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52G15NW9300 2.15138 SIXMILE LAKE010
NORANDA EXPLORATION COMPANY, LIMITED (no personal liability)
SUMMARY REPORT
GEOLOGICAL/GEOCHEMICAL/GEOPHYSICAL SURVEYING
CUNNINGHAM OPTION PROPERTY
N.T.S. 52G/15
NORTHWEST ONTARIO DISTRICT
PROJECT NO. 1326 THUNDER BAY, ONTARIO FEBRUARY 1, 1993
NOISIAIQ O N5MI7J V ID f b J. V ci
AL SMITH PROJECT GEOLOGIST
REG FELIX o 33, ctf SR. PROJECT GEOLOGIST ' 7 7
. 00057
52G15NW93ee 2.15138 SIXMILE LAKE
Table ot contents
1.0 INTRODUCTION
2.0 LOCATION AND ACCESS
3.0 PROPERTY DESCRIPTION AND CLAIM DISPOSITION
4.0 PREVIOUS WORK
5.0 1992 EXPLORATION WORK
6.0 REGIONAL GEOLOGY6.1 Stratigraphy6.2 Age Relations6.3 Exploration Model
7.0 PROPERTY GEOLOGY7.1 Lithologies7.2 Structure7.3 CC Sulphide Zone7.4 East Sulphide Zone
8.0 LITHOGEOCHEMISTRY8.1 Reconnaissance8.2 CC Sulphide Zone
9.0 GEOPHYSICS
10.0 CONCLUSIONS AND RECOMMENDATIONS
REFERENCES
010C
Page
1
1
1
2
2
3333
33445
556
6
7
List of Attachments
Figure 1 Location MapFigure 2 Claim MapFigure 3 Regional Geology MapFigure 4a Property Geology MapFigure 4b Sample Locations and General Geology (back pocket)Figure 5 Total Field Magnetic Map {back pocket)Figure 6 Ternary Diagram-Surface LithosamplesFigure 7 Ternary Diagram-Drill Core Samples
List of Appendices
Appendix l Lithosample Descriptions and Lithologic Unit DescriptionsAppendix II Geotechnical Analyses and Assay ResultsAppendix III Geophysical Interpretation Report and Protem ProfilesAppendix IV List of Personnel
Scale
1:2,000,000(approx) 1:31,680
1:125,000(approx)1:100,000(approx)
1:5,0001:5,000
1.0 INTRODUCTION
Geological mapping and lithogeochemical sampling were completed over a portion of the Cunningham Option property in the Six Mile Lake area (North Sturgeon Lake Belt) between October 18- 20 and 28-29, 1992. The objective of this preliminary work was to document the nature and distribution of felsic pyroclastic units hosting the barren sulphide zone and to search for alteration indicative of VMS-style mineralization. A further objective was to delineate new target areas for base metal mineralization along the top of the Six Mile Lake felsic volcanic cycle, however an early snow covering hampered much of this work.
2.0 LOCATION AND ACCESS
The Cunningham Option property is located approximately 200 km northwest of Thunder Bay and 30 km south of Savant Lake in the Patricia Mining Division (Fig.1). The property is accessible via the Six Mile Lake Road which traverses the central part of the claim group. The Six Mile Road extends easterly from Highway 599, approximately 30 km south of Savant Lake, and is suitable for 4 wheel drive vehicles only. The eastern end of the property is also accessible by boat.
3.0 PROPERTY DESCRIPTION AND CLAIM DISPOSITION
The property consists of 38 unpatented mining claims, comprising approximately 608 hectares as shown in the northeast corner of the Six Mile Lake (G2651) claim map sheet (Fig. 2). The claims are listed below.
CLAIM NUMBERS
Pa 61 1504-506
Pa 642478-482
Pa 642974-986
Pa 642988-997
Pa 719586-587
Pa 719934-937
Pa 719941
NUMBER OF UNITS
3
5
13
10
2
4
1
DUE DATE
04/20/94
04/20/94
06/21/94
06/21/94
04/24/96
03/01/96
04/24/96
Most of the above claims were staked in 1982 and 1984 by L.S. Cunningham. Norex has an option to acquire a 6Q*fa interest in these claims. A property recently staked by Norex bounds the Cunningham property to the north.
4.0 PREVIOUS WORK
CUNNINGHAM OPTIONv^V&ZJBf*. ^ 3^w —,
CUNNINGHAM OPTION PROPERTY
LOCATION MAP
r T- i l t ""•' "~**-*t i **M4*i lot,tM i iunui i g'
1-31- -H- -j- - L . L. L J. J li
/y 9sso6 CUNNINGHAM OPTION PROPERTY
Hiseo/s.
" l r* i ftIM* I MX 4*11
L oh*
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CLAIM MAP
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Exploration work on the Cunningham Option property prior to 1969 consisted of limited prospecting and surface trenching for gold. Base metal exploration intensified in the immediate area following the discovery of the Mattabi base metal deposit in 1969.
The central part of the Cunningham Option property was covered by airborne follow-up work in 1970-71 by Mattagami Lake Mines. Two drill holes (309.4m) were completed to test an airborne conductor outlined by an earlier Questor survey. The conductor was found to be a graphitic argillite horizon at the top of the Six Mile Lake volcanic pile.
