOig2raCO

ia*

en .c*.en ro

oCO

Mamtaev of th* SGS Group (SoottM G*r*nl. d* StmmMtanc*

XRALWork Order: 016810

XRAL LaboratoriesA Division of SOS Canada (ne.

Date: 04/09/97 FINAL Pig* 3 of 6

Element. Method. Det.Um. Units.

SBC85271 SBC8S272 SBC85273 SBC85274 SBC85275

SBC85276 SBC85277 SBC85278 SBC85279 SBC852BO

SBC85281 SBC85282 SBC85283 SBC85284 SBC85285

SBC85286 SBC85287 SBC85288 SBC85289 SBC85290

SBC85291 SBC85292 SBC85293 SBC85294 SBC85295

SBC8S296 SBC85297 SBC85298 SBC85299 SBC85300

SrXRF?

2ppm273

N.A.N.A.N.A.N.A.

209N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

YXRF?

2ppm

14N.A.N.A.N.A.N.A.

25N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

ZrXRF?

3ppm161

N.A.N.A.N.A.N.A.

90N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

NoXRF?

2ppm

7N.A.N.A.N.A.N.A.

2N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

BaXRF?

20ppm

154N.A.N.A.N.A.N.A.

195N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

CrICF80

1ppm

601061021147386839796776185

100819093

11411198

10099877444787576848989

raICP80

1ppm

144746374044459063564951514660656750674669272714343737423839

CuICP80

0.5ppm45.048.083.953.674.667.992.9106127109

74.364.684.295.3159135112

81.4170113148

50.364.127.746.8

13576.780.955.171.7

ZnICP80

0.5ppm85.757.7124

82.190.3126160138195207220206248284122173189343291327266171189103146

91.4118116149120

Aa1CP80

3ppmoO<30OO<30OOo•o<3Ooo0000ooooooo

MoICP80

1ppm

4104

23347346733442443541334

144754

Jfc

ICP800.2

ppm0.90,90.40.50.91.40.91.01.01.61.60.21.4

<0 20.70.90.71.21.30.51.11.20.70.31.51.01.01.10.41.4

Sb BaICF80 ICF80

5 1ppm ppmO 406O 208^ 311^ 195O 161

O 192^ 337O 304O 180O 157

O 1210 147<5 145<5 471^ 190

<5 1580 501<5 170^ 176^ 152

O 208^ 402^ 174^ 151^ 356

^ 250^ 248^ 2050 255^ 398

en ro

o

sMunbw of Hw SOS Gfpup (Sod** G*n*sfe d* SUAMMMIM}

XRALWork Order: 016810

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL Page 4 of 6

Element. Method. Det.Lim, Units.

SBC85045 SBC85W6 SBC85047 SBC85W8 SBC85048B

SBC85W9 SBC85C50 SBC85051 SBC85052 SBC85W3

SBC85054*DupSBC85271*DupSBC85283*DupSBC85295*Dup SBC8SQSO

gCO

PO

Sr XRF?

2ppm

N.A.N.A.N.A.

956N.A.

N.A.N.A.N.A.

9256

N.A.275

N.A.N.A.N.A.

YXRF?

2ppm

N.A.N.A.N.A.

8N.A.

N.A.N.A.N.A.

1315

N.A.13

NA.N.A.N.A.

Zr XRF?

3ppm

N.A.N.A.N.A.

163N.A.

N.A.N.A.N.A.

5654

N.A.159

N.A.N.A.N.A.

Nb XRF?

2ppm

NA.NA.NA.

5NA.

NA.NA.NA.

22

NA.6

NA.NA.NA.

BaXRF7

20ppm

N.A.N.A.N.A.

926N.A.

N.A.NA.NA.

3062

NA.150

N.A.N.A.N.A.

CrICPSO1

ppm10282964978

9711478

131306

33554

1097196

Ni ICPSO1

ppm

3439481333

41455048

137

13213503450

CM ICPSO

0.5ppm78.479.3112

14.348.6

74.4104159

45.2688

84.539.781.745.1106

Zn ICPSO

0.5ppm115150125

69.3116

111124

96.871.21620

80.576.7234142129

As ICPSO

3ppm

O0ooooooooo<30oo

Mo ICP80

1ppm

47644

4541

13

^3347

ICPsJ0.2

ppm

0.90.41.20.20.3

1.11.30.3

•c: 0.21.0

•C021.21.61.21.5

Sb Ba ICPSO ICPSO

5 1ppm ppm

^ 398^ 4370 236<5 870^ 258

^ 323O 120^ 434^ 33O 295

O 967O 400^ 115^ 4580 109

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SEP-04-97 THU 12=14 PH XRAL LABORATORIES

FAX NO. 4164454152

P. 06/07

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XRAL

Work Order: 016810

KRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL 6 of 6

Element. Method. Det.Um. Itoite.

SBC85W5 S8C85046 SBC85047 SBC85048 SBC8S048B

SBC85049 SBC85050 SBC8S051 SBC85052 SBC85053

SBC85054*DupSBC85271*DupSBC85283*Dup SBC85295*DupSBC8S050

wICP80

10ppat

12

PbICF80

2ppm

<2 4

^

<2 <2 <2

<2 ^ <2

<2

Te S C02 AAH3CHM112CHM114

0.1 0.01 0.01. ppn % . . %

rom m

en

0.10.10.1

0.6

o!60'.2

oil-CO. l

N.A. N.A. N.A. 0.23

N.A.

N.A. N.A. N.A. 0.17 3.08

N.A. 0.64 N.A.N.A. N.A.

N.A.N.A.N.A.0.09

N.A.

N.A. N.A. N.A. 0.02 0.11

N.A. 0.05 N.A. N.A.N.A.

enji. enen ro

Mwnbw tt tto SGS Group (Scott* G fcrtn* d. SiuvafflMotl

SEP-04-97 THU 12:12 PH XRAL LABORATORIES

FAX NO. 4164454152

. 02/UY

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^zzz'z

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22:222: zzzzz

to•si*z"z'z'z

ZZZZZ ZZZZZ ZZZZZ ZZZZZ

^zz'z'z zz'z'z'z

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^zzzz zzzzz zzzzz

z'z'z'ziz zzzzz

*ZZZZ -ZZZZ ZZZZZ ZZZZZ ZZZZZ ZZZZZ

ozzzz

zz'z'z'z zzzzz zzzzz zzzzz

zz'zz zzzzz zzzzz zzzzz zzzzz

.zzzzz zzzzz zzzzz zzzzz

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XRALWork Order 016810

XRAL LaboratoriesA Division of SG S Canada Inc.

Date: 04/09/97 FINAL Page 2 of 6

Element. Method. Del.Llm.Unit*.

SBC8S045 SBC8SC46 SBC85G47 S3C85048 SBC85Q48B

SBC8S049 SBC8SOSO SBC85051 SBC85052 3BC85053

SBC85054*Dup S8CBS271*DupSBC85283*DupSBC85295*DupSBC85050

S1O2XRFIOO

0.01*

NA.N.A.N.A.61.7

N.A.

N.A.N.A.N.A.51.454.2

N.A.59.3N.A.N.A.N.A.

AI2O3XRFIOO

0.01%N.A.N.A.N.A.15.9

NA,

N.A.N.A.N.A.13.410.0

N.A.16.0

NA.N.A.NA.

Cai)XRJP100

0.01*N.A.N.A.N.A.4.72N.A.

N.A.N.A.N.A.9.779.36

KA.3.50N.A.N.A.N.A.

MeOXRFIOO

0.01lb

NA.NA.NA.2.52N.A.

N.A.N.A.N.A.8.136.96

NA.2.54NA,NA.NA.

Na20XRFIOO

0.0]*

N.A.N A.NA.4.98NA.

NA.N.A.MA.1.931.10

N.A.6.16NA.N.A.MA.

K2OXRFIOO

0.01•k

NA.NA.N.A.2.23

N.A.

N.A.NA.NA.0.110.11

NA.0.83N.A.NA.N.A.

Fe2O3XRFIOO

0.01*

NA.NA.N.A.5.56

NA.

N.A.NA.NA.13.014.)

NA.8.48

N.A.NA.N.A.

MnOXRFlflO

0.01IkN.A.NA.NA.0.07NA.

NA.N.A.NA,0.150.11

N.A.0.11N.A,N.A.NA

TiO2XRFIOO

0.0011fc

NA.N.A.NA.0.674N.A.

N.A.N.A.N.A.

0.7800.549

NA.1.043NA.NA.NA.

P2OSXRFIOO

0.01•bNA.NA.NA.0.26NA.

N.A,NA.NA.0.06O.OS

N.A.0.25N.A.N.A,NA.

CrtO3XRFIOO

0.01%

NA.N.A.NA.0.02N.A.

N.A.N.A.N.A.0.03O.C6

NA.0.01NA.NA.NA.

LOIXRFIOO

0.01ftNA.N.A.N.A.0.55NA.

NA.NA.N.A0.853.50

NA.2.00NA.NA.NA.

SumXRFIOO

0.01ftN.A.NA.NA.99.2NA.

NA.NA.N.A.99.6

100.3

NA.100.2NA,NA.NA.

RbXRF7

2pptn

N.A.N.A,NA.

62NA.

N.A.N.A.NA.

35

N.A.35

N.A.N.A,NA.

MMnbw Of th* SG* Qrovp (SoottW G*n*r*l8 tt* SurvtnilJK*)

XRALWork Order: 0168JO

Element. Method. Del.Llm. Unto.

/?

SBC85271 SBCS5272 SBC8S273 SBC85274 SBC85275

SBCB5276 SBC85277 SBCB5278 SBC85279 SBC852BO

SBC8528) SBC85282 SBC85283 SBC85284 SBC85285

SBC85286 SBCB5287 SBC85288 SBC85289 SBC8S290

SBC85291 SBC85292 SBC85293

SBC85295

SBC85296 SBC85297 SBO5298 SBC85299 SBC85300

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL fage 3 oJ 6

t/ nl

c

(V

SrXRF?

2ppm27J

N.A.N.A.N.A,N.A.

209N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

YXRF7

2ppm

14N.A.N.A.N.A.N.A.

25N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N,A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

ZrXRF?

3ppm

161N.A.N.A.N.A.N.A.

90N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N A.N.A.N.A.N.A.N.A,

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

NbXRF?

2ppm

7N.A.N.A.N.A.N.A.

2N.A.N.A.N.A.NA.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

BaXRF?

20ppm

154N.A.N.A.N.A.N.A.

195N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

NJV.N.A.N.A.N.A.N.A.

Cr1CP80

1ppm

6010610211473

8683979677

6185

1008190

9311411198

100

9987744478

7576848989

W1CP80

1ppm

1447463740

4445906356

4951514660

6567506746

6927271434

3737423839

CuICJP80

4.5PPm

45.048.083.953.674.6

67.992.9106127109

74.364.684.295.3159

135112

81.4170113

14850.364.127.746.8

13576.780.955.171.7

ZnICP80

O.Sppm

85.757.7124

82.190.3

126160138195207

220206248284122

173189343291327

266171189103146

9L4218116149120

AjICF80

3ppmOoooo0<3OOooo0ooo00oooooooooo0o

MoICF80

1ppra

4104

233

47346

73344

24435

41334

144754

ABICP80

0.2ppm

090.90.40.50.9

1,40.91.01.01.6

1.60.21,4

o!?0.90.71.21.30.5

1.11.20.70.31.5

1.91.01.10.41.4

Sb1CF80

5ppm

^^5O^<5

^<5

O

<5<S

^0

<545<50

0

O

^

^O

^5O

BaICF80

1ppm

406208311195161

192337304180157

121147145471190

158SOI170176152

208402174151356

250248205255398

IX

TZI

x

f—

Sgro.cSto

Tt3*

g

.e.03-C*in•c*enrv)

*~n

Ntanfccf of lh* SGS Gtavf ISocMt* Gftntato tt* SwvaNwwi)

XRALWork Order: 016810

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL 4 of 6

Element. Mdbod. Det.Lim.Units.

SBC85N5 SBC85M6 SBC85M7 SBC85Q48 SBC85048B

SBC8SW9 SBC85050 SBC85G51 SBC85W2 SHC85W3

SBC85Q54*Dup SBC8527I*Dup SBC85283*Dup SBC8S295*Dup SBC85050

SrXRF?

2ppm

N.A.N.A.N.A.

956N.A.

N.A.N.A.N.A.

9256

N.A.275

N.A.N.A.N.A.

YXRF?

2ppm

NJ\.N.A.N.A.

8N.A.

N.A.N.A.N.A.

1315

N.A.13

N.A.N.A.N.A.

ZrXRF?

3ppm

N.AN.A,N.A.

163N.A.

N.A.N.A.N.A.

5654

N.A.159

N.A.N.A,N.A.

NbXRF?

2ppm

N.A.N.A.N.A.

5N.A.

N.A.N.A.N.A.

22

NA.6

N.A.N.A.N.A.

BaXRF?

29ppm

N.A.N.A.N.A.926

N.A.

N.A.N.A.N.A.

3062

N.A.150

N.A,N.A.N.A.

CrICP80

1ppm

10282964978

9711478

131306

33554

1097196

NiICP89

1ppm

34394813 *33

41455048

137132

13SO3450

CuICP80

0-5ppm78.479.3

11214.348.6

74.4104159

45.2688

84.539.781.745.1

106

ZnICP80

0.5ppm115150125

69.3116

111124

96.871.2162080.576.7234142129

A*ICP80

3ppmOOoo<3

0<5o<$ooo0^3o

MoICP80

1ppm

47644

4541

13i*l

3347

AftICP80

0.2ppm

0.90.41.20-20.3

1.11.30.3

•e:0.21.0

•(CO 21.21.61.21.5

SbICP80

Sppm

^^^^C5

<5^O^O

ooo0

BaKP8D

1ppm

398437236870258

32312043433

295

967400115458109

McAibw of ilw SGS G rew (SccJiiiGfetfrrfftd* Surveillance)

C/3m-t3

XRALWork Order: 0 16810

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL P*g* 3 of 6rvi

Eieroenl. Method. Dct.Llm. Units.

SBC8S271 SBC85272 SBC45273 SBC85274 SBC85275

SBC85276 SBC85277 SBC85278 SBC85279 SBC85280

SBC95281 SBC85281 SBC85283 SBC85284 SBC8528S

SBC8S086SBC85287 SBC8SJ88 SBCS5289 SBC85290

SBC85291 5BC85292 5BC85293 SBC852M SBC85195

SBC8S296 SBC85297 SBC85W8 SBC85i99 SBC85JOO

WICF80

10ppm<IO*ilO<10<10<]0

<1000<10<iO<10

<10*:10<10<10<10

<10CIO-CIO0000oo•CIO00oo000000oooooo

PfoICP80l

ppm

3^3

^<2<2^<2<2

<2<2^C2<2

<2<2•C 2<2

3

<212^<2

2

<2<2^<2<2

TeAAH3

O.Ippm0.30,20.10.1

•CO.l

<0.1<0.1<0.1*:o.l<0.1

<0.1O.I<0.1•CO.!<0.1

<0.1C 0.1<0.1•i 0.1<0.1<0.1

0.30.20.10.10.30.2

*C0.1•CO.l

O.i

S CO2CHM112CHM114

0.01ft

0.61N.A.N.A.N.A.N.A.

3.72N.A.N.A.N.A.NA.

N.A.N.A.N.A.N.A.NA.

N.A.N.A.N.A.N.A.N.A.

NJ\.N^\.N.A.N^.N,A.

N.A.N.A.N.A.N.A,N.A.

0.01*

0.05N.A.N.A.N.A.N.A.

0.05N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A,N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

x:

sDO

m en

•e* en

in

in ro

70

CO

toIT-]-a

XRALWork Order: 016810

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 04/09/97 FINAL Fag* 6 of 6

Element. Method. Det.Lim. Uuits,

SBC85M5 SBC85046 SBC85047 SBC85N8 SBC85W8B

SBC85049 SBC850SC S8C8S051 SBC85052 SBC85M3

SBCSSA54*DupSBC85271 'DupSSC85283 'Duo SBC85295*DupSBC85050

WICP80

10ppa<IO<IO<10"CIO•00

<10<10<1000

12

••C 10<lO<10K 10-CIO

Pbicrao2

pjwn<2<2

4*:2Z2

C2<2<2<2

4

OO^<2^

TeAAH3

0.1ppoi0.10.10.1

•CO.l<0.1

*:0.1<0.l

0.6<0.1

0.6

•CO.l0.2

<0.l0.1

<0.1

s CO2CHM112CHM114

0.01t*

N.A.N.A.N.A.0.23N.A.

N.A.N.A.N.A.o.;?3.08

N.A.0.64N.A.N.A.N.A.

0.01. . ^

MA.N.A.N.A.0.09N.A.

N.A.N.A.N.A.0.02O.L1

MA.0.05N.A.N.A.N.A.

ro

en -o

70

i

.c*en

ro

M*nr**f of thvSGSGKvplSoeifM O Strafe d* Surv^illwiM)

AKMU unnsiuuvsiua

3OHPVE

WL1190S1WU190S2

~ WJ.19053VttJ.19054

JBMU-19055WU. 19056WU.19057~y wfciigosa-y^ — -WL119059

-HL119060WL119061

- HL119062WL119063HL119064

* HL119065*WL119066

~ ML119067WL119068NU.19D69WL119070

^ WU.19071

tlU.19072Hvll9073

v^BWill9074v^gCBJ.19075— HL119076

WL119077HL1 19078HL119079

. WU.19080WL119081HU.19082

.WU.190B3.,- WL119084

- WL119085WU, 19086

- KL1 19087 "KL1190BBML119089KL119090KL119091WL119092HL119093

- MU.19094WU. 19095NU.19096HU190~97HL119098-

~ ML119099NL119100KL119101

Sk*i0.19X02 ——— —- to.19103

WL119104ML119105

.•WL119106WU.19107

~ HU.19108WL119109WL119110WU.19111

- WU.19112ML119113HL119114WU. 19115HL119251

- WL119252HL119253ML.1 19254HU119255

^ WU.19256WL1192S7WL119258

O .9W-U

CO2 Ir COOLOM 0.01

0.040.050.020.020.110.04

^—~— —— 0-020.040.013.630.04O. OS0.020.120.010.030.280.790.020.030.060.040.300.100.021.990.103.740.6~60.080.030.04

-OT670 .JH..0,070.036.010.030.020.340.080.07O.O40.190.220.090.060.130.040.054.44

— ———— 0.060.160.050.030.030.170.100.030.030.020.040.020.030. 200.040.050.030.030.030.010.020.03

uii~ y r

NA20 t XHF-F 0.01

3.242.161.731.712.852.582.943.243.591.192.403.281.821.53

- 0.894.721.620.075.401.011.210.673.161.013.290.101.702.91"~ res-4.24*2.434-831.753.181.78

. 2~W-4.396.212.141.492.622.913.041.771.821.09

-1.022.051.931.660.106.422.071.901.381.702.810.974.251.781.851.685.092.S60.301.502.042.801.995.332.863.763.15

(CO t AL2O3 Ir SXO2 Ir XRF-F XSF-F XRF-P 0.01 0.01 0.01

7. SB7.268.709.094.937.668.506.266.303.097.241.65B ."496.75

-1.593.735.5335.25.9814.715.820.610.018.4B. 6234.79.235. 458.424.365.344.616.23i.ac6.35

___ 1,12 ,.1.831.866.257.908.311.387.045.946.916.291.43

- 1.738.787.2632.72.908.537.408.2310.33.127.123.637.652.418.80

——— 1.10 ——6.923.908.778.573.467. OB4.08S. 676.887.47

15.913.715-217.413.713-716.013.114.316.514.1IB. S15.914.413.6- ^16.013.92.4615.010.59.957.6112.1 -7.7213.21.9913.812.815.714.612.715.8~13TO ——

14.913.213.9

^15.015-814.013.514.414.913.814.413.714.111.313.616.414.03.2815.713.613.515-116.515.014.115.814.514.215.0

-as. 4— -14.013.214.214.313.213.416.213.212.613.7

49.650.949.047.2fig.O50.147.749.753.944.949.864.947.744-4.

CZL.2

52.138.157.947.145.947.9

-50 i*47.650.736.349.647.. tt-48.860.850.955.8

'49.865,650.749.868.264.851.350.448.367.550.149.352.853.6

- 70 . 6-69.847.348.838.669.449.749.949.447.049.954. 5SI. 349.566.248.5

-69.350.352.449.349.948.549.857.351.950.050.1

tfUBV A**^^^ *'

P205 t S * XRF-F U90O 0.01 0.01

0.060.080.04O.O40.100.070.070.090.160.190.120.130.05O.OC

} ——— 0.05 —— -0.460.080010.11O.O40.030.02

-0.050.030.06oOl0.08

- . 0.110.060.140.22

__ 0.210.080.150.080.060.110.310.090.060.070.140.080.080.070.13

- —— 0.140.210.050.06c. 010.100.060.070.070.040.230.050.200.070.140.05

~ — 0.13 —0.080.060.040.060.09O.OB0.33O.OB0.120.07

0.030.020.040.020.030.010.010.020.040.060.020.020.100.05

-0.09—0.010.210.100.020,130.010.01*:.01c. 010.060.070.030.04~?70ir"

0.020.01*:.010707~~

0.020.14O.OG0.010.100.010.020.02c. 010.030.130.010.080.020.040.010.220.16•c. 010.020. 060.040.020.060.010.030.050.030.044J.01

0.030.090.020.020.090.040.010. 040.190.04

K2O t CTO t XHF-F XRF-F 0.01 0.01

0,450.060.130.100.430.140.220.200.170.190.251.170.200.10

—— 3.160.910.32^010,090.110.140.020.240.130.32^010.100.480.140.140.180.06—— 6.22 ———2.14 — .0.22J^UL.^1.710.360.330.090.440.990.260.590.521.951.752.440.330.31oOl0.070.280.330.040.190.380.930.970.410.940.122.810.290.040.420.110.240.411.320.610.180.45

9.6510.712.311.42.149.B38.408.969.1020.510.15.1111.312-41.605.6212.20.375.609.569.788.458.888.89B. 161.2011.014.99.02"6.559.507.60 .

"ll.S4.0011.710.63.864.248.8010.99.155.549.0011.98.608.362.033.3610.812.22.831.4112.911.411.211.48.8210.16.0310.66.B312.41.859.5216.411.811.412.711.16.20B. 977.689- 58

ARAL LtABUKKTOK:

SAMPLE-

WL119259HL119260HUL19261HW- 192 62WL119263WUL19264WL1 19265HL119266MU.19267NL119268MU.19269ML119270HU.19271WL119272WL119273

~ HL119274WL119275NU.19276HL119277.

- D HL119051D WL119063D KU.19064D WL119075D WU.19078

- D KL119087D WL119092D WL119097D HL119106

- D HU.19109D ML1192S4D NU.19256D WU.19268

- SAMPLE

ML1190S1HL1190S2HU.19053HL119054

'j^UU.19055WL119056WU. 190 57

"j MU.19058WU. 19059WJ.19060KL1 19061HU.19062WL119063WL119064

- WL11906SKL119066KL119067ML119068KU.19069WUL19070HL119071

("KJ.19072\1fcll9073

i'-'/WJ. 19074VJH19075WL119076WL119077WL119076

~~ WL119079WL119080HL1190B1WU.19082

- MLU90B3WL119084WL119085HL119086

TTEB 3O-|J1

O02 VCOOIJOM0. 01

0.100.020.040.020.030.130.200.030.020.17e. 010.030.020.020.024T.01-0.020.02c. 010.040.01--

0.02--

0.01-~

0.04--

0.04--

0.020.18

THJ2 *XRF F0.001

.0.7180.9950.6510.5850.4380.9760.8651.301-090.6481.210.5460.8230.9170.2170.8220.83S0.1490.7510.6200.5370.4090.7730.5400.8010.1230.8281.100.8850.6662.101.051.030.6741.040.910

un-97

NA2O tXHF-F0.01

1.122.281.927.062.885.131.562.601.532.633.403.141.842.523.85

—— 3.332.232.123.473.22..

1-51.-

2.89—

2.00--

1.71—

2.00..

2.61

CR2O3 *XEF-F0.01

0.070.060.080.080.020.050.06o 010.030.030.020.030.070.070.020.020.040.770.060.210.310.370.070.340.041.160.100.050.060.040.020.030.030.020.030.03

MOO *XRF-F0.01

3.677.169.572.41S. 171.366.20S.464.814.902.532.798.309.872.76

.-0.4311.79.168.047.56--

6.73-.

5.43--

1.40—

10.4..

7.07—

4.88

HMD *2RF-F0.01

0.170.190.170.150.050.190.160.250.150.090.210.220.170.190.140.090.170.180.100.220.210.180.210.210.190.120.170.180.190.130.180.140.220.070.220.20

AL2OJ tXRF-F0.01

12,4M. 516.817.213.116.013.713.113.213.716.414.515.413.614.9

- 13.011.113.413.115.9..

14.4..

12.9-~

15.0~-

16.6-,

13.4-.

13.6

FE2O3 \XHF-F0.01

11.512.811.110.56. S313.613.216.210.55.1114.16.6012.313.15.066.9712.511.98.6114.113.511.112.511.613.412.511.710.713.17.8515.99.1013.36.3413.613.7

nORnQRl

SIO2 *XRF-F0.01

52.149.246.559.848.763.645.048.351.150.962.365.449.849.662.5

-76.151.950.551,649.5..

49.9 ...

46.9—

67.7..

47.1

49.7a.

51.0

en PPMTCP0.5

13221278.075.840.556.656.673.534.583.235.924.672.6

11014.027.8

11122.931.463.622.621.753.111.065.03.0

64. S50.817.474.734.37.0

54.013.772.622.0

P2OS *XRF-F0.01

0.130.070.040.130.320.170.310.280.090.060.220.230.050.060.170.040.060.070.070.06

~-0.06-.

o.u0.14--

0.04..

0.08-~

0.06

ZN PPMice0.5

73.869.980.670. S83.749.2

11611593.724.885.0

35883.794.275.186.184.867.731.886.875.081.994.272.589.495.081.183.6

11535513187.155.829.896.2

104

S tixm0.01

0.030.010.01c. 010.220.010.250.130.070.040014:. 010.03c. 01*:.01c.Ol0.030.020.020.030.11--

0.05..

0.01--

0.02--

0.03--

0.040.04

AS PPMICP

3

0OC3^3c3

OO43^3^3^^3^3c3^3*3

5^3^3OOc30<310c3<30<3C3C3C3<3^3O

ffffSS 2

K2O *XRF-F0.01

0.300.200.460.730.340.790.271.030.350.740.660.670.230.200.32---2.52.0.650.420.160.46. .

0.10..

o.so--

1.00.-

0.16

0.42..

0.73

RB PPMXRF- F

2

16

62

126g3925

2995

6446

94249B795

1211

511

9e23

4268

52

CAD *XRF-F0.01

13.011.110.75-398.673.138.438.6013,211,37.347.7711.610.86.191.818.4011.68.569.64

-~12.3

14.9

S. 52—

11.5

11.1-.

11.3

3R PHIXBF-F

2

2289793

10693

120124118429

7696

29495

104112985251

13155453515

10448

13628

118186144230

9218080

1328761

AJUftu unrr T 1 1 i rrr i n

SAMPLE

WL119087NU.19088

y HU19089NU.19090WU19091NU.19092WU.19093NU19094WU.19095WU.19096WU.19097WL119098HL119099HL1 13100WL1 19101

-^ Will9102HU19103WL119104KUL1910SNU.19106

" HU19107HL119108HU19109HIJ. 19110

- WU.19111WU.19112ML119113HLJ.19114WU19115

" WL119251HU19252WL1192S3WL119254

- NU19255NL11925CHU.19257WU19258WJL19259

- WL11926DWU. 19261NUL19262WL119263

.- KU.19264WU.19265WL119266ML119267WL119268

•- NU.19269NU.19270WU.19271VJL119272WL119273HU.19274HL119275WL119276WL119277

-) WU.190S1) WL119063

J KU.19064D ML119075D HU.19078

l WL1190B7' MU.19092

LI WL119097D MU19106A NU.19109

' WL1192S4' WU.19256

D WL0.19268

i0 ju — uun'

TE02 V QXRF-F ;0.001 1

0.3240.5811.110.8541.050.6911.151.181.090.7510.3660.5460.7320.9820.1770.5070.6610.9340.9040.5012.280.5930.5840.9580.6170.6910.3571.160.8760.6850.8071.550.9880.6421.071.460.9281.410.9530.6190.6092.360.7902.492.181.140.8810.7070.5930.6590.7410.755

— -—0-209 -0 .6630.7030.8060.721--

0.916--

1.09--

0.690..

0.496--

0.983

0.881

14203 f SRF-F D. 01

0.030.02•c. 010.020.06c. 010.030.030.050.050.020.020.070.060.24C. 010.130.040.060.120.030.050.030.040.040.110.030.030.040.070.090.040.040.02*.01•s. 010.030.020.030.090.02c. 010010.030.020.040.040.020.030.090.170.030.050.120.150.040.07

~-0.07--

O.O5-.

c. 01-~

0.13—

0.04..

0.04

iwiruKi.

mo fr i XRF-F 0.01

0.050.050.200.210.210.080.170.210.200.170.080.070.170.220.14c.Ol0.150.210.170.150.250.150.090.170.090.160.030.200.150.170.180.210.200.110.200.240.210.210.210.160.080.240.140.220.210.160.200.080.060.170.170.160.020.180.170.180.17

—0.19

~-0.18

-~0.08-.

0.15-.

0.21—

0.20

FE2O3 t XRF-F0.01

3.414.3814.814.114.14.7714.413.612.111.18.834.1911.312.49.021.3010.313.312.59.6116.99.40fi. 2813.75.2510.72.7014.110.711.411.515.813.66.7414.216.113.814.613.210.75.2516.17.0917.516.612.813.3S. 314.0610.710.87.011.8311.910.313.211.4

-~13.1

~-10.6..

4.77..

9.64..

13.6..

13.3

CO PPMICP 0.5

4.728.1

10179.0

12510.674.988.059.467.38.4

26.367.8

15015.22.4

95.115267.256.954.149.847.272.040.5

10712.043.249.584.978.617.3

13520.842.648.242.4

17733.138.912.345.910.574.264.586.462.616.518.482.232.818.44.2

26.833.337.7

13769.9

~-67.4

—4.4—7.7-.

41.4-~

39.760.1

BH. J-^^d^

ZH PPM t ICP 0.5

56.144.2

11098.4

12751.2

10317789.8

11989.786.586.3

13666.617.471.588.8

1O567.6

15671.887.1

10267.266.549. S

10667.489.188.4

13083.5

10511710610820212490.735.098.666.786.4

11861.9

16279.460.279.775.777.255.192.583.782.672.783.4

-~91.6

-~56.4~-84.6~-76.1

-~105159

l

IS PPM ICP

3

rirfrfrfrf^3rfrfc3rfrfrfrfrfrfrfrfrfrfrfrfrfrfrfrfrfrf^3rfOrfrfrfrfrfrfrfrforfrfrfrfrfrfrfrfrfrfrfrfrfrfrf^3rfrfrf--

rf-~rf-~rf

—rf

-~rfrf

r*WA -*

RB PPM XRF-F

2

441013

817331120234327671310

8*2e

206 '65

30442132

775

7275

101940

3112011

914201030

9341617231812

942

C.— -51"" 27

192

13~-4-~

13~-

32-.7..

19~-

18

SR PPM XRF-F

2

77527914099

169214145

8679

13739

415137186

3518921112012112713044

9001584O2106403

91137134180233112

101016311018116311812655823326375523636719453464112310O41S161162153141225

—102

~-190

—215

~-129

~111

--194

30-Gun-97 REPORT --—— WORKORDHl 15533 PAGE

SJWPLS

HU.19051 - NU.19052

HL119053NUL19054

'-•t-Sllill9055WU. 190 56ML1190S7

JE.1CJ.1905BWU. 19059NU.19060NU.19061NLH9062HU.19063HU.19064HU19065

- WL119066HL119067WL11906BWL119069WU.19070

""" WUL19071rWU.19072

o jJ8ill9073' J Vbll9074- (jpill9075

NL119076HL119077HL119078NL119079

~ HL119080ML1 19081WL119082WL119083

~ WL119084HU.19085HU.19086WU.19087HL1190BB

~ HL1190B9RL119090NU.19091HL119092

^ WL119093NL119D94ML119095HL119096HL119097

- HLH9098KU.19099KU.19100ML119101

.36*119102HL119103WL119104WU.19105WU.19106

- WUL19107HL11910BHL119109HL119110MU.19111HL119112WL119113NL119114WL11911S

- WUL192S1WL119252WL119253WL119254WLJ.192S5

~ NU.19256KU19257HL119258

•t PPMXRF- F

2

20 231611

9221925IB1632131924IB252242161914131614IB4

27252218442224182919

79

2424211525262420191416204242183223114012172516161229251620352918222827

ZR PPM 1 XRF-F

2

76 775751

142797593

1049496

126666891

1737427

12749474476S3782177

10681

13015315278

1517S78

123218

846274

13890829487

107126

627031

17763726749

15159

13771

10260

18193605766

10777

148 .93

11179

SB PPM XRF-F

2

2 3325442666744694956563

1027g474

10182453S9

41336443235437825436

42536

127434

42f3B

^2*24

MO PPM ICP

1

4 526742235

^163

10643

ci3

124l41

1^4l^J38

el634

1383489342725559e4

653844263694

14393

13348545

4l4

A3 PPM iICP0.2

024.24.24.24.24.20.24.24.24.20.34.2

4.20.24.24.24.24.20.30.30.24.24.24.24.20.24.20.34.20.24.20.20.34.20.60.54.20.24.20.30.24.24.20.30.20.3C. 20.24.24.24.20.24.24.20.24.20.24.24.24.20.34.24.24.20.20.34.24.24.20.34.2

SB PPMTCP

5

245

6^5^54545^545^5^5,;5

45454;5^17^57e

n45

9

31

454545^4545^54545^45,-5C54545

^54545454545

56

45454545454545454545454545454545454545454545

TS PPM FAA0.1

0.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.10.10.14.14.14.14.14.14.10.10.24.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.10.14.14.14.14.14.10.20.2C.I4.14.14.14.14.14.14.14.14.14.14.14.10.14.14.14.14.14.1

EA PPM ICP1

79 19282877234936531525

3095933

833891113

12392521

5no4565

523

11723497749

2175122864

914125

702379

20741

1001864604146047249

4327

5572114163

256561109179

301140

501668284595

664854297

BA PPM XRF-F

20

134 937472

131100117134126

90102364

9086

8138901*7

8299718949

18091

1286692

168112

96171123

97524

92114863175125

8813922113114922745439655990

10551

3091001359094

166264489116211

881090

11471

11688

122152655142136154

4WM-I J-MM-MBkr.UkW.Tk>*

SAMPLE

HL1192S9- ML119260

WL119261RLJ. 19262HUL19263HL119264

— WL119265WL119266WL1 19267HL119268HL1 19269WL119270WU.19271WL119272WL119273

- KL119274WL119275KL119276WL119277

D WU.19051~D WL119063

0 NL119064D HL119075D MLJ.19O78

—D MLH9087D HU.19092D ML119097D WU.19106D HL119109

~D WJ.19254D HL119256O HL11926B

. SAMPLE

KL119051- NL119052

HL119053WL119054

^V;"PL|119055WU.19056HL119057

L'/KlillSOSSNL119059HL119060

- HL119061HL119062ML119063HL119064WU19065WU.1906EKL119067WL119068WL119069

- ML119070WL119071

("HJ. 19072. c \MCill9073^ /JflU.19074

(JOL119075HL11907SWL119077WL119078

- WL119O79NL1 19080WL119081WL119082ML119083

~ WL119084WL119085WL119086

..CMJ J W" W

Y PPMXRF-F

2

352713104116433527251716182312•eS.26241819--

22--

28

13--

13--

27--

25

W PPMICP10

ClOcloclOclOdOcXO^10clOclO^10^10clOClOC^O^10^xo*dOclOClOClOClOclOclOclOclOclOClOClOClOClOClOClOclOClOclOclO

'UK* y f

ZR PPMXRP-P

2

1067453

1481941811841757675

134119

5971

14011072698677

—68

~-104

--135

—48

—79

—77

PB PPMICP

2

c2*2c2C2c2c2c2c2c2c2c2c2c2c2c2c2c2

3c2c2c2c2c2c2c2C2c2c2c2C2c2c2c2c2f2c2

I^EIC^/WA

NB PPMXRF-F

2

74

c26

208

2814238S3e6

267462

4.~5.-5--4-~4..4

LOI *XRF-F0.01

1.000.700.550.602,800.601.600.600.807.050.600.851.450.652.000.900.7011.20.601.602.103.702.153.151.4513.31.304.55-.100.550.600.652.951.400.900.60

MO PPMICP

1

63373632

177662269a1242--1-—e..9--B--57

SUM IrXRF-F

0.1

100.099.699.798.9

100.399.599.899.9

100.299.5

100.2100.1100.3100.099.799.9

100.1100.4100.399. B99.5

100.1100.299.7

100.3100.599-7

100.399.9

100.1100.199.9

100.199.899.999.9

nw*u*w*

A3 PPMICP0 .2

0.4c.20.4c.20.4c.20.50.4c.2C.2c.2c.2c.2c.2c.2c.2c.2C.2c.2c.2C. 2..c.2--1.2-~c.2.-c.2--c.2c.2

i r^rr ^0 9*9 *J

SB PPMICP

5

cScS

6cSc5cScScScSC5C5CScSc5c5cScScSCSc5c5~-

cS..

c5..

c5-~c5-.

cScS

l

TB PPMFAAO.I

c.lc.lc.lc.lc.lc.lc.lc.lc.lc.lc.lc.lc.lc.lc-lc.lc.lc.lc.lc.lc.l-.c.l~-c.l—0.1..c.l. -c.lc.l

HA PPMICP

17657

16420919813275

33637

1603993486959

121302276

98427552~-

69..

908..

394. -

499..

77173

BA PPMXHF-F

20

129106185255292173190394108230389358116105156288297135107138

92.~

166-.

219..

90

1S5-.

233

*wa* m** f* n rna^n ri* t \

SWOW!

WL1 19087— HL119088

WL1 19089HL119090WL1 19091WU, 19092

- HL119093HL119094HU.1909SHL119096WL1 19097NU.19098HU.19099HL119100WU.19101

i^ Mjll9102WL119103HL119104WL1 19105HL119106

~~ HL119107NU.19108WL1 19109MU.19110

- WJ.19111WU.19112HUL19113KL119114HL119115

~ WU.19251NU.19252WL119253HL119254

— WL119255WU.1925CHL1192S7WLH9258KL119259

- KU.19260HL119261HL1192S2HL119263

^ HL119264HU192E5WIJ.19266WL0.19267MLH9268

- WL119269WL119270HL119271WH19272NL119273WU.19274WL119275WL1 19276WL119277

^ HU.19051i WU.19063

HL119064D HL119075D WL119078

NLH9067WL119092

u ML119097D NU.19106

-0 WL119109NL119254WL119256

D WL119269

e*w i^w— t.

W PPM ICP 10

ClOclOClOclOcloclOclDClOClOClOclOdoclOclOClOclOclOclOClOClOClOclOClOclOclOclOClOclO230clOclOclOClOClOclOclOClOclOClOclOclOclOClOClOClOclOclOClOclOclOclOClOclOClOclOclOclOclO

-~ClO

-~clO-~ClO

--clO

~-ClOclO

tUffl 7 1

PB PPM ICP2

2c2c2*3C2c2c2C2c2c2c24

c2c2

3c2c2c2C2c2c2c2c2C2c2c2c2c2c2c2c2c2c2c2^2c2C299c2c2c2c2c2c2c2c2c2c2c2C2c2c2c2c2c2c2c2c2—C2

c2.~

c2—c2..

c2c2

fl^rWKA

U)I f XRP-P 0.01

1.151.551.051.701.351.200.651.202.302.602.502.150.951.1513.21.551.2S1.150.501.700.501.551.000.851.550.651.300.751.30O.BO0.951.551.451.051.151.250.751.2S0.751.551.402.152.004.501.551.851.500.800.900.800.650.600.851.40O.BO0.851.00

—0.65--

4.35..

1.00..

1.45-~

1.45..

1.50

STJM t XRF- P 0.1

100.3100.2100.1101.3100.1100.199.8

100.2100.210U.3100.1100.398.899.2

100.399.499.7

100.299.699.3

100.399.6

100.4100.3100.298.9

100.399.999.499.299.9

100.2100.299.5

100.0100.3100.3100.399.799.2

100.2100.1100.3100.4100.0100.3100.299.9

100.399.799.299.3

100.3100.499.4

100.199.8-.

100.0..

100.0,.

100.2..

99.4--

100.1..

100.2

WOMCORPgR 15B33 ffOE

XRALWork Order: 015684

XRAL LaboratoriesA DM*kn of SQS Canada hie.

Date: 03/07/97 FINAL l Of t

Element. Method. Drt.Llm. Unite.

WLI 19001 WL1K002- WL119003 WLI 19004 WLI 19005

WLI 19006 WU 19007 WLI 14008

^.6 WU 19009 WLI 19010

WLI 19011 WLI 19012

SBWtllMU ^ WU 19015

WLI 19016 WU 19017

SB WLI 1901 9 ^6*1119020

^Wt 1 19022

WLI 19024 WLI 19025

WLI 191 16 WLI 19117 WLI 191 18 WLI 191 19 WU 1 9120

SI02 AI2O3 CaO XRF102 XRFM2 XRF102 XRF0.01 o.oi o.oi o.oi

MgOmn Na2O K2O K2O3 MnO TKM P2OS Cr2O3 LO! Sun Rb XRF102 XKF102 XRFI02 XRF102 XRTJQJ XRTI92 XRP102 XIWIOZ XRF1D2 XRF102aoi OJ1 0.01 0.01 0.01 o.ti i.oi 0,01 0.01 ^

47.762.848.047.550.8

51.248.746.747.849.3

65.463.465.649.065J

47.250.1

-60.750.430.8

63.657.548.656.168.2

48.248.949.263.757.0

15.314.816.314.613.3

14.1I5J16.15.7614.016.715.014.417.915.1

12.614.615.515.21.64

15.115.113.812.215.6

13.314.114.315.614.3

10.23.7512.412.410.910.510.611.07.529.555.302.565.1411.84.43

15.810.93.3912.02.50

5.496.6112.97.002.48

9.268.7311,63.569.49

8.324.568.818.056,35

7.038.2210.621.610.2

1.553.471.966.142.613.483.605.305.9533.7

3.984.833.952.291.49

5.497,514.162.243.63

2.373.792.101.602.522.402.001.430.172.38

3.641.093.912.704.72

0.783.265.102.270.07

4.084,231.751.556.412.483.432.183.872.36

0.46l.ZO0.120.110.17

0.240.250.22

^.010.35

1.126.840.800.540.52

0.410.740.360.78

*C0.01

0.190.840.591.100.55

0.800.200.602.651.18

12.85.369,3312.713.4

12.612.111.012.211.2

4.334.646.3610.15.55

16.913.97.0610.110.4

5.979.0415.616.23.26

16.114.615.35.059.57

0.190.080.150.200.19

0.150.180.150.220,200.080.070.050.150.08

0.330.170.140.380.22

0.160.140.220.310.04

0.210.200.210.070.13

0.900.630.550.911.16

0.820.810.630.430.70

0.660.650.460.680.591.421.700.651.360.11

0.551.012.002.260.37

-2.391.222.000.660.52

0.070.470.040.070.12

0.060.060.040.030.04

0.130.130.140.050.14

0.110.170.130.140.01

0.090.210.210.290.110.340.090.220.270.13

0.070.040.140.060.03

0.030.070.070.390,09

0.020.020.020.060.02

0.030.040.020.030.28

0.030.030.040.020.020.030.030.030.020.02

1.452.600.901.100.90

0.500.851.004.300.950.752.100.850.550.95

1.35J. 001.751.1020.7

0.850.800.701.001.701.600.850.701.651.95

99.9100.599.099.499.999.799.299.1

100,599.1

99.8100.2W.799.7

100.1

100.5100.3100.199.8

100,4

100.1100.5100.4100.4100.3100.3100.01C0.699.6

100.4

17301686

108

107

1543

182181723

1220102519

^32164521

329

178931

MwntMr of Id* MS Group (Soclft* Q intrtfe d* SvnwMno*)

XRALWork Order: 015684

XRAL LaboratoriesA Divltion of SOS Canada Inc.

Date: 03/07/97 FINAL Fifo 2 of 9

Method.Dtt.Ltm. Unite.

WLI 19121 WLII9I22 WU 19123 WLI 19124 WLI 19125

WLI 19126 WLI 19127 WLI 19128 WLI 19129 WLII9I30

WLI 19131WLI 19132WLI 19133

•S6JH.1 19134

WU 19278 , WLI 19279-!* WLI 19280 WLI 19281

WLI 19282 WLI 19283 WLI 1 9214 WLI 19285 WLI 19286WLI 1 9187 WLI 19288 WLI 19289 WLI 19290 WU 19291

SI02 A1203 CaO MtO XRF102 XRF102 XRF102 \RF1M

0.01 0.01 0.01 0.019* *k Ik *

68.2 38.0 53.8 41.1 64.959.5 49.9 45.0 68.3 49.849.8 52.4 50.8 48.8 53.151.4 52.9 59.8 50.9 55.948.551.7 48.7 61.7 64.250.9 48.6 49.651.4 49.7

16.0 19.1 14.97.51 17.915.9 14.3 13.4 15.0 14.214.3 13.7 14.2 13.5 14.813.5 15.0 15.214.3 11.5

13.6 13.7 14.3 145 13.614.8 14.0 14.4 14.0 15.3

2.97 9.63 12.5 4.57 3.625.938.19 14.3 2.40 14.214.3 8.94 14.9 11.9 (.189.05 13.4 5.77 9.37 8.5912.4 9.75 11.5 5.456.123.49 9.54 10.5 11.4 11.0

1.56 12.4 4.39 24.91.512.94 6.15 7.02 1.70 4.824.73 2.93 4.16 8.344.479.70 2.84 3.86 7.54 6.434.46 6.55 8.17 2.71 1.986.35 7.69 6.94 3.08 7.00

N*2O K2O R2O3 XRF102 XRF1W XRF102

0.61 0.81 0.01 % % %

5.36 0.99 0.96 0.09 6.113.37 3.13 1.01 4.60 1.831.80 2.28 1.91 2.32 4.152.47 1.33 4.69 3.30 2.071.80 3.47 1.63 5.56 1.114.24 2.74 265 1.78 2.13

1.13 0.93 0.77 0.02 1.141.68 0.13 0.35 2.92 0.420.46 0.91 0.37 0.64 0.360.52 0.69 1.76 0.310.400.61 0.24 1.262.67 1.060.64 0.46 1.08 0.72 0.31

3.51 14.0 9.27 13.6 3.178.75 15.7 17.3 2.85 12.512.514.7 11.3 11.6 11.411.0 11.0 6.3312.4 12.515.7 12.7 11.8 4.21 7.0614.5 14.0 12.4 14.1 11.2

MnO XRF102

0.01*,

0.03 0.18 0.16 0.20 0.090.13 0.22 0.24 0.04 0.210.21 0.17 0.22 0.18 0.240.23 0.24 0.09 0.19 0.20

0.23 0.19 0.19 0.05 0.100.22 0.20 0.18 0.21 0.17

Tf02 P205 XRF102 XRF102

0.01 0.019* K

0.45 0.95 0.99 0.30 0.470.87 2.19 0.78 0.36 0.810.82 2.65 0.82 0.81 0.840.63 0.87 0.61 0.86 0.991.560.91 0.71 0.53 0.601.25 1.07 0.79 1.99 0.75

0.16 0.07 0.21 0.02 0.150.17 0.24 0.06 0.12 0.060.06 0.36 0.06 0.15 0.150.05 0.07 0.32 0.07 0.090.12 0.06 0.05 0.28 0.200.09 0.08 O.G6 0.20 0.07

CrZOJ XRFI02

0.01•k0.02 0.12 0.04 0.40 0.020.03 0.02 0.05 0.03 0.050.05 0.01 0.05 0.05 0.040.08 0.06 0.03 0.04 0.040.03 0.02 0.08 0.03 0.030.01 0.05 0.06 0.04 0.05

LOI IRF102

9.01

0.55 3.95 1.95 7.60 0.651.350.25 0.95 1.J5 1.000.85 0.85 0.90 1.35 2.251.00 1.15 1.10 0.75 1.550.80 0.65 1.40 1.50 1.701.60 1.10 0.95 0.90 2.35

Sun RkXRF102 XRF102

0.01 2W

100.1 100.3100.0 100.3 100.0100.6 100.4 100.5 99.7 99.999.9

100.1 99.7 99.7

100.199.8 99.6 99.8

100.1 100.3100.0 IOO.D 99.9 99.4 99.9

100.1 99.5 99.6

100.0 100.1

ppss52 33 32 9

6268 4

13 75 1410 21 9

(8 1510 25 38 12 13H

5 64 37 3025 13 34 10 23

l MMT*m of Ui* SOS Group BucMt* 6ln*tto d* Snmlir*ic*i

XRALWork Order: 015684

XRAL LaboratoriesA Dtofcion of SOS Canada Inc.

Dale: 03/07/97 FINAL 3 of 9

Element. Method. Det.LJm. Units.

fct 1 19292)WLI 19293

i 19294)WU 19295LWLI 19296

1 19297119298119299

. 119300 VLHSOOI

WLI1S304 WLI 19305 —— WL1 19306

WLI 19107*DwpWL119001*DupWLl 19013*Dop WLI 19025*Dvp WL1 19127

*Dnp WLI 19280*Dvp WLI 19292*Dwp WLI 19304

SiO2 AI2O3 CaO MgO N*2O K2O Pe2O3 MnO TIO2 P2OS CrlTM intXR?J? ^'S? ****1X ***Jk XR?M XR™* ™™8 XR™ x*™ XRnoa xSKS nw o.oi 0.01 0.01 o.oi 0.01 0.01 0.01 0.01 0.01 0.01 o!oi oloi^'•'•ftftftftftftftfll^

48.0 50.2 68.6 49.2

J5I.8-

49.6 50.0 50.5 48.3 59.6

46.0 57.8 50.9 49.1 49.8

50.0 48.1 65.9 67.8 49.9

51.0 48.1 50.9

13.9 137 15.614.2 15.3

15.0 13.7 14.3 11.8 15.018.7 16.5 133 13.9 13.6

15.0 15.4 14.5 15.6 14.4

14.414.0 13.2

11.2 8.24 2.28 11.6 7.99

10.6 10.5 9.47 9.67 5.4910.6 5.12 5.27 11.51.16

11.410.2 5.15 2.48 8.19

9.39 11.2 5.30

5.2? 6.61 1.22 9.57 4.11

7.50 7,02 7.50 9.13 3.3610.8 4.47 4.92 3.97 7.10

7.59 8.34 1.98 1.49 6.16

7.56 5.27 4.91

2.34 3.97 4.19 2.06 2.30

2.43 2.80 3.11 2.58 4.56

1.70 5.24 3.54 1.72 3.25

1.76 2.38 3.93 f. 42 3.14

3.28 2.36 3.53

0.66 0.37 2.74 0.16 0.44

0.14 0.15 0.73 0.28 0.590.22 041 0.10 0.50 0.38

0.51 0.46 0.78 0.55 0.13

0.30 0.65 0.11

15.4 14.5 3.09 10.8 6.52

12.7 13.8 12.3 15.8 8.25

9.30 8.15 18.5 15.2 15.5

11.0 12.8 6.40 3.30 15.7

12.5 15.4 18.5

0.24 0.19 0.03 0.16 0.08

0.17 0.19 0.28 0.25 0.11

O.H 0.14 O.J2 0.21 0.21

0.18 0.19 0.05 0.05 0.22

0.19 0.24 0.32

1.52 1.74 0.43 0.62 0.57

0.97 1.05 1.09 1.24 0.87

0.43 0.76 2.59 1.99 1.41

0.70 0.8S 0.45 0.37 2.20

0.86 1.52159

0.11 0.15 0.15 0.04 0.13

0.08 0.08 0.11 0.04 0.28

0.04 0.13 0.34 0.20 0.100.06 0.07 0.15 0,12 0.24

0.07 O.I I 0.34

0.03 0.03 0.02 0.08 0.04

0.08 0.05 0.04 0.02 0.03

0.09 0.03

^.01 0.03 0.02

O.M 0.07 0.02 0.02 0.02

0.04 0.03

*:O.OI

1.00 0.40 1.25 0.80 0.95

0.60 0.80 0.95 1.45 1.50

1.95 1.10 0.30 0.70 0.85

1.25 1.10 0.80 l.CO 0.20

0.93 1.05 0.20

Sun Rb XJU102 XRF102

0.01 2 ft ppm

99.8 100.2 99.999J

100.3

99.9 100. 1 100.5 100.6 99.8

100. 1 99.9

100.2 100.1 100.5

99.7 100.1 100.1 99.9

100.5

100.6 100. 1 100.1

8 16 69

8 30

3 S

32 17 18

17 17 4

19 142518 20 22 5

117 3

l Mmriw of tt* 80S Group noetttt Ointrali d* Suwtllline*)

XRALWork Order: 015684

XRAL LaboratoriesA Olvbion of 803 Cinnta Inc.

Date: 03/07/97 FINAL

Mclfcod.Det.Um.Unite.

WL! 191)01WU 19002WL119003

-WU 19004•^ WLI 19005

WU 19006 WL1 19007 WLI 19008

WL 1 1901 0WLI 1901 1 WLI 19012WLI 19014WLI 19015WLI 19016 WLI 19017WLI 19019 WLI 19020

(WLH902I) WLI 19021VJN,I 19023

WLI 19024WLI 19025WLI 19116 WLI 191 17 WLI 191 1 8 WLI 191 19 WLI 19120

4 or g

MmntMr of ir* SOS Group (SocUU Qtntate d* SvwlthflMl

Sr XRF102 J

2 ppm145

1080 124 127 153137 119 122

12 429

250 129 113 180 285180 160 456 131 77

196 430 189 105 493236 114 136

1050 227

Y[RP102 :

2ppm

23 23 25 28 2820 18 16 18 239

21 10 21 1639 369

33 96

28 45 556

43 27 44 27 (6

ZrKRFI02 J

2ppm

10 231 141 328 12596 64 53

179251

J43 129 139 67

15388

135 141 124 21

138 148 135 193161193 127 142 184114

Nb [RF102

2 ppm

58 7 832 2 27 65 54 3 77 5 4 7

104

10 15 7

1320 47 84

Ba XRFI02

20PPI189

1630 91 93

132123 113 86 41

1(5289

1060 188 140220179231 190 279

83116289 257 341 236392 140 238

1040 275

KfA 0.2

ppm0.2 0.3

*:o.2 0.5

C0.2C 0.2

0.2 •C0.2 •C0.2

0.3C 0.2

0.2 0.3

*C0.2 0.23.6 0.4 0.3

C0.2 •C0.2

0.4 0.4

c 0.2 0.5

^.20.6

•C0.2 C0.2

0.4 c 0.2

CuICP80

•.5 ppm100

17.9 37.5 66.4 58.366.5 97.7 34.9 49.8 78.616.4 57.4 27.3 54.2 3.3101

65.1 18.0 95.6 12.914.8 9.7

32.6 53.8 30.2126

47.4 38.3 33.2 3.0

Pb ICP80

2 ppm

10 18 3 6 886 4 39

10 8 6 8 48

13 7

12 338

11 22

848 12 13 22

5

ZnICP80

0.5 ppm112

69.9 39.8 61.1 70.545.3 82.8 47.3 67J 67.077.8 60.0 16.5 43.8 14.0101

91.2 96.0 61.0 25.871.0 81.5

111 144

24.5121

69.5 112

67.5 35.0

AsICPtO

3ppm

97 4

C347

O Ooc3

5C3

6 14

C37 7

O 7

OO10o18

C39

12 13 9

O

MoICP80

1 ppot

4 6 3 44

4 4 2l

O

56 9 3 6

121 6 3 6

O7 3 i

10 57 2 3 6 4

Sb ICP80

Sppm<5 <5 <511 5

C5 <5 C5 C5C5

c56

C5 C5 C5

6 C5

8 C5 C5O

9 •CJ 8

O<5

7 6

C5 C5

WICPtO

K) ppmCIO CIO CIO CJOooCIOoo

II00 CIO

0000ooC 10 00

00 CIOoo00 CIOCIO 00

14c looooo00 CIO C 10

H

Ba ICP801

DfiDlrt*"*

165 1830

88 116 73

248 98 95 20

107440

1200 246245 261108 184 202 230 20

117 235 197 268 364390 107 155

1220 276

-

r

trE cr-

c? *.[

iljcJc4

r

XRALWorit Order: 015684

XRAL LaboratoriesA Division of SOS Canada Inc.

Dale: 03/07/97 FINAL Fiat 5 of 9element Melted. Det.Lltn. UoHs.

WLII9I21 WU 19122 WLII9I23 WU 19124 WL1I9I25

WL 1 19 J 26 WLI 19127WLI 19128 WLI 19129 WLI 19130

WLI 19131 WLI 19132 WLI 19133 *K.1 19134 WLI 19135

WU 19136 WLI 19278 WL1I9279 WLI 19280 WLI 19281

WLI 19282 WLI 19283 WLI 19284 WLI 19285

SB**. 119286

WLI 19287 WLI 19288 WLI 19289 WLI 19290 WLI 19291

SB,

ST V Zr Nb Bs XRF102 XRF1W XRF102 XRF102 XRFI02 1 2 2 2 20

ppm ppm ppm ppm ppm854 11 186 8 931 62 26 82 8 436

141 21 113 7 427 33 8 28 6 56

1370 13 211 8 900255 238 73

615 160146 129 163 454 576277 131 683158 103

209 131 196 544603

195 218 299 222 124

14 47 26

5 2723 (8 24 25 2116 20 25 21 24

34 20 23 13 19

27 25 23 39 26

143 151 57

153 67

69 261 70 75

1336f 71

164 81 91

103 86 57

204 128

105 83 76

133 69

4 6 5 6 5

4 9 2 6 52 2 9 3 2

3 3 3 7 5

2 3 8 6 5

396 152 166

1370 158

132 298 106 225 175205

1200 1210

144 223

231152 350

1050 351

229147 289 212 116

ICPfiJ 0.2

ppm0.4

c 0.2 0.2 0.4 0.4

^.2 CO.2 C 0.2 CO.2 *:0.2

CO.2 0.4

•CO.2 *C0.2

0.3CO.2 C 0.2

0.3 •CO.2

0.5

*C0.2 CO.2 C 0.2

0.3 0.4

0.3 *C0.2 •CO.2 CO.2 C 0.2

CdICP89

0.5 ppm

18.4 8.4

19.8 39.6 22.0

25.2 28.5 59.8 26.5 30.5

31.4 72.9 35.3 47.4 77.5

36.4 45.6 40.7 32.0 69.1

29.0 21.6 163

18.3 231

149 38.4 35.526.8 66.3

Pb ICF80

I ppm

16 3

10 2

23

7 11 6

29 68

17 5 9 8

10 6

11 8

17

9 6 8

12 12

9 8 9

12 8

Zn 1CPW

0.5 ppn

39.0 60.1 50.7 69.f 32.5

90.T 100

86.7 62.* 83.1

86.1 184

63.4 44.4 37.J

63.3 40.4 58.353.4114

101 73.3 69.8 21.0 1450

87.5 68.2

109 109

52.6

AsICP80

3 ppm

C3 C3

6 C3 C3

10 19 3 4

C3

C3 7

C3 C3

7

C3 S

17 6

10 C3 10

C3C3

C3 C3C3

10 C3

MeICP8D

1 ppm

7 1

34 ci

7

6 CI 38

8 5

5 89 t3

cit 4 2

11

3 2 44

12

2 3 2 4 5

Sb ICP80

5ppm

CS CS

8 CSCS

CS 6

C5 CS CS

CS 13

CS CS CS•C5 ^ CS CS

85

CS CS CS CS

7 CS CS 12

C5

WICF80

10 Ppm

•CIO OO CIO

13•CIO

CIOcio•CIO CIOcioCIO CIO

12 CIO CIO

CIO CIO CIO CIOCIO

1117

CIO cioCIO

ISCIO CIO CIO

13

•aICF80

1 ppm970 565 458 24iiifiIfJOJ

42571

188 1800

93110 277 65

400 117377

1720 1310 238190

191 82

454 1290435

218 213 404 128 102

Mfmlwr of til* 848 Groap (SocMMfltnfote di SutvtHftnc*)

XRALWorkOrden 0 15684

XRAL LaboratoriesA Olvitlon of 808 Canute Inc.

Date: 03/07/97 FINAL t or 9Element.Method.Drt.Llm.Unite.

119192119293119294

19295119296

(WU 19297\VL119298J WU 19299

WLI 1*300VWLIIMOI

'PU 19302 WU 19303 WLI19304 WU 1930S WLI 1930S

WL119307*Dup WL J19001*DupWL119013*Dup WLI 19025*DopWLll9l27

*DupWLll9280*Dup WLI 19292*Dup WLI 19304

Sr Y Zr Nb Ba XRFI02 XRF102 XRF102 XRF102 XKF102

1 1 2 2 20ppm346 238 819 129 219

118 13417984

698

132 289 115 155 174148 146115 490 236

158344 115

ppm .3442

9 17 16

23 26 32 29 23

12 19 53 42 3519 24 H7

46

22 3552

ppm101 144 181 57

110

82 81 98 92

160

48 138 202 135 109

67 70

137 162 153

82 100 203

ppm

56 7 3 7

3 8 37 8

58 87 4

4 6 5

127

3 47

pptn187 150

1040 103136

94 102 361 131 358

90 161 171 188196

126 194 187 241 151

140 188173

Ai tem6.2

ppmCO.2

0.4 0.2

CO.2 CO.2

CO.2 CO.2

0.3 0.6 0.2

CO.2 0.2 0.6

c 0.2 CO.2

CO.2 CO.2

0.3 CO.2

0.2

C0.2 CO.2

0.7

CorcpMIhS

ppm37.2 25.5 39.4 75.0 3.0

47.3 39.5 48.4 231

68.4

52.3 CO.5 13.0 34.2 19.4

108 108

29.127.6 31.9

30.9 40.2 12.3

Fb 1CP80

2fpm

15 13 20 34

6 5a

1013

C2 5

171313

7 14 8 9

13

517 15

Znicno0.5

ppm900 89.8 61.3 38.3149*~*W

58.6 42.0 68.9 78.4 62.5

39.6 37.7 159 10}

90.7555114

17.1 36.5 100

53.9 954 ISS

AaICP80

3ppm

14 10

C3 C3 C3

15 9 8 9

10

3 9

13154

C3 8 8 8

13

O 19 22

Mo ICP84)

1ppm

3 O

8 273 4 1 3 5

3 3 3

12 1

6 7 9 7

CI

1 31

Sk ICP80

SppmC5 C5 CS

5C5

C5 CS C5 C5 C5

O C51412 7

O C5 C5 O C5

C5 O10

IV ICP80

10 ppm

10 13

00 0000

ooCIO CJOoo00

oo oo00

1512

15oo ooC 10 C 10

CIO CIO 00

BaICP80

Ippm

180 161

1430 294231601 280 356 96

429

230 306 79

124181

186 155 208 480 56

130 204 67

Mtmtwr of UM SOB Croup (SoollU afcUr*l* d* SirviftaM*)

XRALWork Order: 015684

XRAL LaboratoriesA Dlvltlon of 808 Canada he.

Dale: 03/07/97 FINAL 7 of 9

Element.Mctiwd. Vft. Urn. Unto.

WU 19001 WLI 19002 WLI IJ003 WLI1J004

WL1I9GG6 WL1I9C07 WLII9C08

WLI 19010WLI 1901 1WLI 19012

(WL119013{WiJlWl4IWLII9D15

WLI 19016 WLI 19017

C WLI 1 9011

WLI 19020

19023 LI 19024

WLI 1 9025

WLI 19116 WLI 191 17 WLI 19118 WLI 191 19 WLI 19120

Te S CO! AAK3CHM1UCHM1I4

0.1 0.01 0.01 ppn to Ik

O.I

<0,J

0.3 0.2

0.2 0.2

0,1

0.2

0.1

0.020.080.020.020.03

0.020.030.020.030.01

4:0.01 0.01 0.09 O.OS

410.01

0.120.050.010.030.29

0.01

0.030.270.10

0.1S 0.08 0.04 O.I l

4:0.01

0.060.270.030.170.04

0.01 0.04

4:0.01 0.05 0.05O.IS 0.09 0.02 0.03 0.020.020.280.030.0715.2

0.260.070.050.030.11

0.120.020.260.621.49

r

j cj c

r

l Mimbw of th* SO* 0*mp BocMtt Otrttml* d* SurmlNiitcvl

XRALWork Order: 015684

XRAL LaboratoriesA Dfefelon of SGS Canada Ino.

Date: 03/07/97 FINAL fig* l of 9

Element. Method. Drt.Lhn.Units.

WLI19I21 WU 19122 WU 19! 23 WU 1*124 WLI 19125

WL1I9126 WLI19127 WL119128 WLI 19129 WLI i 9130

WLI 19131WLI 19132WU 19133

SB WU 19134SB WLI 1913 J

•SB &LI19136 WLI 19278 WU 19279 WL119280 WLI 19281

WL119282 WLI 19283 WLI 19284 WLI 19283

-SP) WU 19286WLI 19287 WLI 19288 WLI 19289 WLI 19290 WLI 19291

Te S CO3AAH3 CHM1I2 CHM1I4

0.1 0.01 0,01

•CO. l

0.3

•CO. l

0,1COI

0.5

0.04 001

0.02 O.I l 0.02

0.030.020.050.020.02

0.020.250.030.020.240.010.040.160.020.05

0.020.020.080.600.78

0.250.030.020.030.03

0,030.370.121.520.06

0.03 0.02 0.05 0.27 O.OB

0.08 0.03 0.13 0.03

O.Ol

0.010.310.020.040.53

0.040.040.111.050.16

0.020.030.020.050.06

IMmbM of Hi* BOB Group (Sod** Of ntfrtlk * SwvtHlfcneO

XRALWork Order: 015694

XRAL LaboratoriesA DMilon of 8GS Caned* (no.

Dale: 03/07/97

Element, Method. Dft.Llm. Unite.

Te S CQlAAftt CHM1I2 CHM114

0.1 0.01 0.01ppm 1b K

119292 1 19293 11*294

19295119296

119297119298119299 l (9300

19301SB WU 19302

1 19303 19304

WU 19305 WLI 15306

WL1 19307*Dup WLI 19001*DupWLll90l3*Dup WLI 19025*Dup WLI 19127

*DnpWUI92SO•Dupvu mn*Dup WLI 19304

•CO. CO.

0.'

co!

o!

co.

0.02•CO.Oi

0.030.03

<0.01

0.020.010.030.220.11

0.03CO 01

0.050.030.020.040.020.090.110.02

0.020.020.03

0.060.020.080.020.03

COOIo!o20.040.010.01

0.020.050.020.01

•CO 01

0.020.08

<0 01o! 12<0.01

0.040.010.01

FINAL 9 of 9

Fr

I

o

c

"

C

C

Mantar of ih# SOS Qroup (SoeMtA 6Mr*h dt SunvWMMl

XRALWork Order: 015882

XRAL LaboratoriesA Olviston of SQS Canada Inc.

Date: 22/07/97 FINAL Ptge l of 3

Etontot, Method. Del.LIm. Units.

WL1 19164 WL1 19165 WL1 19166WL119167 WL1 19168WL11920I WL1 19202 WL119203 WL1 19204 WL1 1920SWL1 19206 WL1I9211 WLl 19226WL1 19228

WL1 19229 WL 1 1 9230 WL1 19231 Wtl 19176

Sg, WU 19177

*DopWLl 19164*DupWLl 19226

SIQ2 AI2O3 CaO Map Na2O K2O Fe2O3 MnO TK)2 P2O5 O2O3 LOI Sum Rb XRF102 XRF102 XRF102 XRFJ02 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102

0.01ft63.149.948.354.049.148.063.260.649.153.0

52.447.950.248.551.650.044.950.664.650.0

63.350.3

0.01ft

15.113.713.812.414.88.0815.516.012.512:412.117.311.08.51n.715.09.7215.916.414.9

15.311.0

0.01ft

4.329.8611.28.6510.28.554.269.638.4610.29.128.969.048.418.7010.77.3210.73.4811.2

4:399.05

0.01ft

2.256.8711.63.724.1317.53.001.4511.88.69

9.477.8412.614.010.68.9419.37.602.006.76

232.12.8

0.01ft

3.331.961.322.332.981.014.751.501.941.96

2.683.092.331.582.702.370.602.554.951.883.272.35

0.01ft

2.900.200.270.560.210.051.182.500.200.140.220.340.150.260.280.430.020.202.600.43

2.840.14

0.01ft

6.3014.311.315.115.712.65.275.9613.011.7

11.911.911.814.113.310J12.89.654.6712.4

6.2411.8

0.01ft

0.090.210.170.210.210.210.070.130.210.16

0.160.280.180.190.180.160.180.250.060.190.090.18

0.01ft0.791.590.542.432.110.610.670.540.810.730.710.840.620.570.660.540.550.660.600.910.800.62

0.01ft

0.160.150.040.330.230.030.200.110.060.06

0.080.050.050.030.050.030.020.030.260.07

0.160.05

0.01ft

0.020.030.11

<0 010.020.260.020.020.100.060.100.050.120.160.080.140.360.090.010.04

0.020.13

0.01ft

1.800.750.900.550.403.002.101.102.250.650.701.251.203.501.300.804.351.351.351.201.751.20

0.01ft

100.499.699.5

100.3100.2100.0100.499.6

100.599.999.799.899.499.8

101.199.5

(00.299.6

101.2100.0

(00.799.7

2ppm

959

131275

2847598

H1013181914126520864

Member of ilw SOS Group {SoeMt* (Mnfnrtt d* BiHvriHanct)

a- \j

XRAL XRAL LaboratoriesA Division of 80S Canada Ino.

Work Order: 01S882 Date: 22/07/97 FINAL p* 2 of a

Element. Method. Del.Llm. Units.

\j2 WU 19164S WU 19165g! WU 19166o WL119167? WL119168

^ WL119201 z WL119202 g WU 19203 *- WL119204

WL119205

WL119206WU 19211

Sti WU 19226^^6*1.119227

2 WL119228

i WL1192297 WL119230i WL119231l ^ft 9^1191765 ^R WCl 19177

U

J)

-3

•DopWLl 19164*Dup WU 19226

Sr Y Zr Nb Ba XRF102 XRF102 XRP102 XRF102 XRF102

2ppm58918310719615554

679151153210

33312610984

119

14543

100907151

581102

2ppm

253618744314171718222020191725

1923191924

2314

2ppm16811953

23614155

1761307370

7776626264564864

17977

166. 62

2JJBHH

1075

13937534

52557

610207563

20ppm99012097

36016085

67133812790

108187119100139448

58146969129981123

Cu ICP70

0.5ppm25.095.7

11544.070.728.518.120.157.940.5

51.451.418.3

9929.645.818.054.812.8132

28.918.1.

ZB ICP70

0.5ppm121

24.16.8

40.718.217.950.224.4155

10.48.9

20.015.931.523.66.0

22.713.548.348.0122

16.7

AsICP70

3ppmOOoooo<3Oo

5

oooooooooooo

Mo ICP70

1ppm

42222

•CI341222•^11

l^

122

4*cl

icpri0.2

ppm1:0.2•C 0.2•"i 0.2

0.2•C0.2•C0.2

0.2*C0.2<0.2•C0.2

•C0.2•C 0.2C 0.2

0.3c 0.2•c 0.2

0.20.2

•C0.2•C0.2

-CO 2•C0i2 .

Sb ICP70

5ppm<5<5<5<5•^

<5<5<5<s•C5

<5<5<5<5•C5

<5<S<5<5^

<5<5

B* ICP70

1ppm

5919213510

19441614101419191114

418

184223

5319

Pb ICP70

2ppm

20<2<2

2^^

3<2

9<2

3<2<2

6<2<2<2^

7<2

19<2

W ICP7C

10ppir<10^0<10<10<10

<10^0<IO<IO<10

<10•CIO^0•C 10<IO

<lO•C 10<10<10<10

cioc 10

r— XRALWork Order: 015882

XRAL LaboratoriesA Divfrion of SOS Canada Ino.

Date: 22/07/97 FINAL hge 3of 3

CD•ST

ea

Element. Method. Det.Um. Unite.

WU 1 91 64 WL1 19165 WU 19166 WU 19167 WL119168

WLI19201 WLI 19202 WLI 19203 WLI 19204 WLI 19205

WLH9206 WL119211 JH.1 19226 WL119227 WLI 1 9228

WL119229 WLU9230 WL119231 WLI 19176 WLI 19177

*Dup WLI 19164*DupWL119226

Te S CO2AAH3 CHM112 CHM114

0.1 0.01 0.01ppm % %

Q.I

Oil

0.3

0.020.020.020.070.09

0.020.070.030.300.04

0.030.020.010.440.03

•CO.l

0.030.010.04

0.030.01

0.270.020.050.050.27

*:o.oi0.200.02

•CO.Ol 0.01

<0.01 0.02 0.02 0.03 0.04

0.04^.01

0.17

0.04

0.280.05

CM

CO CD

CO

Mwnbw oftfc* SOB Onwp |8odM (Mnfrito d* SurwMmo^

miiftyH XRAL Laboratoriesmm*m*^*mm A Division of SGS Canada Inc.

Work Order: 015798 Date: 23/07/97

Element. Mftbod.Dcl.Llm.Units.

SBI 19026v/SBI 19027 —————

SBI 19029SBI 19030

SBI 19031SBI 19032SBI 19033

SBI 19035

SB II 9036SBI 19037

SB 119039SBI 19040

SBI 19041, SBII9I37- ——— -—SBII9138SB 1191 39SBI 19140

\JL3RII9M1VUM1 19142SBI 19143—-—-"

SBI 19144

/SBII9146- ——— —. SB 1191 47 ——— ——

' cm lOiJftODI IVMOen li 0140dDI l™!™-*

SBI 19150

FINAL rage 1 of li

SJO2 AI2O3 CaO MaO N*2O K2O Fc2O3 M*O TIO2 MO5 Cr2O3 LOI Sim Rb XRF102 XRF102 XRP101 XRF1M XRF102 XRF102 XRFI02 XRF102 XRF101 XRT102 XRFI02 XRPI02 XRTI02 XRFI02

0.01*50.6—————— 50.7

—————— 49.559.955.6

47.253.0n.a.— ———— 62.5D. a.58.3a.a.in f.a.a.n.a.49.7———— —^50.661.154.651.8

43.463.5——— —— 49.964.6

. —— ——— 51.2— ——— —61.3—— ——— -61.7

52.348.647.2

0.01K

14.313.715.715.715.7

14.813.2o.a.14.6n.a.14.7n.a.1.54n.a.n.a.15.012.714.311.515.318.015.213.714.913.1

14.714.616.215.013.6

0.01"k

9.2210.59.637,2110.S

11.310.2n.a.4.20n.a.7.17n.a.1.13n.a.n.a.

10.89.586.783.1311.214.55.998.065.90II. 0

4.394.53II. 110. 111.9

0.01*

8.037. IS7 ftoi . V7

2.213.40

9.186.14n.a.3.41n.a.

5.62n.a.

An 2TV . t n.a.n.a.

8.056.393.622.019.39

7.492.31S.921.887.18

3.413.414.966.616.32

0.01*2.542.552.394.483.45

1.881.64n.a.4.25n.a.3.70n.a.0.09a.a.n.a.

2.262.702.492.502.33

0.992.923.SO2.972.77

4.554.493.531.802.16

0.01*

0.140.160.940.740.56

0.250.24n.a.3.20n.a.0.55n.a.

•CO.OLn.a.n.a.

0.570.530.760.430.36

0.101.530.591.200.44

3.043.270.621.64059

0.01•k

I3.5I3.0II.57.188.01

12.213.3n.a.5.35n.a.8.08o.a.9.51o.a.n.a.11.415.58.7620.78.00

11.55.8815.57.0812.2

5.635.538.4011.615.7

0.01*

0.180.180.160.150.150.180.30n.a.0.08n.a.

0.15O.a.

0.1504.o.a.

0.180.210.170.280.14O.lf0.090.240.120.19

0.090.080.180.240.33

0.01*

1.160.910.810.610.74

0.660.95n.a.0.51n.a.0.60n.a.

0.09n.a.n.a.

072l.tl0782.170.49

0.830.611.310,520.93

0.630.610.680.710.98

0.01•h

0.120.06Oil0.090.080.040.10n.a.0.32n.a.

0.06o.a.

0.01o.a.n.a.

0.050.090.120.200.07

0.050.130.100.140.13

0.360.360.050050.10

0.01*

0.040.060.060.030.05

0.07o.ota.a.0.03B. a.

0.11n.a.0.26o.a.n.a.

0.050.020.020.020.130.030.020010.020.020.090.020.050.050.09

0.01K

0.600.65l. 70l. 451.85

1.000.95n.a.1.10n.a.1.35n.a.7.95aa.n.a.

0.800.651.250.650.95

2.401.701.050.850.700.951.001.203.851.00

0.01"h100.599.fi

inn iIUII. 499.1

100.2

98.8100. 1

n.a.99.8n.a.

100.4n.a.

100.5n.a.n.a.99.6

100.2100.3100.3100.4

99.4100.1100.0100.2100.0

99499.999.4

100.4100.1

2ppra

96

411819

63

n.a.64

n.a.

20n.a.

3n.a.n.a.

136

3!1616

4312035107482186810

c c rrtca rc ct

3-

yrrDcEi

f^

—t3

g

j:OXo.t

R

-T

M*flibM of t** SCS Group ISotIM Gln4r*li d* SuMttlanc*)

XRALWork Order: 015798

XRAL LaboratoriesA Diviaion of SGS Canada hie.

Date: 23/07/97 FINAL i or 12

Element. Mttbod.Det.Uni.Units.

SBII9I5I USB 119 152SB 119 13 3SBI 19154SBI 19155

SBI 19156 '''' .SBII9I57 ,v,.- . - ;SBI 19158

•/SBI 1 9159— ————— -— -SB 119160 _____ — ——

WL Sftl 19161SBI 19162 ——— ——— ——SB! 19 163 Q,\v.-Vk..USBI 19308^ F- jl - rSBI 19309

SBI 19310SRI 1931 1

, / qo 1 1 yjl f-vSB 1 1931 3 . — ——— - ——— SBI 19314—

ci \ l A, rf SBII93I5- - - f ' --V*SB 1 1 931 6 T- —— — , -

t SB1I93I7 ——— - ———

SBI 19319 —— -— -— ~

S8II9320 v-:-;

SB 1 19312- V,CD 110121jDiiyjtJSB1193H -".M

SiOl AJ20J CaO MgO Nt20 K2O F*2O3 MnO TiOl P2O5 CrtOJ LOI Sum Rb XRFI01 XJtPlOl XRFI02 XRF1W XRF102 XRF102 XRF102 XRFI02 XVF102 XRF1Q2 X RF 102 X RF 102 XRF102 XRPIOl

0.01ft— 70.5

53.053.144.567.0

47.9.7 73.2

48.3——— 45.2—— 46.7

57.5- —— 49.2

' ' -11.254.8

65.647.1

——— 50.0

58.2

-65.2~5fl 1* •~38 7

—— 38J —— 39.2

- 47.2'. . 64 i: 58.8

47.651.1

0.01ft

11.714.713.912.114.4

9.3914.715.116.615.4

16.114.213.58.4412.1

16.911.414.814.215.2

15.416.60.691 on.510 2.26

14.815.215.914.714.4

0.01ft

2.798.8011.19.204.86

12.14.7312.710.310.1

7.7411.810.67.309.02

3.0412.412.110.54.99

4.0211.90.430.453.70

14.23.437.3114.011.7

0.01*1. 217.124.347.321.29

14.20.727.3112.011.7

^i!^9.186.300.634.47

1.1412.58.738 00

• VO

4.82

2.126.5543.8IRAJD.U30.0

6.082.264.025.135.31

0.01ft

2.491.802.301.493.29

III1.520.971.621.68

2.402 121.850.662.49

7.861.011.632.236.52

4.411.920.070.080.05

1.544.924.610.991.26

0.01ft

2.141.140.420.751.13

0.161.560.190.170.13

0.850.110.600.180.25

0.550.550.700.830.31

1.620.23

^0.014?O 01•coioi

0.962.690.180.600.46

0.01ft

6.899.4312.021.55.24

11.52.2312.110.611.5

7.8910.912.43.9112.2

3.0812.09.7211.07.73

4.8610.48.499 -)0.*o 10.7

13.24516.9112.813.7

0.01ft

0.110.200.320.410.09

0.230.030.170.160.16

0.130.180.200.100.19

0.040.190.160.190.13

0.090.150.120.120.12

0.240.060.140.220.22

0.01*

0.490.800.960.790.65

0.540.270.840.480.53

0.560.651.020.411.27

0.350.530.590.760.72

0.570.700.040.110.14

0.840.511.191.051.18

0.01ft

0.100.210.110.090.12

0.050.060.060.030.03

0.090.050.100.060.10

0.050.030.050.070.18

0.150.05

^0.010.020.01

0.070 4ftVf.TV

0.120.090.11

0.01ft

0.030.050.090.050.04

0.260.020.060.110.07

0.040.080.040.030.02

0.010.170.070.070.02

0.020.040.220.271.16

0.050.020.070.11003

0.01ft

2.052.300.902.101.85

1.150.900.501.751.15

1.450.651.001.301.25

0.501.201.55

1.35

1. 75o.as7.5011.913.4

1.051.000.501.100.75

0.01ft

100.699.799.3

IOQ.4100.0

98.6100.098.399.299.2

100.099.199.6

100.3100.2

99.299.1

100.2100. 1100. 1

100.399.6

1001100.3100.7

100.299.499.898.5

1002

2pptn

38373148

436695

154

20O

4

917213113

561516122

4061

61414

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wcu U3O

3 HI i AKHL

t-HA NU.P. U

4/13

g seas" sa**^ ss"*e

n

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ggg-g

85

* 82882

S2S.8S? P

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0

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— —

O

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O—

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0-0

—*^

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00

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a •s

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d

dd

dd

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ddddd

ddddd

oddoo

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i ~

*^" ,

.'^•~"'~

; ^^ —

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^

^: — —

f*l^

! -^"(rf^^.^^^/

^^(j^

^cs

oodod ooodo do'ddo ddood o'ddo'd

o'eado'o*

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ooo-o ooddc! ddddd C--0- ddddd "'dddd

ooooo ooddd ddddd ddddd ooooo dddd

*;ss?s

=fS

Cb S

. O

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-idd

d

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M3.

XRALWork Order: 015798

XRAL LaboratoriesA DlvUion of 8GS Canada Inc.

Dale: 23/07/97 FINAL Page 4 of 12

Elemmf. Method. Def.Llm. Urite.

SI02 AI2O3XRFlOa XRF16Z

0.01 0.01

CaO MfOXRF1W XRF102

0.01 0.01

NalOXRF102

•.01K2O

XRF102 •.01

FelOJ XRFI02

0,01

MnO XRF1W

0.91

•Dup5BM9323•Pup SB 119337•DupSBM9349

48.850.346.6

15.513.) 7.78

10.911.0a. 54

8.047.0111.4

2.2S 2.55 0.44

0.880.350.04

11.212.413,1

0.160.270.22

no?XRFIOJ

0.01Ik

0.650.990.52

P2O5 XRF102

0.01•h o.os0.110.05

CrtO3XRF102

0.01

0.100.040.25

LOIXRFJ02

0.01

1.650.703.00

Sum XRFlOt

0.01

100.299.099.0

Rb XRF102

2 P?ra

567

c 4:c

c o

Mf mb*r tt Ihl SOS Groip (SocIM G*nl(*t* rf* Survtillanot

XRALWork Order: 015798

Eltmcat. Method. Drt.Llm. Units.

SB]19026 SB 11902 7 SB 119028 SBJl9029 SB1190 30

SBI1903I SB! 19032 SB119033 SB 119034 SBII9035

SB) 19036 SB 119037 SBI19038 SB119039 SBI 19040

SBI 19041 SBI 19137 SBI 19138 SBI 19139 SBI 19140

Wt- Hi 19141VJLM1I9I42

SBI 19143SBI 19144SBI 19145

SBI 19146 SBI19I47 SBI1914B SB119I49 SB 119150

XRAL LaboratoriesA Division of SOS Canada Inc.

Dale: 23/07/97

Sk-

FINAL5 oftt

XRFI02 XRFI432 XRF102 XRF102 2221

ppm ppm ppm ppm

153 35 100 8 120 25 g4 15286 21 8J 7 149 12 |35 3 277 21 108 5155 113

K. a. 777n.a.

232 n.a.

9aa.n. a.

119129 414 92

295

172394 200 204 394

844 893 168 98

174

20 27

n.a. 21

o. a.IH

n.a. 2

n.a. n.a.

22 28 26 52 16

2110 34 15 25

28 26 18 20 31

5583

n.a. 174 n.a.95

o.a. 20

o.a. n.a.

65 89

136 163 79

58120 101 12384

185 185 76 67 84

5C2

n.a.7

n.a.

4n.a.

5 n.a. n.a.

3 3 7 6 5

3 54 4 6

9 8 527

BaXRF102

20 ppm

117 93

280 195193

96107 n.a.

1040 •.a.195 n.a.

63n.a. n.a.

128 137 329 175 186

98 381 206 280 241

1070 1060 213 317 215

icprS0.2

ppm

C0.2 0.20.2 O.2 O.2•C 0.2 C0.2 C0.2 0.20.20.2 O.2 0.2 02 0.2

O.2 C 0.2 0.2 O.2 02

O.2 O.2 0.2 0.2 0.2

O.2 0.2 0.2 0.2 0.2

Cv ICP70

0.5ppm

63.0 16.2 59.1 59.4 55.8102

85.7 46.6 13.0 329

32.4 15.5 12.3 101

87.5

86.2 12.1 20.6 16.5 32.4

64.7 25.6 123 8.0

41.8

43.0 13.2 89.8 215

80.7

Pb ICP70

2 ppmC2C2

3 6

C2

C2 O

2 C2

7

38 3 2 2

2 ^

4 4

O

3C2

3 3 2

2 ^ O

6 C2

Za ICP70

9.5 ppm

15.9 6.3

21.2 78.0 23.8

11.8 II 8 12.6 29.5 23.2

12.3 IS.6 33.5 17.2 8.0

LI. 3 10.1 19.6 36.1 7.6

10.6 53.334.146.5 87. r

31.7 23.2 9.0

30.6 17.4

AsICP70

3ppraC3 O Oooo0o o oo o c3 o o0o0o ooo o ooo0o oo

Mo ICP79

1ppn

33 2 4344 4 4 3

37 2 1 2

1 3 4 67

45252

4 3 3 3

10

Sb W ICP70 ICP70

5 10PPM ppm

C5 000 00o oo^ 000 Ofl

^ 00^ oo^ 00^ oo0 00

o oo^ 00 ^ 00 0 00 0 00

^ 00 0 00o oo o oo^ CIO

0 CIO C5 CIO ^ CIO 0 CIOC5 CIO

C5 00^ oo^ 00 C5 00ci oo

Ba ICP70

1 ppra

6 2

12 1913

8 14 7

171Qto

13 95 9

12

14 8

52 48 35

10 100

17 661825 30

6 102 42

M*mb*r of Ih* SOS Group ttotllM G*n4'*fe d. SurvilHinc.l

XRALWork Order: 015798

XRAL LaboratoriesA Divillon of SOS Canada Inc.

Date: 23/07/97 FINAL 4 of ii

Element. Melted. Dd.Llm. Unite.

SBH915I SB 1 1 91 52 SB 1 191 S3 SBI 19154 SB 1 19155

SB l i 9156 SB 1 1 9157 SB H 9 158 SBI 19159 SBI 19160

Ml 19161 SBI 19162 SBI 19163 SB 1 19308 SB 1 1 9309

SB 1 1 9310 SBI 1931 1 SBI 1 9312 SB) 19313 SBI 19314

SBI 19315 SBI 19316 SBI 19317 SB 1 1 931 8 SBI 19319

SBU9320 SB1I9321 SBI 1 93*2 SB 1 1 9323 SB 1 1 9324

Sr Y Zf Nb B. XRF102 XRFM2 XRTI02 X RF 102 XRF102

2ppm

12)348257109340

841957685

122

1831112185180

550160195194262

318126

171248

1991410

193181112

2ppm

1021273410

152

2011II

1317281831

C213162318

2320

C22

C2

2725282931

1ppm

101969474

127

5197614847

99608776

114

171455870

177

14965172527

632011267485

2ppm

C25

C263

36342

242534

C2469

7141210

8487

173

20ppm

669373145252295

78337Lil10170

25411022366

152

439149218262127

337115718956

2971370335324218

ICP700.2

ppm

0.2CO.2CO.2

0.2•C0.2

•CO. ZC 0.2C 0.2CO.2CO.2

CO.2CO.2C0.2<0 2•CO.2

•CO.2C0.2•C02CO.2CO.2

C 0.2C0.2•cO.2CO.2CO.2

C 0.2CO.2CO 2CO.2C0.2

C*ICP70

0.5ppm

72.695.359.2356

36.3

24.53.5

79.54.6

31.0

41.467.342.816.826.4

3.433.994.2178

29.5

13.083.33.96.1

12.9

75.723.621.966.759.0

PbICP70

2ppm

7C2

252

C22

C2C2C2

C2C2C2

2C2

2C2C2C2C2

3C2

436

44

C2C2C2

Zi ICP7D

0.5ppm

91.136.814.627.555.9

13.222.65.2

ll.fl6.6

43.45.7

14.024.2L4.8

8.414.327.523.212.1

34.425.246.241.819.9

30.550.79.4

17.010.3

Ai ICP7B

3ppmC3c3C3C3C3

C3CiC3OC3

c3C3C3C3C3

C3c3•C3^^C3C3c3C339

^C3OC3C3

Mo ICP70

1ppm

716424

2532232392

52222

423

*:l

13354

Sb ICP70

5ppm

C5csc5^5C5

C5C5< jC5C5

c5C5C5C5<5

C5c5C5C5<5

<5C5CiC5CS

C5C5C5C5C5

W ICP7d

10ppm

CIOClOCIOCIOclOCIOCIOCIOCIOCIO

CIOCIOClOCIOClO

CIOclOCIOCIOClO

CIOClOCIOCIOClO

CIOCIOClOCIOCIO

Ba1CP70

1ppm133114

161087

599

9II8

185

1777

9192030

8

14163

103

2465242619

Mimber oHh. SOS Oroup (SocKM Q4n4ri!i d*Sinv*fltonc*)

XRALWork Order: 015798

Element. Method. Oet.l.ln.UniU.

SDI19325 SBI19326 SB 119327 SRI 19328 SBI 19329

SBI 19330 SBI 19331 SBI 19332 SBI 19333 SBI 19334

SB 119335 SB 119336 SBI 193)7 SB 119318 SB 1193)9

SBI19310 SBI 19341 SB 119342 SBI 19343 SB 119344

SB 119345 SBI19346 SBI 19347 SB! 19348 SBI 19349

*Dop SBI 19026*DupSBI19038*Dup SBI 19145*Dup SBI 19157*Dup SBI 19313

XRAL LaboratoriesA Division of 80S Canada Inc.

Date: 23/07W FINALPage 7 of 12

Sr V Zr Nb Ka XRFI02 XHFI02 XRF102 XRFI02 XRF102 1 2 2 l 20

ppm ppm ppm ppm ppm•ytfi * ** - -4JV297 200 161 117117J57 153 271 145

146 314 III 146 53

176 134 172 252 163

1230 124 74ti 154

19

152 10

389 195 194

id 22 2131 28

23 20 27 19 25

2126 28 2615

13 38 36 1827

33 18 26 22 14

37 3

21 2

24

61 97 64 90 83

NO 94 76 81 65

63 92 9163

109

78 104 98 58 83

178 64

200 6250

101 20 1497 69

2 6 3 3 2

6 12 52S

4 S 54 6

3 5 2 2 3

9 4

13 9 4

10 74 7 7

236 425 377182 115

252 315 119 127 124

149 317 111 140 649

297 338144 283 135

1050 116 418 205

55

112 65

224 337 265

icrA0.2

ppm•:0.2 *:0.2 *:0.2 C 0.2 ^2•C0.2 c 0.2 *:o.2 c: 0.2 C02C 0.2 •:0.2 ^.2 *:0.2 c 0.2*C0.2 *C0.2 f. 0.2 *:0.2*:o.2*:o.2 •C0.2 •C0.2 •C0.2 •s:0.2

•C 0.2 "C0.2*;o.2 *;o.2 *:0.2

Cu ICP70

0.5ppm

52.4 114

31.6 93.1 62.1

52.2 50.4 85.8 13.1 83.4

134 68.1 64.7 32.9 46.9

27.9 15.0 11.5 960 134

26.1 103

45.9 45.3 79.2

62.9 11.7 42.8 3.5 174

Pb1CP70

2 ppn

2 2

^ ^

32 3 2

C2^16 3

^ ^

17

C2 0 O <2

2

4 2 8

<^ ^

3 6

^O O

Zm ICP70

0.5PPM

80 28.1 9.3

13.9 14.3

64.9 25.8 13.7 7.9

11.6

11.4 26.1 10.5 9.0

59.0

20.9 9.1

17.0 5.7

14.7

44.2 25.8 12.3 7.3

17.2

14.831.4 8.6

21.0 21.9

AsICP70

3 ppm

O0 O Oooo0o0

o o oo

o o0o oo o o o oo o o o o

MoICP70

I"pD!

2 4 332

4 1 1 2 2

8 2 5 2 6

2 22 2 2

32 2 21

J1 1 5 2

Sb W ICP70 ICP70

S 10ppm ppia

O 00 ^ 00 ^ OO 0 00 ^ cio^ OQ ^ 00 ^ 00 ^ 00 0 00^ 00 ^ 00 0 000 00 ^ CIO

0 CIO ^ CIOo cio0 00 ^ 00

0 00 ^ CIO ^ CIO ^ 00 0 00

^ 00 ^ 00 0 00 0 00 0 00

Ba ICP70

1ppin

13 118

13 10 4

105 32 5

12 9

29 16 11 12 26

17 H 5

15 7

45 13 13 13 9

56

19 10030

M*mb*r of ik. 80S Group (SocJfti GMnff * Su rv,ui.nMl

XRALWork Order: 015798

XRAL LaboratoriesA Division of SOS Canada Inc.

Date: 23/07/97 FINAL F*S* l of uElement. Method. Det.Llm. Unite.

*DvpSBII932S•Dap SB 119337 'Dtp S8119349

Sr Y Zr Nb Da XRF102 XRF101 XRFI02 XRTI02 XRPI02

2 2 2 2 20ppm251 113

14

ppm21 309

ppm61 8950

ppm4 52

ppm232 10476

ICPll OJ

ppmC 0.2 -C 0.2

02

CuICP70

0.5ppm54.0 62.777.6

Pb ICP70

2ppm<2 <2

2

Zn ICT70

0.5ppm

8.3 9.9

15.1

AsICP70

3ppmO 00

MoICP70

1ppm

25

<\

^ Sb w Ba ICP70 ICP70 ICP70S 10 |

ppm ppm ppm<5 CIO |4<5 <IO (t<5 <W g

^ 5r

C

x o

u fu f\

c (f

Mcmbor of lh*SGSfeo*p (SocWl* CHnttutt O* SurvfHkco*)

XRALWork Order: 015798

Haunt. Method. Del. Urn. Unite.

SBI 19026 SB 1 19017 SBI 19028 SBI 19029 SBI 1 9030

SBI 19091 SBI 19032 SBI 19033 501 19034 SB 1 19035

SBI 19036 SBI 19037 SBI I90J8 SB! 19039 SB 1 19040

SBI 1904 1 SBI 19137 SBI 19138 SB119I39 SBI 19 140

Vv;uSftH9l42 SBI 191(3 SBI 19144 SBII9145

SBU9I46 SBI 19147 SBI 19148 SBI 19149 SBI 19150

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 23/07/97

Te S C02AAJ13 CHMI12CHM114

0.1 0.4)1 C.OIppm % *!t

<0.<Q.<0.<0.<0.

•CO.0.

xJO.<0.

0.5

<0.0.2

<Q.*^0

0.3

<0.<0.<0

0.<0.

<0.•co!<o.-co.<0.

<0.<0.<0.

Q.0.

I 0.03<dol

0.090 11007

0.040.06o.a.

0.03n.a.

o.nn.a.0.04n.i.DJ

0.040.020.020.05

•C 0.01

0.060.020.11

<aol0.07

0.010.010.020.380.15

0.050.020.100.64I.OS

0.150.24n.a.

0.02o.a.

002n.a.049n.a.d. a.

0.010.020.02001O.OJ

0.010.180.100.040.02

0.110190.602.360.04

FINAL P*te 9 of 12

c 3

3

r3 C

-\ 3

j. Cf O

or\

c ^o

M*mb*f M tit* SOS Group UocMttf Gtniul* e* Su(viffl*nc*)

XRALWork Order: 015798

XRAL LaboratoriesA Divliion of SGS Canada Inc.

Date: 23/07/97

Element. Method. Det.Um.Units.

sen 9i51SBI19152 SBI 19153 SBI 19154 SBI 19155

SBI 19136 SBII9IS7 SOI 19158 SBI 19139 SBI 19160

VL )Q119151 SBI 19162 SBI 19163 SBI1930S SBI 19309

SB 119310 SB 119311 SBI 19312 SBI 19313 SBI 19314

SB119313 SBI 19316 SB 119317 SBU9318 SB 119319

SB 119320 SBI 19311 SB 119312 SB 119323 SB l I93H

T* S CO2 AAH3CHMII2CHMI14

0.1 0.01 9.01 ppnt % %

0.'o.;*:0.0.*co.

<o.<0.<0.<0.*:o.<o.<o.<0.<o.o.:*:o.

0.<o.0.^.

<O.J<0.<0.<0.

0.^

<0.<0.<0.<0.*CO.

t 0.34l 0.36

0.110.930.36

0.01•C 0.01

0.03O 01

0.02

0.030.020.02

1 0.05l 0.03

0.03•CO.OI

0.01O.H0.01

0.030.030.010.040.13

0.030.080.030.020.03

O.OJ0.020.160.300.11

0.060010.020.010.02

0.360.020190.52O.S9

0.030.280.050.030.03

0.030.030.430.484.14

0.240.160.040.240.12

FINAL PH* 10 or 12

Cf j: V

K

tfeitibM of td* SQS Gimp (SocUM G tntrmlt tt SurvtHlf *M|

XRALWork Order: 015798

XRAL LaboratoriesA Division of SGS Canada Inc.

Date: 23/07/97

Element. Method.Det.Llm. UuMs.

SB119325 SB119326 SB! 19327 SB 119328 SBI19329

SB 119330 SBI 19331 SBI 19332 SBI 19333 SB 119334

SBI 19335 SB 119336 SBI 19317 SB 119338 SB 119339

SBI 19340 SBI 19341 SB 119342 SB 119313 SBH93H

SBI 19345 SBI 19346 SBI 19347 SBI 19348 SBI 19349

*DupSBH9026*DupS8ll9G3S*DupS8ll9l45*DupSBII9l57*DupSBH93l3

Te S C02 AAH3CHM1I2CHM114

0.1 0.01 0.01 ppm fa *k

co.iCO.l CO.l CO.l

0.1:o.i0.2

•CO.l 0.)

CO.l

O.I 0.1

0.030.050.020.080.05

0.090.040.070020.02

0.030.020.040.010.61

0.040.020.020.140.17

0.090.060.060.020.10

0.030.050.070.010.15

0.400.040.220.360.06

0.060.030.230.030.03

0020.030.230.210.02

0.020.020.040.050.09

0.060.040.020.060.04

0.04 0.48 0.02

C 0.01 0.03

FINAL Pigcll of 12

r

j:

C f J. CI

o r*

Mmter of thn SOB Oroup (Soeltlt G4n*ril* 4* Sinveiflinc*)

KRAL

Work Order: 015798

KRAL LaboratoriesA Diviiion of SGS Cinad* Inc.

Date: 23/07/97 FINAL P*|*I2 of 12

EltOlMl.Mclbod.

Unlla.

Tc S C02AAH3CHMII2CHM114

0.1 0.01 0.01ppm I K

c. Crrc

3r

ccJ J

*DupSBl|932S*DupSBlt9337*DupS8M9349

0,030.040.10

0.390.230.03 r

DC

5 c

r

c4- t.c

M*mbw •rtH* SOS Group ISocMl* G4*4r.t* d* Su/vsHUnoo)

i a l l

^sj

sssa

?-A

—

—Z

— —

..

..M

UZ

^S

'S

&W

hft

. fe

i*:

OO

OO

O

OO

oZ

o

OO

—O

O

pp

Zp

p

po

ZsJO

O

OO

OZ

#sppppp pppZp ppppp ppZo ooZoo ooooZ

8=88

3 SJ

o?-l8

B

sJ

sSs

op

op

p

pZ

p

oo

oo

o

o.Z

oo

o

oZ

oo

o

ow

oZ

ooooo OooZo ooooo ooZoo ooZoo ooooZ

poooo eoSKao ooZoo ooooZ

* (A

to

wM

MU

i M

bar

OB*

O

BO\r

a?!^

Tl

TO

g

ni /

?n 'J

7CT

hCft

hOT

h 'A

M

VU

JCT

3 T M

n 1 U

UnO

UT

HU

UV

Tr

t "7

^-00

T\

i i

to

-j-j

nnti

Work Order: 016102

gf L LaboratoriesA Dlvlcfcm of SOS Canada Inc.

Date; 22/08/97 FINAL Fige 2 of 6

Etenicnl. Method. Dd.LJm. UniU.

WLI 19401 WLI 19409 WLI 19410 WLI ISM) l SB 119362

5B119363 ' SBI19364 SB 119365 SB 119366 SBII9367

SB 119368 SBI 19369 SB119370 WLI 19371 WLI 19372WLI 19373 WLI 19374 WLI 19375 WLI 19376 WLI 19377

*DupSBH9l79*Dup SBI 19250*Dup WLI 19402*Dup SBI 19364*Dup WLI 19376

S1O1XRF101

0.01ft

47.3v/46.6

S0.8N.A.

t^47.Sv-^S-O

N.A.^*5.1

55.653.1N.A.52.451.0

/47.850.950.14B.250.9

X47.050.9N.A.N.A.45.0N.A.47.0

AI2O3XRF102

0.01%14.27.3614.5

N.A.10.6

10.0N.A.10914.111.3

N.A.15.115.35.3214.4

15.414.514.69.1115.1

N.A.N.A.10.7

N.A.9.13

CoOXRF101 XI

0.01ft

10,58.1811.6

N.A.7.62

7.46N.A.6.859.2710. 1

N.A.11.210.02.3810.0

10.89.6410.58.4510.6

N.A.N.A.12.2

N.A,8.43

MgOUTQ2

0.01ft

9.8620.77.77N.A.15.9

18.4N.A.17.06.7411.1

N.A.6.427.4226A8.337.808.887.3818.17.57N.A.N.A.9.65N.A.18.0

Na2OXRF102

0.01ft

1.910.352.30N.A.1.931.15

N.A.1.303.012.82

N.A.2.313.18O.L52.68

2.962.132.121.113.16

N.A.N.A.1.26

N.A.1.12

K2OXRP102

0.01ft

0.370.020.20

N.A.0.47

0.21N.A.2.450.370.29

N.A.0.290.530.030.250.440.360.460.060.45N.A.N.A.0.30N.A.0.06

FcZOJXJUT102

•41ft

13.111.310.3

N.A.12.5

12.4N.A.12.59.388.18

N.A.9.0610.511.110.810.414.111.412.09.73

N.A.N.A.16.8

N.A.12.0

MnOXRF102

0.01ft

0.260.190.23N.A.0.18

0.18N.A.0.160.120.14

N-A.0.200.230.130.200.230.230.250.190.20

N.A.N.A.0.41N.A.0.19

TIOZXRF10Z

0.01ft

0.620.370.67N.A.0.59

0.60N.A.0.630.730.56N.A.0.710.730.310.610.730.760.600.460.70N.A.N.A.0.53N.A.0.46

F205XRP102

0.01ft

0.040.03004N.A.0.040.04N.A.0.050.110.16

N.A.0.210.050.020.030.050.050.040.030.05N.A.KA.0.03N.A.0.03

Cr2O3XJRF102

0.01ft

0.080.280.05M. A.0.25

0.21N.A.0.290.070.13

N.A.0.050.050.460.01

0.050.060.09OJ50.07

N.A.N.A.0.54N.A.0.35

LOIXRF102

0.01ft

J.203.950.65N.A.2.803.95

N.A.2.250.750.90

N.A.0.651.005.901050.750.850.853.050.75

N.A.N.A.2.00N.A.3.10

SumXRF102

0.01ft

99.699.399.1N.A.100.499.7N.A.99.6

100.398.9N.A.98.6

100.0100.499.4

99.899.899.399.999.4

N.A.N.A.99.5N.A.99.8

RbXRF?

2ppm

1736

N.A.20

12N.A.

1011410

N.A.1120

27

1212124

12N.A.N.A.

8N.A.

5

M*mb.f el Ih* SOS GKwp {SocMl* 6*ft4'*l4 d* RurveBino*)

XRALWork Order: 016102

XRAL LaboratoriesA DlvUlon of 8G8 Canada Inc.

Date: 22/08/97 FINAL 3 of i

Ekman. Method. Dcl.Ura. Unlu.

SB 119179 SB 119110 SBI19111 SBII9II2 SBI 19113

SBI 19114 SBI 19185 SBI 19186 SBI 191*7 SBI 19188

1918919190

SBI 19250 WL119191 WU 19192

WU 19193WL119194WL119I95

SB fei 19196**6 WLI19I97

WL119198 WLU9I99 WL119200 WLI19401 WL119402

WLI 19403 WLI 19404 WLI 1940S WLU9406 WL119407

STXRP7

1PR*

N.A. 4244

1547822

50SN.A.

3850

14071

N.A.1754

3714588

3291020

71N.A.

626117

9014532192

YXRF7

1ppm

faVll'(412

87

N.A.10109

12N.A.

912

81013IIO

15N.A.

659

126

108

14

ZrXRF7

3ppm

Cj06/6543

25127

N.A.2936

3835

N.A.3141

36513987

154

48N.A.

221933

3825342846

MbXRF7

2ppm

N.A.4 732

34

N.A.<2^

3<2

N.A.22

3<1^2

44

3N.A.

<223

442

334

BlXRF?

20ppm

/2T\4638

741610N.A.

504091

196N.A.

2922

5893

577186944

87N.A.

222689

662155

<J:Q

146

CrICPUO

1ppm1210N.A. N.A.N.A.N.A.

N.A.N.A.

168N.A.N.A.

N.A.N.A.1200N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.190

N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

NlICP88

1ppm

505N.A. N.A.N.A.N.A.

N.A.N.A.

76N.A.N.A.

N.A.N.A.

648N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.58

N.A.N.AN.A.

N.A.N.A.N.A.N.A.N.A.

CuICP80

0.5ppm48,620.4 18.893.9

*:0.5

14.9<0.539.44.6

*C0.5

13742.)90.1260

52.9

15.627.664.253.355.0

62.774.720.820.050.6

57.435.321.1

6*6

Znicrw9.5

ppm

65.8 194 263130

77.7

13374.190.568.373.2

69.274.940.464.664.071.367.164.457.869.2

64.063.847.656.473.1

59.7146

73.567.369.3

As[CF80

3ppmO O

90O

Ooooooooooooo

B10

37

^30Ooo

8O

6

MoICP80

tppm

3 1 12•ci

22721

93212

12l35

23882

310232

At1CF80

0.2ppm

•C 0.2 <0.2 ^0 2•C 0.2

•^0.2

*IO 2C 0.2•C0.2

•C 0.2^g.2^0.2*I0.2^0.2

^0.2^Q,2^0.2<0.2*C0.2

O2O.2

^5.2*:o.2^.2^.2O.2*C0.2"C0.2

Sbreno5

ppm

cio^JJ^J<5<5

i* 5^5<5<5

^^j<5<5

<5

^<5

<5^5<5O

BaICP80

1ppm

25

693363

1630322

613963

172822064

3980

494159864

2517319II60

53li43

571131

l Mwnber olth*SflSGroup(3oot*t*04n**lidt 8urv*ltlinc*|

XRALWork Order: 016102

XRAL LaboratoriesA Division of SOS CtMda tno.

Date: 22/08/97 FINAL hgu 4 of 6

Element. Method. Del.Un. Units.

WLI 1940S WLI19409 WLI 19410 WLI 19411 SB 119362

SBl19363 SBl19364 SB i 19365 9B119366 SB 119367

SBll9368 SBl19369 SBl 19370 WLI 19371 WLI 19)72WLI 19373 WLI 19374 WLU937S WLI 19376 WLI 19377"Oro SBl 19179*Dvp SBl 19230*Dup WLI 19402*DroSBU9354 'Dtp WLI 19376

SrXRF7

2ppio

583494

N.A.113

59N.A.

49251600

N.A.132207

23172

22168

13658

106

N.A.N.A.

18N.A.

58

VXRFT

2PH"

124

14N.A.

II

10N.A.

1511f

N.A.1415

37

1113Hf

13

NANA

10NA

5

ZrXRP7

3ppm

392344

NA43

39NA.

4492

112

NA.50492238

5046373043

NA.NA.

34NA.

29

NbXRF?

2ppm4:24:2

4N.A.

2

2N.A.

254

N.A.2322

33232

N.A.N.A.

2NA.

3

B*XRF7

2ftppm

213^0213

NA.103

55N.A.

59089

165

N.A.167155

OO93

11311610937

291

NA.N.A.

88NA.

36

CrICP80

1ppm

NA.N.A.N.A.

106N.A.

NA1120N.A.N.A.NA.

130NA.NA.NA.NA.

N.A.N.A.NA.NA.N.A.

13401050NA.1260N.A.

M1CP80

1ppn

NA.NANA

38NA.

NA.336

NA.NA.NA.

15NA.NA.NA.NA.

NA.N.A.NA.NA.NA.

444654

NA.334

NA.

Cuicrao0.5

ppn

27.216.243.9

101*I0.5

4:0.548.824.631.212.648.290.053.819.788.6

90.182.062.979.629.3

45.1100

50.446.874.1

ZnICP80

0.5ppn

71.561.258.3

10363.1

62.3113

59.832.853.037.447.760.858.854.1

68.977.658.053.255.S

64.241.385.0

11761.5

AtICP80

3ppm

11OO

3O

OO

96

O6

OOOO

9O

9OO

3OOoo

MoICP8D

1ppm

1l33

O

22142

*C131*:i2

23322

22322

ABICF80

0.2ppm

*:0.2*:0.2•cO.2"C0.2*:o.2*C0.2^.2•?0.2*:o.2*C0.2^.2-:0.2*C0.2*:o.2•C0.2

•C0.2•C0.2-C0.24:0.2^.2

^.2•C0.2*:0.24:0.2410.2

SbICP80

5ppm

415O4:5O^OOO4J54:54T5<5<5<5<5

0OOO<5

OO4TJ<5<5

BaICP80

1ppm360186195206

83

325

38489

184

501235206

669

21728410127

243

316070

729

l MwnbM of Ut* SOS Onuo BocMM Gtiririb d* SvrmHmc*!

KRALWork Order: 016102

KRAL LaboratoriesA Division of SGS Canada Inc.

Date: 22/08/97 FINAL 5 or 6

Element. Method. Dct.Um. Vain.

SB1 19179 SB1 19180 SB! 1918 l SBI 19182 S8II9I83

SBI 19184 SBM918S SBI 19186 S81 19187 S81 19188

VI L. SBI 19190 SBI 19250 WU 191 91 WL1 19192

WLI19193 WLII9I94 WL119I95

l 19196 119197

WL1 19198 WLI 19199 WU 19200 WLI 1940 1 WLI 19402

WLI 19403 WLI 1 9404 WLI 19405 WLI 19406 WLI19407

wICPJO

10ppm

000000oo00

OOOO00OOoo00OOOO00OO

00OO00OO 00

0000OOK 1000

000000OOOO

Pbicno2

ppm1113221812

141322

912

10128

1212

121417

81214131118

916151315

Te s C02AAH3CHM1I2CHM114

0,1ppm

0,2 .O.I•CO. t0.1O.I

O.IO.IO.IO.IO.IO.IO.IO.I

O.Io.tO.IO.IO.IO.I O.I

o.tOJO.I0.10.3

O.I0.2

O.IO.IO.I

0.01*N.A.6.070.030.23

O.OI

0.03O.01

N.A.0.01

O 01

0030.03

N.A.0.100.44

0.010.110.010.04 0.04

O.OIN.A.0.070.070.29

0.020.400.06

•C 0.01O.OI

O.OI%

N.A.0.040.050.020.03

0.020.04N.A.0.020.03

0.880.07

N.A.0.040.04

0.070.030.020.06 0.30

0.03N.A.0.720.770.60

0.670.020.040.02O.IS

c4 Jt.*-

r

l Mwntwr of MM SOS Group (SoeMtt 34nferi* 4. SunrtlftoKrt

XRALWork Order: 016102

XRAL LaboratoriesA Division of SOS Canada bio.

Date: 22/08/97 FINAL P*|e 6 of

EJencnf. Method. DH.LIm. IMU.

WL119408 WU 19409 WL119410 WL1194II SB119362

SB119363 SBI19364 SBII936S SBI19366 SBI 19367SBI19368 SBI 19369 SBI 19370 WU 19371 WU 19372WU 19373 WLI19374 WU 19375 WU 19376 WU 19377

'Dap SB 119179*Dip SBI 19250*Dop WLI 19402*Dyp SBI 19364*DupWLL 19376

Wicno10

ppm<IO<IO<IO00<IO

<IO<10<10<10•cio0000000000

oo<10<10<IO00

<IO<10<10<10oo

H)tent2

ppm

1613122815

(8131415132515171015

1118121314

1610191616

Te 5 CO2AAH3CHMII2CHMII4

0.1 0.01ppm *

<0.<0.<0.

0.2•co.<0.<0.<0.•co.<0.

0.(CO.CO.

0.CO.

co.0.co.

co.co.0.co.0."

•co.co.

•CO.OI<O.OI<O.OI

N.A.o.os0.03

N.A.0.050.03

C 0.01

N.A.0.02

C 0.010.110.04

0.070.020.020.140.01

N.A,N.A.0.28N.A.0.13

0.01Ik

0.030.080.09N.A.0.04

0.02N.A.0.020.020.03

N.A.0.040.010.600.07

0.070.030.040.030.02

N.A.N.A.0.58N.A,0.02

Mrnibir of *M 803 G**p (Socttt* Qlntota d* 9urv*MMiM)

LO O XRAL

Work Order: 016398

XRAL LaboratoriesA Division of SOS Canada Inc.

Date: 26/08/97 FINAL Pile l of 9

CVJ LO

LO *5T

CO

Element. Method. Det.Llra. Units.

,, SB Wtl 19412-WO —— WU 19413

r WLI 19414WL1 19415MLH9416

WLI 19417 WLI 19418 WLI 19419 WLI 19420 WLI 19421

/A*— SB r SB

SI

CD

iS

WLI 19422 WLI 19423 WLI 19424

119425 SBl 19426

— SB119427—58119428

r SBl 19429 SB1 19430 . SBl 19431

SB119432 SB119433 SBl 19434 SBl 19435 SBl 19436

SB119437 SBl 19438 SBl 19439 SBl 19440 SBI19441

S101 A1203 CaO Mop Na2O K2O Fe2O3 MoO TIO2 RO5 Cr2O3 LOI Sim XRF102 XRF102 XRF102 XRFI02 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102

0.01ft

48.945.5

N.A.70.952.952.1

N.A.N.A.49.4N.A.46.6

N.A.N.A.53.449.351.151.4

178.03— +P

69.671.2N.A.N.A.68.672.449.371.5N.A.N.A.51.2

0.01*

12.07.77N.A.16.915.915.3

N.A.N.A.16.0

N.A.11.4

N.A.N.A.14.313.316313.915.315.610.6

N.A.N.A.14.314.513.214.6

N.A.N.A.15.7

0.01ft

6.927.47N.A.1.0110.98.96

N.A.N.A.9.03N.A.7.82N.A.N.A.9.359.189.969.45

(^j!662.822.29N.A.N.A.2.712.618.841.47

N.A.N.A.11.9

0.01ft

12.220.8

N.A.0.385.965.64

N.A.N.A.8.27

N.A.14.5

N.A.N.A.5.144.314.824.80

"2.!881.212.79N.A.N.A.1.790.564.500.95N.A.N.A.4.04

0.01ft

2.710.35

N.A.8.852.503.48N.A.N.A.3.14

N.A.1.82

N.A.N.A.2.662.723.843.69 1.983.494.610.69N.A.N.A.3.803.312.274.56N.A.N.A.0.72

0.01ft

0.260.07N.A.0.250.380.23

N.A.N.A.0.93N.A.0.17NA.N.A.0.330.710.83jrfb

^fl!831.960.39N.A.N.A.1.991680.903.44N.A.N.A.0.94

0.01ft

13.612.1

N.A.0.909.5312.4

N.A.N.A.10.3

N.A.13.5

N.A.N.A.11.317.410.1

d&b5.912.38831N.A,NA.4.972.0417.12.01N.A.N.A.13.0

0.01ft

0.170.22

N.A.<Q 01

0.210.25

N.A.N.A,0.27

N.A.0.20

N.A.N.A.0.250.440.230.18 0.040.080.030.10NA.NA.0.060.010.400.02NA.NA.0.25

0.01ft

0.690.40NA.0.140.750.68N.A.NA.0.70NA.0.68

N.A.NA.1.251.540.801.54 0.370.690.350.28NA.NA.0.510.251.580.26NA.NA.0.81

0.01ft

0.050.03NA.0.010.040.03NA.NA.0.05NA.0.04NA.NA.0.090.10

0.050.15 0.160360.110.07NA.NA.0.150.070.120.07NA.NA.0.06

0.01ft0.140.35NA.0.020.050.04NA.NA.0.11NA.0.16N.A.N.A.0.030.020.050.02 0.050.030.020.03NA.NA.0.07.0.020.020.02NA.NA.0.05

0.01ft

2.404.40NA.0.350.650.60NA.NA.0.95N.A.2.90NA.NA.1.001.051.952.05 1.602.150.803.55NA.NA.0.950.402.001.05

NA.NA.1.20

0.01ft100.199.5

NA.99.799.799.7NA.NA.99.1NA.99.8N.A,NA.99.2

100.0100.1*99'799^499.5

100.3NA.NA.99.999.9

100.3100.0NA.N.A.99.9

PP

22336

MMntwr of ft* SOS Group (SeeMtft Gfcrfrtte d* SwveManctt

CO CD XRAL

Work Order: 016398

XRAL LaboratoriesA Division of SGS Canada Ino.

Date: 26/08/97 FINAL Ptge 2 of 9

Element. Method, Det.Lira. Udts.

CM IT)

LO

CO *3-

x:•o: u.

COco

SB1 19442 SB1 19443 SB1 19444 WLI 19378 WLU9379

WLI 19380 WL1I9381 WLI 1 9382 WLI 19383 WLI 19384

WLI 19385 WLI 19386 WLI 19387

I 19388 l 19389

VJL^gl 19390 VJL8V119391 SB WLI 19392

WL119393 SB119451

SB!19452 5B119453 SB 119454 SB119455 SB119456 -

SB119457 SB119458 SB119459 SB119460 SB119461

SiOl AI2O3 CaO MeO Na2O K2O Ffc2O3 MnO TIO2 P2O5 Cr2O3 LOI Sum XRFI02 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRF102 XRFI02 XRF102

0.01*50.448.049.549.945.641.649.6N.A.49.645.650.1 \

\c -51 455.150.755.851.051.247.852.7

52.556.556.353.7— -69.0

49.071.372.768.644.9

0.0196

5.222.9514.013.38.5514,215.5

N.A.16.67.97128)1 14^'10.915.113.513.215.715.38.7914.4

16.711.1 .15.514.015.615.514.314.415.211.8

0.01%

16.52.3710.38.077.707.8212.4

N.A.3.677.24

i ioS\l 9.82J

8.159.789.467.6110.910.98.619.81

7;06, 9.85

9.258.151.466.993.182.931.8610.7

0.01t

12.729.78.269.5419.815.26.28N.A.7.5421.36.975.2611.4S.80\{ 4AV

4.395.776.5018.26.73

6.757.343.263.561.094.211.070.711.135.53

0.01*

0.680.052.153.390.631.331.24

N.A.4.850.31

/YlB\V4i4V

3.023.212.502.852.171.720.942.44

3.902.482.685.777.914.363.572.813.331.78

0.01tt

0.32•SO.Ol

1.000.380.110.610.52

N.A.0.050.0103j\

' o!28/0.340.370.360.330.941.490.130.49

0.451.08 .1.390.230.130.452.203.455.180.50

0.01%

10.68.1412.112.612.2

14.511.9

N.A.13.111.5I52\

k ii:o/11.48.3015.612.210.69.5112.010.4

9.79.9.788.7812.73.20

16.33.412.34-2.9922.2

0.01Ik

0.260.120.250.160.200.200.31

N.A.0.260.18025^

( Oi26 J0.180.150.340.250.210.240.210.27

0.34. 0.18

0.150.180.050.370.050.030.020.52

0.01•k0.250.150.670.760.470.910.74N.A.0.880.541.20)0,700.640.821.531.530.760.760.340.790.740.500.930.650.401.650.310.240.261.43

0.01*

0.110.010.030.040.030.080.05N.A.0.050.040.090.050.040.050.100.100.050.050.020.04

0.040.050.170.050.140.100.070.060.070.09

0.01•k0.180.250.050.060.370.100.05

N.A.0.060.32003oioP0.200.060.020.030.050.050.210.05

0.050140.050.040.010.010.020.020.020.02

0.011

1.258.551.401.603.953.351.45

N.A.3.404.40

, 0.55^)1.55V1.350.401.000.701.251.402.900.901.801.201.451.151.251.250.700.550.650.85

0.01tt

98.6100.399.799.899.799.9

100.0N.A.100.099.4

100.1100.199.199.299.899.099.599.1

100.199.0

100. 1100.299.9

100.2100.2100.2100.1100.299.3

100.3

CO CVJ

Mwntar of rix SOS Group (SocUM Q*n4nb d* SmwMimt)

CO

XRAL

Work Order: 016398

XRAL LaboratoriesA Division of SQS Canada Ino.

Date: 26/08/97 FINAL 3 of 9

CVJ LO

LO •ST

CO

rx:

enCO

Element. Method. Det.Llm.Units.

SB1 19462SB1 19463SBI 19464SB1 19465SBI 19466SBI 19467SBI 19468SBI 19469SB 1 19470

SBI 19472SBI 19473SBI 19474SBI 19475

4/1 SBU9476A/1 SBI 19477

SBI 19394SBI 19395SBI 19396- —— ————SBI 19397SBI 19398SBI 19399*Dup WU 19412*DupWLI 19424*Dup SBI 19436

*DupWL119381*DupWLl 19393*Dnp SBI 19462*Dup SB 119474

SIO2 A12O3 CaO MgO N*2O K2O Pe2O3 MnO HOI P2O5 Cr2O3 LOI Sum XRF102 XRF102 XRF102 XRFfOl XRF102 XRF102 XRF102 XRP102 XRF102 XRF102 XRE102 XRF102 XRFI02

0.01 0.01 6.01 0.01 6.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01t53.256.554.346.361.051.349.353.862.0

66.151.257.050.265.964.856.655.0———— 60.051.251.451.648.8N.A.72.6

49.747.853.357.0

ft

15.714.814.99.9114.817.014.812.814.6 n 1i j.*

16.415.014.412.915.614.613.315.214.614.114.315.911.9

N.A.14.615.78.8115.714.4

ft8.807.7711.010.18.6110.814.18.475.724 01wTn 3.4910.35.328.886.444.227.5610.45.4812.07.1613.46.94N.A.2.6212.38.638.815.32

ft5.615.635.3916.34.303.985.534.532.57 3.071.437.603.494.771.352.494.683.84A TO•f* J*

6.815:284.8612.3

N.A.0.556.2618.35.623.50

ft0.864.393.350.843.143.450.972.372.97 4.105.202.696.233.185.104.893.293.223 At .012.713.080.872.69

N.A.3.291.260.920.886.24

ft

0.440.140.200.120.460.710.460.321.12 3nn.UVI

2.570.520.190.430.511.300.920,512.331.030.410.140.25N.A.3.660.510.120.450.18

ft

12.79.289.4012.46.4511.112.815.88.72 5.76

3.6110.710.416.23.095.7611.39.777 "IH .1010.215.911.613.7

N.A.2.0312.012.012.710.3

ft

0.190.200.220.180.150.210.250.320.18 n rutu.uo

0.040.190.180.320.040.100.260.310.130.220.250.240.17N.A.0.01

0.310.210.190.18

ft0.640.790.860.570.570.760.691.481.61A ttlU./U

0.410.631.261.470.39

0.611.561.540.790.791.770.750.70N.A.0.240.730.340.641.26

ft0.050.060.060.050.060.040.040.100.11 0.420.120.050.100.100.150.120.100.100.360.060:il0.050.05N.A.0.070.050.020.050.10

ft0.100.050.050.300.060.050.020.020.03 0.020.030.050.020.020.020.030.020.020.020.050.020.050.14N.A.0.020.050.210.100.02

ft

2.000.800.452.400.500.801.050.100.75 0.750.700.651.701.701.601.150.550.5004flV**fU

0.950.500.402.20N.A.0.451.452.801.951.65

ft100.3100.4100.299.5

100.1100.2100.1100.1100.3 99 277 *A

100.199.6

100.3100.2100.2100.1100.2100.3W Q.0

100.2100.199.899.8NA.100.1100.3100.1100.4100.2

Mtmbar of UM SOS Group (SocMtf G4n*nta rf* Bwrtlsne*(

CO

XRAL

Work Order: 016398

XRAL LaboratoriesA Division of SQS Canada Inc.

Date: 26/08/97 FINAL Ftp 4 of 9

CAJLO

LO•^rCO

Element. Method. Det.Lim. Unlta.

Lu

03 CO

CXI

03 CO

WL1 19413 WL1 19414 WL11941S WL1 19416

WL1 19417 WL1 19418 WL1 19419 WU 19420 WL1 19421

WU 19422 WL1 19423 WL1 19424 SBl 19425 SB1 19426

SB1 19427 SB1 19428 SB1 19429 SBl 19430 SB l l 943 l

SB119432 SBl 19433 SBl 19434 SBl 19435 SBl 19436

SBl 19437 SBl 19438 SB l 19439 SBl 19440 SB l 19441

ST XRT7

2ppm11039

N.A.3666369

N.A.N.A.

56N.A.

78N.A.N.A.

158134266510346702343

53 N.A. N.A.

487135104262

N.A.N.A.

89

YXRF7

2ppm

129

N.A.•C21416

K.A.h. A.

15N.A.

10N.A.N.A.

23321427

314

5N.A. N.A.

131031•C2

N.A.N.A.

18

Zr XRF7

3ppm

4928

N.A.584344

N.A.N.A.

38N.A.

45N.A.N.A.

809254

11382

215111114

N.A. N.A.

167141

99102

N.A.N.A.

53

Nb XRF7

2ppm

22

N.A.443

N.A.N.A.

4N.A.

3N.A.N.A.

33

23375

N.A. N.A.

5654

N.A.N.A.

2

Ba XRF7

20ppm

84<20

N.A.133165233

N.A.N.A.

391N.A.

57N.A.N.A.

113326264514365275472

88N.A. N.A.

590794228620

N.A.N.A.

377

Cr ICF80

1ppm

N.A.N.A.

rJMtpN.A.N.A.N.A,dzh

dBfflP-N.A.

363N.A./-IW^

C 1660rt *^v*N.A.N.A.N.A.N.A.N.A.N.A.N.A.

/1240(( 579

N.A.N.A.N.A.N.A.

256435

N.A.

Nl ICP80

1ppm

N.A.M, A.

Ofifel^N.A.N.A.NAcdsi?' 35?^NTt

110NJL.\ /"'14o*

)(6KUNTA.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

^.Ar^N.A.N.A.N.A.

30320

N.A.

CMICF80

0.5ppm67.727.437.431.544.855.276.238.137.1151

28.6\ 46.1J 8.4

25.587.977.593.553.067.515.4203

v 513 } 70.0' 31.1

15.354.34.7

29.488.091.7

Zn ICP80

0.5ppm

86.269.590.56.8

65.475.5

166145

68.7146

86.183.367.0115140

71.6155

74.574.554.8

75.3 65.2 57.955.735.8254

34.140.8127

70.1

Aa ICF80

3ppmO.^Oo0oo•C3<3•C3

0^O<30O<3OOC3o o•C3<3

oO<3O<3

Mo ICP80

1ppm^<l

261

^3

•CI<l

1< l

3331

41<I1467

1049828953

icrsl0.2

ppm03

<0 20.40.90.3

^2030.80.4

C0.20.3

<0.20.3

<0.20.20.40.70.50.40.41.2 0.7 0.51.00.30.50.70.60.8

•C0.2

Sb 1CF80

5ppm

61410^<5*; 5<5136

<54^3<5

9<5<5

^^5<S<5<5

8C5<5<5<3<5<5<5

i Mwibwofth*SQSGro*p{Soet*t4G*n4r*J.d.Survem*nc*)

CO

CDCD XRAL

Work Order: 016398

KRAL LaboratoriesA Division of SG8 Canada Ino.

Date: 26/08/97 FINAL Pai* 5 of 9

Element. Method. Del.Ltm. Unite.

CO

.SB l J 9442 SBI19443 SBI19444 WLl 19378 WLl 19379

WLl 19380 WLl 19381 WLl 19382 WL119383 WLl 19384

WLl 19385 WLl 19386 WLl 19387 WLl 19388 WU 19389

Vi U9Q119390 WL.S8119391 SBWL119392

WLl 19393 SB119451

58119452 SB 119453 SB119454 SB 119455 SB119456

SB119457 SB119458 SB119459 SBI19460 SB119461

CO

CO CM

SrXRF?

2ppm247

2110718828

82147

N.A.4711

91371424111128

8516615569

132

113245407277213

2032G8

9213088

YXRF?

2ppm

815149

2121

N.A.129

2714101528281818121415111913H

202

^231

ZrXRF?

3ppm

5711455932

6434

N.A.5237

8356585196

8449493252

4367

10848

231

999997

10691

NkXRF?

2ppm

32332

32

N.A.53

32234

33242

2353

11

35442

B*XRF?

20ppm

129

25097

•C20

123153

N.A.23

^0

9088

152152104

275138504102182

205225640

89128

154521474585169

Crrcroippm

N.A.N.A.N.A.N.A.N.A.N.A.N.A.

114N.A.N.A.N.A.N.A.N.A.N.A.N.A.N,A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

mICP80

1ppm

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.

20N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

CM1CP80

•.5ppm5.4

16.579.756.019.18.6

82.739412.854.6190174241

55.039.526.073.0

13112.094.437.747.655.9

13915.056.86.8

10.330.461.4

ZaICP80

0.5ppm98.253.173.761.8132270

90.470.158.263.6

96.054.964.3101174

18183.568.174.980.4

82.083J74.241.926.0

10844.380.866.2270

AsICF80

3ppmOOC3O•O

0<3OOO

o<3•C3<3O

0Oooooo•ooo3

<3OO

MoICF80

1ppm

48•O^<^<l•CI

123•CI

1*;l

1^l

32

235

^1

24325

*;l866

<l

AtICP80

0.2ppm0.3

•c 0.20.60.2

•C 0.24^02•C0.2

1.50.30.2

•C0.2•C 0.2

0.5C 0.2C 0.2*C02•C0.2

0.5<0.2

0.5

^0.2^0.2C 0.2

0.90.5

•C0.20.30.20.3

SbICP80

5ppm

•C56

^<5

13

<5<5^5<5

9

<5<5

5•C5<5

<5<5OC5<5

<5<5•C5<5<5

<5C5^<5<5

Mwnbw of tlM SOS Oravp (SocMM Q*ntt*t dt Sunwfftono^

CO

o

al XRAL

Work Order: 016398

XRAL LaboratoriesA DMafon of SOS Canada Inc.

Date: 26/08/97 FINAL Page 6 of 9

Element. Method. Det.Lim. Units.

S S

OJ LO

LO •"S"

CO

tolil

l

TCO CM

SB119462 SBI19463 SBI19464 SBI19465 SB119466

SBI 19467 SBI19468 SBI19469 SBI19470 SBI19471

SBI19472 SB 119473 SBI19474 SBI 19475 SBI19476

SBI 19477 SBI19394 SBI19395 SBI19396 SBI19397

SBI19398 SBI19399*DupWLi 19412*Dup WL119424*Dup SBI 19436

*Dup WL119381*Dap WL119393*Dup SBI 19462*Dup SBI 19474

Sr XRF7

2ppm

8516327480

39312413011666

1370

49310519814223939778

103960160136106113

N.A.1361497084

196

Y XRF7

2ppm

121215101017142732

84-2

122228

61032281515

311614

N.A.1123111423

Zr XRF7

3ppm

465467447448449082

19710641

11187

1511258886

17154

1084751

N.A.143353344

111

Nb XRF7

2ppm

22223

333552364652562223

N.A.73435

Ba XRF?

241ppm106527422

306503125131246

1190629206193141213534284221

1080381257

2882

N.A.791

155104105196

Or ICP80

1ppm

N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

NA.N.A.N.A.1660N.A.N.A.N.A.N.A.N.A.

Nl ICP80

1ppm

N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

N.A.N.A.N.A.

654N.A.N.A.N.A.N.A.N.A.

Co ICP80

0.5ppm141

41.864.15.9

59.079.4120

49.247.410.415.630.961.5282107

27.923.827.930.162.575.8

10374.3

8.717.887.012.1139

62.6

ZB ICP80

0.5ppm

91.685.2102114

84.789.274.5

11584.583.564.481.354.1269

23.288.5133143

95.188.3148

92.293.371.537.393.478.789.454.2

An ICP80

3ppmOOOOooooooo<3O<30o^ooooooo0o0

Mo ICF80

1ppm

414o512253

10•O11532331

•CI5

4\39

*C1^

42

icm0.2

ppm0.50.5

<0.20.30.2

030.50.60.61.0

0.7^Q 2o!?

0.40.6

0.3<0.2

0.40.4

•C 0.2

^(U0.30.30.9

•C0.2•C0.2

0.40.9

Sb JCP80

5ppm

O<5^.5

8O4^5<5<5<5^4*5<5<5<5*S3

O<5O<5O^<5<5

8O^

5^<5

BicraW*156'5

341

71'

l\2l30151^32:

1361

66121'10'41124(56^34^27(

133(381iif2t8(72

897

32029

400114

M*mbar of Di* SOS Qroup (SocMt* Gtatah rf* Survoftlanct)

XRALWork Order: 016398

XRAL LaboratoriesA Olvfslon of SOS Canada Inc.

Date: 26/08/97 FINAL 7 of 9

OJinUT)*3-•^rCO

S

enCOCM

i

Method.Det.Lim.Units.*SS WU 19412

WL119413 WL119414 WL119415 WL119416WL119417 WL119418 WU 19419 WLM9420 WL119421WL119422 WL119423 WU 19424 SBll9425 SB! 19426SB119427 SB119428 SB119429 SB119430 SBl19431SB119432 SBll9433 SBl19434 SB11943S SBl19436SB119437 SB119438 SB119439 SB119440 SB119441

WICP80

10ppm<10<10•CIO•00<lO<JOC 10"CIO•CIO<10

<10<IO•cio<10<10<10<10•c: 10<10<10<10<10•C 10<10<10<10<10•CIO•CIO*clO

PbICP80

2ppm<2<2<2•C2<2<2

7<2•C2<2<2<2<2•C2<2<2<2

7•C2<2

34

<2^<2<2<212•C2

<2

TeAAH3

0.1ppm0.10.2

^.10.1

•CO.l0.10.20.30.10.10.10.10.20.20.20.20.30.20.10.10.30.30.2

•C0.1*;o.i0.1

<0.10.10.40.1

S C02CHM112CHM114

0.01K

0.040.02N.A.0.030.030.02N.A.N.A.0.01N.A.0.01N.A.N.A.0.100.330.140.770.520.040.131.05

N.A.N.A.0.080.030.190.02N.A.N.A.0.06

0.01ft0.010.01

N.A.0.020.02

0.07N.A.N.A.0.07

N.A.0.01N.A.N.A.0.010.370.040.020.020.010.030.01

N.A.N.A.0.010.010.010.01

N.A.N.A.0.25

MwnbM of tb* SOS Group (SocMtf gfcrfraft d* Surveflfamtt)

CO

CM XRALWork Order: 016398

XRAL LaboratoriesA Division of 80S Canada Inc.

Date: 26/08/97 FINAL Pap S of 9

Element. Method. Del.Lim. UniU.

cvjLO

LO

CO

^r

SB1 19442 SB l 19443 SB1 19444 WL1 19378 WL1 19379

WL1 19380 WL1 19381 WU 19382 WL1 19383 WL1 19384

WL119385 WL1 19386 WL1 19387 WLI 19388

CM

enCO OJ

\vLSRll9390 WU Sftil 939 1GR WLI 19392

WLI 19393 SB1 19451

SB1 19452 SB1 19453 SBI 19454 5B119455 SB119456

SBI 19457 SBI 19458 SBI 19459 SBI 19460 SBI 19461

W ICP89

10 ppm

<10 <10

<10 •CIO

•CIO

•CIO•CIO•CIO

oo

0000

PbICP80

2 ppm

3•C2 <2 <2

<2 •C2 <2 <2

<2<2

3

•C2 <2 <2

<2

O•C2•C2 <2<2

Tc 5 CO2 AAH3 CHM112 CRM 114

O.I 0.01 0.01 ppm % %

<0.1 0.3 0.1 0.1

•CO.l

0.1 Oil

0.1

<0.1<0.1

0.1

<0.1 0.1 0.1

•C2 <0.1

<2 O.l^ <0.1<2 <0.1

<0.1

0.1

•CO.l^0.1

0.1

0.020.300.050.020.01

0.05 N.A. 0.04 0.04

0.080.050.330.020.08

0.020.060.020.010.02

0.010.100.080.130.04

0.500.040.030.020.26

0.712.260.230.080.08

0.01 0.16 N.A. 0.24 0.03

0.010.040.010.020.01

0.010.010.190.020.02

0.030.460.040.08

-C 0.01

0.01

o!oi•C0.01

0.01

Mwnter of th. S6S Group (SotMM Otnirato dt SurvcMmc*)

AUG-

26-9

7 TU

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LABORATORIES

FAX

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6445

4152

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COo XRALWork Order: 016503

XRAL LaboratoriesA Division of SOS Canada hie.

Date: 03/09/97 FINAL l of 9

CD

Method.Det.Llm.Units.

SB l 19445 SB l 19446 SB1 19447 SB l 19448 SB! 19449

SB l 19450SB85201SB85202SB85203SB85204

SB85205 SB8S206 SB85207 SB85208

CO

en en

VILJB85210VILJB85211VLH852I2

SB852I3SB1I9400SB1 19478 SB1 19479 SB1 19480 SB1 19481 SB1 19482SB1 19483 SB1 19484 SB1 19485 SB1 19486 SB1 19487

S02 AB03 CaO MM) Na2O K2O Fe2O3 MnO TK)2 P2OS Q3O3 LOI Sum UPIOO XRF100 XRF100 XRJFTW XRF100 XRF100 XRF1W XRF1W XRP100 XRF1W XRF100 XRF100 XRFIOO0.01

*69.357.5N.A.NA.52.467.050.052.249.645.3

NA.71.178.068.1NA.55.954.562.5NA.52.8

NA.71.159.149.756.7

NA.63.857.064.148.5

•.01%

15.113.9

NA.NA.13.3

13.915.014.69.458.85

NA.14.711.514.6

NA.13.315.915.6

NA.15.0

NA.15.013.314.615.6

N.A.14.514.115.212.6

0.01*

5.058.13NA.NA.8.204.5412.410.311.88.01NA.3.172.511.75

NA.7.3510.46.12NA.9.68

NA.2,596.2614.49.16

NA.6.608.585.8210.1

0.01•k

1.476.27NA.NA.4.491.976.925.4211.620.3

NA.0.960.512.09NA.6.885.05231NA.6.18

NA.0.765.387.354.70NA2.693.992.634.95

0.01*

1.582.62N.A.N.A.1.832.841.632.002.050.46NA.2.513.074.58

N.A.3.723.483.03NA.2.92NA.4.543.051.983.64

NA.3.683.485.151.71

0.01ft

2.800.54NA.NA.0.532.190.330.410.120.12NA.2.591.843.31NA.0.640.150.93NA.0.47NA.1.78.3.030.270.35NA.0.800.581.520.34

•.01ft

2.968.17NA.N.A.16.64.9911.012.712.311.3

NA.2.751.293.48

N.A.9.748.087.48NA.10.4

NA.2.907.4710.27.65NA.6.039.313.9419.1

•.01Ik

0.030.17NA.NA.0.310.090.250.340.270.21NA.0.050.020.04NA.0.130.220.12NA.0.18

NA.0.060.120.260.23NA.0.120.200.080.55

•.0(1ft

0.3370.676NA.NA.1.6500.5580.7190.6820.4510.492NA.0.2860.1720396NA.0.7440.6380.578NA.0.666

N.A.0.2950.6860.6760.715NA.

0.6151.2410.4721.457

041ft

0.070.05

N.A.N.A.0.110.150.040.040.020.02

NA.0.060.070.18NA.0.090.040.12NA.0.05NA.0.050.350.050.05NA.0.060.100.190.10

0.01ft

0.030.12NA.NA.0.030.050.050.050.450.24NA.0.030.020.03NA.0.050.110.02NA.0.06NA.0.02.0.030.050.05N.A.0.050.030.040.02

•Jlft

1.350.95NA.NA.0.501.250.800.401.304.30N.A.1.651.151.30

NA.0.700.550.85NA.0.60N.A.0.800.450.650.40N.A.0.650.950.600.70

0.91ft

100.099.1NA.NA.99.999.699.199.199.599.6NA.99.9

100.299.8NA.99.399.199.6NA.99.0N.A.99.999.3

100.299.2NA.99.699.699.8

100.1

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LO XRALWork Order: 016503

XRAL LaboratoriesA Division of SOS Canada Inc.

Date: 03/09/97 FINAL Fife 3 of

Element. Method. Det.LJm. Units.

OJ LO

LO"srCO"S4

8l

SB85018 SB85019 SB85020 SB8502I SB85022

SB85023 SB85024 SB85025 SB8S026 SB85027

5B85301 SB853Q2 SB85303 SB85304 SB85305

SB85306 SB85307*DupSBl 19445*DupSB85207*DupSBlI9482

*DupSBl 19494*DupSB85006*Diip SB85018*DupSB85303

8102XRFIOO

0.01%N.A.47.048.S50.152.4

48.4N.A.N.A.N.A.63.355.897.657.764.452.462.261.869.478.156.646.871.6

N.A.57.7

AI203XRFIOO

0.011

N.A.10.114.515.112.812.6

N.A.N.A.N.A.14.9

11.50.5513.813.73.6111.013.715.111.615.514.415.2

N.A.13.9

CaOXRFIOO

0.01%

N.A.13.612.55.588.7810.2

N.A.N.A.N.A.4.4310.20.4610.36.4614.76.975.715.062.539.1320.12.34N.A.10.3

MfOXRFIOO

6.01•kN.A.11.17.378.894.954.95

N.A.N.A.N.A.3.035.190.161.942.0418.34.063.511.460.504.685660,73N.A.1.96

N*20XRFIOO

0.01ft

N.A.1.462.492.241.761.41

N.A.N.A.N.A.6.771.110.102.713.360.721.732.921.563.083.670.945.28

N.A.2.70

K2OXRF1M

0.01ft

N.A.0.270.322.040.690.43

N.A.N.A.N.A.0.610.19

-CO.Ol0.891.950.181.561.252.801.820.340.14-

. .2.09N.A.0.88

Fe2O3XRFIOO

0.01•kN.A.13.411.711.615.819.3

N.A.N.A.N.A.4.9112.91.0010.26.407.4610.17.642.961.307.628:81

. 1.95N.A.10.2

MnOXRFIOO

0.01ft

N.A.0.280.280.280.310.54

N.A.N.A.N.A.0.070.33

0.010.280.150.140.210.120.030.020.220.260.02

N.A.0.29

TKMXRFIOO

0.001t

N.A.0.5800.6860.7351.4651.435N.A.N.A.N.A.0.5170.5540.0691.5110.5520.2541.0540.6380.3350.1680.7100.4610.245N.A.1.521

P2O5XRFIOO

0.01ft

N.A.0.030.040.040.100.10

N.A.N.A.N.A.0.140.030.010.100.110.04

0.100.060.070.070.050.16

. 0.05N.A.0.11

Crt03XRFIOO

0.01ft

N.A.0.260.050.050.020.02

N.A.N.A.N.A.0.020.050.050.030.050.400,040.120.030.020.050.260.02N.A.0.05

LO!XRFIOO

0.01ft

N.A.0.700.703.500.650.40

N.A.N.A.N.A.0.851.100.200.400.501.050.952.301.301.050.501.15n.m

N.A.0.40

SumXRFIOO

0.01ft

N.A.98.799.2

100.299.799.7

N.A.N.A.N.A.99.598.9

100.399.999.699.399.999.7

100.1100.299.199.299.9N.A.100.1

FXRf

PPN./

71

N./IN.AN./i

1124

42841

I5!

N.A2.

CO

en

•BOB Mmtar of th* SOS Gmp (SocMtt QtMrata dt Surarittane^

CO CD XRAL

Work Order: 016503

XRAL LaboratoriesA Division of SQS Canada Inc.

Date: 03/09/97 FINAL rite 4 of 9

ffi

COw—l•*3-

Element. Method. Det.I/lm. Units.

SBI 19445 SB1 19446 SBI 19447 SBI 19448 SBI 19449

SBI 19450SB85201SB85202SB8S203SB85204

SB85205 SB85206 SB85207SB85208

V L 3985209

S385210

rx:

as o-cvj

CO CD

COd)UJ era

9B85212 SB852I3 SBI 19400

SBI 19478 SBI 19479 SBI 19480 SBI 19481 SBI 19482

SBI 19483 SB 1 19484 SBI 19485 SBI 19486 SB l 19487

SrXRF?

2ppm413263

N.A.N.A.

81

938112828940

N.A.217257575

N.A.13867

362N.A.

91

NJL287

1010150145

N.A.280431776139

YXRF7

2ppm^12

N.A.N.A.

26

4141588

N.A.2

^3

N.A.

141010

N.A.12

N.A.2

141414

N.A.10212

27

ZrXRF?

3ppm

9667

N.A.N.A.

103

13147453333

N.A.10083

119N.A.

8936

122N.A.

40NJL

941664645

N.A.80

10312895

MbXRF7

2ppm

32

N.A.N.A.

34332

^

N.A.336

N.A.

334

N.A.4

N.A.4..522

N.A.2443

BaXRF?

20PPI*

418261

N.A.N.A.

217

66113012742

00N.A.

782290699

N.A.245

41205

N.A.482

N.A,. 4581050

8458

N.A.264149

1020125

CrICP80

1ppm

N.A.N.A.1620621

N.A.

N.A.N.A.N.A.N.A.N.A.

178N.A.N.A.N.A.

640N.A.N.A.N.A.

97N.A.

240RA.N.A.N.A.N.A.

238N.A.N.A.N.A.N.A.

NlICF80

1ppm

N.A.N.A.

60866

N.A,

N.A.NA.N.A.N.A.N.A.

26N.A.N.A.N.A.

ISON.A.N.A.N.A.

19N.A.

263.N.A.N.A.N.A.N.A.

17N.A.N.A.N.A.RA.

CuICP80

0.5ppm50.954.4*:o.556.150.0

23.052.819.317.4

•*0.526.24.46.6

^.529.23.3

76.822.850.159.90.7

•COJ21.39.89.68.4

37.517.114.663.3

ZnICP80

0.5ppm56.971.246.549.692.355.162.468.966.854.411.624.731.847.9128

35.342.192.4355

65.9

•32.031.872.251.353.431.170.390.544.5182

AsICP80

3ppm

11*3O18OO

63

OOO

5OOOooo

6Oo100

6O

4OOOO

MoICP80

1ppm

9756

17104433

129877436

105

76554

146

1055

A*ICP80

0.2ppm^.2-C0.2•C0.2*:0.2•c: 0.2

0.20.2.

O.2-C0.2*:0.2

0.4f 0.2•C 0.2*C0.2•c: 0.2

o:0.2*:o.2•C0.2•C0.2*C0.2

*;o.24:0.2•C0.2•C0.2•C0.2•i 0.2*:0.2^.2*C0.2*C0.2

SbICP80

5ppm<5<5<5<5<5<5^<5<5<5<50OOOO^0^<5

<5O^^^<5^<5<5<5

Muntar rf Hw MS Group {Soda* QMnM d* Surv*lftMO*t

r— o XRAL

Work Order: 016503

XRAL LaboratoriesA Dtvfeton of SGS Canada Inc.

Date: 03/09/97 FINAL Ftp S of 9

CM LO

LO "ST

CD

Etono*. Method. Det.Llm. Unit*.

SB 119488 SB119489 SB119490

VJL 39119491

V/L,

O-

coCO CD

CO CO

UJto

M1949311194941119495

5B119496 SB119497

SB119498 SB 119499 SB119500 SB85001 SB850Q2SB85003 SB85004 SB85005 SB85006 SB85007SB85008 SB85009 SB85010 SB85011 SB85012SB85013 SB85014 SB85015 SB85016 SB85017

Sr XRF?

2ppm

67450234

73111734233

1270138120

123N.A.

113115179385598158318417

332N.A.N.A.

5652

36216526024

115

Y XRF7

2ppm

-—<2

9101576

11132927

N.A.25163144

28^23

N.A.N.A.

2511212677

16

Zr XRF?

3ppra

39107883648

15943

1954591

91NJL

835396

108122969196

100N.A.

"N.A.7438

10798923448

Nb XRF?

2ppm

^

33

<2372923

4N.A.

432443332

N.A,. .,N.A,

3333322

Ba XRF?

39ppm

mm

398524113186857

72992

42189169

N.A.96

111135375393264487199210

N.A..N.A.

11061

319109397<20

35

OrICP80

1ppm

N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

110N.A.N.A.N.A.

N.A.N.A.N.A.N.A.N.A.N.A.

10099

N.A.N.A.

N.A.N.A.N.A.N.A.N.A.

Nl ICP80

1ppm

N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.N.A.

34N.A.N.A.N.A.RA.NJLN.A.N.A.N.A.N.A.

It26

N.A.N.A.N.A.N.A.N.A.N.A.N.A.

Co ICF80

0.5ppm19.34.2

15.9<0.521. 112.15.32.8

62.230.3

33.7121

21.565.943.110.615.418.10.833

19.340.1127

23.740.622.46.9

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0.5ppm116

48.754.758.568.6

97.334.579.853.3125115

73.4102

97.692.9

51.653.8156

33.640.2

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3ppm

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Date 03/09/97 FINAL 6 of 9

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533

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57N.A.N.A.N.A.N.A.N.A.

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SEP-03-97

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LABORATORIES

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6445

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P. 11/11

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Appendix V

Spruce Bay Property

Lithogeochemical Plots

List of Plots

Figure 5: Total Alkalies (Na2O 4- K2O) Versus SiO2 (after Irvine and Baragar 1971) Diagram of Volcanic Rock Samples from the Spruce Bay Property. Symbols: filled squares - ultramafic to mafic volcanics; filled diamonds - mafic volcanics; filled circles - intermediate volcanics, crosses - felsic volcanics.

Figure 6: Total Alkalies (NajO + K2O) Versus SiO2 (after Irvine and Baragar 1971) Diagram of Mafic and Ultramafic Intrusive Rock Samples from the Spruce Bay Property. Symbols: half-filled boxes-peridotite, open boxes-hornblendite/pyroxenite; open diamonds-gabbro; X-unsubdivided mafic intrusions; and pluses-mafic to intermediate intrusions/lamprophyre.

Figure 7: Total Alkalies (TS^O + K2O) Versus SiO2 (after Irvine and Baragar 1971) Diagram of Late Archaean Granitoid (half-filled circles) and Intermediate to Felsic Hypabyssal (filled triangles) Rock Samples from the Spruce Bay Property.

Figure 8: Q-P Discriminant (Debon and Le Fort 1983) Diagram of Late Archaean Granitoid (half-filled circles) and Intermediate to Felsic Hypabyssal (filled triangles) Rock Samples from the Spruce Bay Property. Granitoid fields: l, granite; 2, adamellite, 3, granodiorite; 4, tonalite (trondhjemite); 5, quartz syenite; 6, quartz monzonite; 7, quartz monzodiorite; 8, quartz diorite; 9, syenite; 10, monzonite; 11, monzogabbro; and 12, gabbro.

Figure 9: Jensen (1976) Cation Diagram of Ultramafic to Mafic Metavolcanic Rock Samples from the Spruce Bay Property. Abbreviations: TR, tholeiitic rhyolite; TD, tholeiitic dacite; TA, tholeiitic andesite, CR, calc-alkaline rhyolite, CD, calc- alkaline dacite; C A, calc-alkaline andesite; CB, calc-alkaline basalt; HFT, high-iron tholeiite, HMT, high-magnesian basalt; BK, basaltic komatiite; and PK, peridotite komatiite.

Figure 10: Jensen (1976) Cation Diagram of Mafic Metavolcanic Rock Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 11: Jensen (1976) Cation Diagram of Intermediate Metavolcanic Rock Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 12: Jensen (1976) Cation Diagram of Felsic Metavolcanic Rock Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 13: Jensen (1976) Cation Diagram of All Metavolcanic Rock Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 14: AFM (Irvine and Baragar 1971) Diagram of all Metavolcanic Rock Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 15: Jensen (1976) Cation Diagram of Peridotite, Hornblendite/pyroxenite, Gabbro, Unsubdivided Mafic intrusion, and Mafic to Intermediate Intrusion/Lamprophyre Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 16: AFM (Irvine and Baragar 1971) Diagram of Peridotite, Hornblendite, Pyroxenite, Gabbro, Unsubdivided Mafic Intrusion, and Mafic to Intermediate Intrusion and/or Lamprophyre Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 17: Jensen (1976) Cation Diagram of Diabase Dike Samples from the Spruce Bay Property. Abbreviations same as Figure 9.

Figure 18: Mn-Ti-P Ternary Diagram (after Mullen 1983) of Mafic Metavolcanic Rocks from the Spruce Bay Property. Abbreviations: CAB, calc-alkaline basalt; IAT, island arc tholeiite; MORB, mid-ocean ridge basalt; OLA, ocean island alkalic basalt; and OIT, ocean island tholeiite.

Figure 19: Mn-Ti-P Ternary Diagram (after Mullen 1983) of Gabbro and other Unsubdivided Mafic Intrusive Rocks from the Spruce Bay Property. Abbreviations same as Figure 18.

Figure 20: Rb Versus Y + Nb Plot of the Granitic Rocks (half-filled circles-late Archaean felsic to mafic intrusions; and filled triangles-intermediate to felsic hypabyssal intrusions) from the Spruce Bay Property. Abbreviations: ORG, ocean ridge granites; syn-COLG, syn-collision granites; VAG, volcanic arc granites; and WPG, within plate granite.

Figure 21: Nb Versus Y Plot of the Granitic Rocks (half-filled circles-late Archaean felsic to mafic intrusions; and filled triangles-intermediate to felsic hypabyssal intrusions) from the Spruce Bay Property. Abbreviations same as Figure 20.

Appendix V

Figure 5: Irvine and Baragar P

lot

Spruce B

ay Meta volcanic R

ocks

LO

CO

m

.2*

rv.G

O

leen(D!6 CDBG

C.yo -5D

Q8i.CO

inCO

CM

O

C

O

l

CM

GO

CD

O

GO

OcOl * OSeN

CO

CM

Appendix V

Figure 6: Irvine and Baragar P

lot

Mafic and U

ltramafic Intrusive R

ocks

CD

rsiC

D*

Appendix V

Figure 7: Irvine and B

aragar Plot

Granitoids and Felsic/lnterm

ediate Dykes

T

LO

mP:GOle 2SoCDJl)C15 -8.S

isCD

CO

CM

CO

(D

S

To

LO

CO

CM

S

CO

LO

LO

CD

CD

CO

CM

.2"

CO

g"SLL- 0)

lO

O

I SCDO

D

CO

Appendix V

Figure 8: Debon and Le Fort Plot

Granitoids and Felsic/lnterm

ediate Dykes

sCM

LJ

C3

O

CM

g

CM* y] - e/is - o

Appendix V

Figure 9: Jensen Cation Plot

Spruce Bay Metavolcanic Rocks

CM

OO

O

)SDCOQ.

10

CO

O

l fe

™ *xo

^a

s S

oO)

Appendix V

Figure 10: AFM P

lot

Spruce B

ay Metavolcanic R

ocks

oGCsGO

(D^5.

CO

CMen

CDen

eaO)

'

Appendix V

Figure 11: Jensen Cation Plot

Ultram

afic to Mafic M

etavolcanic Rocks

CM

Qo "Sl.QTo0

}

CO

IU

C

D

LJ

CD

i

SO)

Appendix V

Figure 12: Jensen Cation Plot

Mafic M

etavolcanjc Rocks

CMo

vt

.O03o

c3

.25.

"SoC

O

LJ

CTJ

Appendix V

Figure 13: Jensen Cation Plot

Intermediate M

etavolcanic Rocks

CM

Q

O)

."2

CD

(D

LO

1^

en

.o•S3 CJ

Appendix V

Figure 14: Jensen Cation Plot

Felsic Metavolcanic Rocks

CM

.QoZ ltoIfra.S

'

CD

v*

T—-

l j

IS

CJ

J

Appendix V

Figure 15:

Jensen Cation P

lot

Mafic and U

ltramafic Intrusive R

ocks

CMo.oS59

0

aa "io

en LJ

en

Appendix V

Figure 16: AFM

Plot

Mafic and U

ltramafic Intrusive R

ocks

o(DVi

O)

.0To.yCO

to

CMento !6CO00O)

Appendix V

Figure 17: Jensen Cation P

lot

Diabase

CM

QoO*(D

V

if)

-sQB.

en

CD

li** O)

Appendix V

Figure 18: Ti-Mn-P Plot

Mafic M

etavolcanic Rocks

CM

Q.s•Q^

oOD in

CO

-*f

Q

to

Appendix V

Figure 19:

Ti-Mn-P

Plot

Mafic Intrusive R

ocks

CM

Q.Q

To•B

CM

2 S

ro

^

^

02^

S

Jsil

Appendix V

Figure 20: R

WY

+NbcN

b/Y P

lot

Granitoids and Felsic /Interm

ediate Dykes

(ujdd) q y

Appendix V

Figure 21: N

b:Y Plot

Granitoids and Felsic /Intermediate Dykes

J•gCDOD

to

i l

iCVJ

CD G

C O

CD

i!l

l l

l l

l l

l l l

l l

l l

ll l l

l l

l l

(tudd]

31 '97 11:31 FR MINING RECORDER TBflY 82" 475 1124 TO MINING

Ontariooc

lanrtlon of Assessment Work Performed on Mining Land

Ad. SutaMtkM eKaen*Mtn. U.O.1HO

tNum

Persons! information cod Mining Ael. the intormttk Questions aboul (his M 933 Ramsey Lake Road.

42C13SE2002 2.17973 WHITE LAKE (NORTH")

Instructions: - For -—.- r........— ..- Please type or print in

. Under section a ol in* i ifw tntnirtj tend noldw.

em no*.

900

i. Recorded holder(s) (Attach a list if necessary)2 .1797 3 OCT 3 1 1997

KECBKEDGoVe\ Corp*

Cient Number

Address Telephone Numbef

RECEIVED! gNlfflf (J

OCI 31 r997Number

GEOSCIENCE ASSESSMENomor2. Type of work performed: Check ( f ) and report on only ONE of the following groups for (his declaration.

Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

Physical: drilling, stripping, trenching and associated assays Q Rehabilitation

J

Office UseCommodityTotal S Value of Work Claimed

On ,os To| UMTI l TM! NTS Reference

Qlobal Petitioning Syttim Ot(* (A avaUbli) TewnsnipfAiMMining Division

M or O-Pttn Nuiribw Re*idem Geoiogni

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required:- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)

4. Certification by Recorded Holder or Agent

None)______ . do hereby certify that l have personal knowledge of the facts set

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

OC1 31 '97 iii31 FR MINING RECORDER TBflY 807 475 1124 TO MINING LrtMDS P.03/04

' S . Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous Rnk must accompany this form. \ \ O*1( f,A t AA Q/ *1

Mining CWm Number. Or if work was done on other eligible mMng land, show in In* column the location number indicated on the claim map.

•g TB7827

NumMr el Claim Unite. For other mining land. H* hectares.

16 ha

Vekwef workperfofiviefl on this claim or other mining land.

S2S. 826

Vetueolwafk applied lo this cWm.

Value of wefk assigned to other mining claims.

Bank. Vsloe of work to be distributed at a Mure data.

N/A

1234567 12 S24.000

eg1

1234568 98,892 S 4,000 S4.892

H3323I)-

TB

o* 3, 2.00 o

10

1112

13 msl mi14 EOSCI15

Column Totals

, do hereby certify that the above work credits are eligible underTmt fan Nairn)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to

the claim where the work was done.in Writing

6. Instructions for cutting back credits that ere not approved.

Some of the credits claimed in this declaration may be cut back. Please check ( K ) in the boxes below to show howyou wish to prioritize the deletion of credits:

v r p6 1 - Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.D Z . Credits are to be cut back starling with the claims listed last, working backwards; orD 3. Credits are lo be cut back equally over all claims listed in this declaration; or

D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: if you have not indicated how your credits are lo be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use OnlyRecened Sump ThwderBajr

Mtataa-Dmaon

OCT 3 l W? '

RECEIVED

OewnM Approved Dal*

Trat* Approved

DM* NotUicition Sent

Total Value of Credit Approved

Approved tor Recording By Mining Recorder (Signature)

©OntarioOCT 31 . 97 U:32 FR MINING RECORDER TBSY 907 .75 1 124 TO MIN.NG L^DS

0 Statement ol Costsfor AMeMroent Credlt

•ertontl Information cotoclm) on (hit term It obWxtd undtr th* tuthorHy ol MbMeHon B[l) of DM Ajsewnenl Wort RtgiftOon SIM. Undtr McUon 8 d Ih* Mining Ael, Di* Mbrmttton it t pgMc noon). Thlt Infoontfon wffl b* md to ravttw dw utmtMnt work md centipond wWi h* mining land holdtr. OueiUonj tbout IMt collection tbouW be directed w (h* CNtf MMng Recorder, MlnMiy ol Northern Development end Mn**, 6th now, 933 Ftamt*r LA* A"d- Sudbury. OnUrlo, PIE 985.

Work TypeUnits of Work

Depending en (he type el we*. Hit V)* numtar of fiovft/deyt wortud. meirn of drDtng. W*- metrtf ol grid lint, number ol itmptes. ttt.

Cost Per Unit Total Cost

T

-g^S Z

Associated Costs (e.g. supplies, mobilization and demobilization).

IK*-C*ttA VJ *X\ VfN6^

irtyt-Coixat dooo

7uvu W*

vrxwi^1Transportation

-REFood and Lodging Coats OCT 3 1 1997 3/5

3L3-0EfljT3E0S-QEElfcL

Total Value ol Assessment Work

Calculations of Filing Discounts:

1. Work filed within two years of performance Is claimed at lOOtt of the above Total Value of Assessment Work.2. H work Is filed after two years and up to five years after performance, it can only be claimed at 50"* of the Total

Value of Assessment Work. If this situation applies to your dalms, use the calculation below:TOTAL VALUE OF ASSESSMENT WORK _______x 0.50 - ______Total S value of worked claimed.

Not*:- WorK older than 5 years Is not eligible for credit.- A recorded holder may be required to verify expenditures claimed In Ihls statement of costa within 451 m request lor verification and/or correctton/clariricatton. If verification and/or correctton/dajiricaUon te not made, ^ Minister may reject all or part of the assessment work submitted. ____OCT 3 1 J997

Thunder!Certification varlfyina costs:

l, . A ) lar\Mi ram)

reasonably ba~determined and the costs were Incurred white conducting

the accompanying Declaration of Work form as J

RECEIVED

"V; . ___ , do hereby certify, thatO 1997

shown are as accurate as may

(rtcortfti) hddw.

on the lands Indicated on

l am authorized•Bi fgning mtnoriiir)

to make this certification.

PflQE.04 **

Ministry ofNorthern Developmentand Mines

Ministere du Developpement du Nord et des Mines

March 19, 1998

WINSLOW GOLD CORP.1290-112 4TH AVENUE, SOUTH WESTCALGARY, ALBERTAT2P-OH3

OntarioGeoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (888)415-9846 Fax: (705) 670-5881

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2 .17973

StatusW9740.00967 Approval After Notice

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Bruce Gates by e-mail at gatesb2@epo.gov.on.ca or by telephone at (705) 670-5856.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 12026

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.17973

Date Correspondence Sent: March 19,

Transaction First Claim Number NumberW9740.00967 1097947

1998

Township(s) 1 Area(s)WHITTLE LAKE

Assessor: Bruce Gates

StatusApproval After Notice

Approval Date

March 13, 1998Section:12 Geological GEOL 17 Assays ASSAY

The requested expense verification as outlined in the Notice dated January 27,1998, has been received. Accordingly, assessment work credit has been approved as outlined on the Declaration of Assessment Work Form accompanying this submission.

Costs associated with this project outside of the dates reported on the Report of Work form accounted for the higher costs being reported for this submission.

Correspondence to:Resident Geologist Thunder Bay, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):Allan MacTavish THUNDER BAY, ONTARIO

WINSLOW GOLD CORP. CALGARY, ALBERTA

Page: 1Correspondence ID: 12026