Prospecting by Cunningham and Chorzepa in the eastern part of the property in 1970 resulted in the discovery of the "CC" showing, a 37m long zone of heavy pyrite-pyrrhotite mineralization within carbonatized felsic lapilli tuffs and fine grained metasediments. A 37 unit claim block containing the showing was acquired in 1973 by Santa Maria Mines Ltd., with geological/geophysical surveys and diamond drilling (2 holes-61m) being completed. Slightly anomalous gold (1.88 gW2.7m) was encountered in a zone of coarse felsic fragmental rocks containing ID-50% pyrite over 4.5 to 6.1m. No significant base metal mineralization was found.
In 1982-83 a 31 unit claim block containing the CC showing was staked and geological mapping, stripping and trenching were completed by Canadex Res. Ltd., Playfair Res. Ltd., Santa Maria Res. Ltd. and Swansea Gold Mines Inc. in 1984. Santana Petroleum Ltd. completed a time domain IP survey for Canadex et al in 1985 and outlined a 1200m long anomaly coincident with several surface sulphide zones. The IP anomaly and surface showings were trenched and drill tested (10 holes-1520m) in 1985. A siliceous pyritic unit was intersected at the contact between pervasively carbonatized agglomerate-lapilli tuffs and finer overlying crystal and ash tuffs. The siliceous unit, averaging approximately 1.5m in width returned assay values up to 860 ppb Au and 511 ppm Zn.
5.0 1992 EXPLORATION PROGRAM
Initial work on the Cunningham Option property consisted of examination and sampling of Santana Petroleum Ltd's drill core at the Kenora MNDM Core Library. Selective analyses for base metals and whole rock geochemistry were completed.
The field program consisted of linecutting, geophysical surveying, and limited geological mapping and lithosampling, between July and October, 1992. A partial grid was established on the property with a 6.3 km baseline (Azimuth 070") extending across most of the claims. A detailed grid consisting of 200m spaced tie lines was cut over the main sulphide zone and 1 km spaced grid lines were established over the rest of the property.
A total of 10 km of magnetometer and moving loop PEM surveying was completed by Northwest Geophysics Ltd. of Thunder Bay over the detailed grid. Geological mapping and lithogeochemical sampling were carried out over the same area to upgrade the previous mapping and to establish the geological setting of the sulphide/alteration zone.
6.0 REGIONAL GEOLOGY
6.1 Stratigraphy
The Six Mile Lake area is situated in the North Sturgeon Lake Belt within the eastern end of the Archean Wabigoon Greenstone Belt. The regional stratigraphy from north to south comprises 2 south facing bimodal mafic to felsic volcanic cycles (Fourbay and Six Mile Lake cycles) overlain by a third mafic volcanic cycle (North Sturgeon Lake Cycle) (Fig. 3).
The Cunningham property straddles the contact between the upper Six Mile Lake Cycle felsic rocks and the basal massive to pillowed flows of the North Sturgeon Lake Cycle. Six Mile Lake Cycle felsic rocks are comprised of subaqueous pyroclastic flows, agglomerates, lapilli tuffs and crystal-ash tuffs capped by iron carbonate and sericite-altered tuffs and argillaceous metasediments. Pervasive quartz-sericite and iron carbonate alteration form a 9000m long zone of schistose rocks along the top of the eastern portion of the Six Mile Lake Cycle. The overall Six Mile Lake felsic package reaches a thickness of 6 km in the Cobb Bay area and thins in an eastward direction with an approximate thickness of 2.5 km in the vicinity of the Cunningham Option property.
The volcanic sequences have been intruded by numerous late mafic dykes, sills and sheets and by quartz-feldspar porphyry and feldspar-porphyry dykes and sills. Two feldspar porphyry stocks up to 1.5 km by 5 km occur north of the Cunningham property near King Bay.
6.2 Age Relations
The lower most Fourbay Cycle volcanic rocks are approximately 2.755 b.y. (Davis 1988) and are therefore the oldest in the North Sturgeon Lake Belt. The Younger Six Mile Lake cycle rocks have not been age dated however, they are correlative with the Handy Lake volcanic sequence within the Northeast Arm of Sturgeon Lake (Williams and Nacha, 1991). There is a 10 m.y. gap between the ages of the Handy Lake Volcanics and the Mattabi-Lyon Lake Mine stratigraphy (2735 1.5 Ma; Davis et al 1985).
6.3 Exploration Model
Felsic volcanic rocks of the Six Mile Lake cycle are prospective for Mattabi-type VMS deposits based on a number of similarities exhibited between the two sequences. Quartz crystal pyroclastic flows and ash flow tuffs similar to those which host the Mattabi deposit are present at the top of the Six Mile Lake Cycle, demonstrating a similar subaerial to shallow water environment. The semi- conformable Fe-carbonate alteration zone characteristic of the footwall of the Mattabi Mine is similar to the Fe-carbonate zone capping the Six Mile Lake pyroclastic unit on the Cunningham Option property. It should be noted that the characteristic aluminous mineral assemblages of the Mattabi footwall alteration zone have not yet been documented for the Six Mile Lake Cycle.
7.0 PROPERTY GEOLOGY
7.1 Lhhologies
The Cunningham Option property spans approximately 7 km of the contact between felsic pyroclastic rocks of the Six Mile Lake cycle and massive to pillowed flows of the overlying North Sturgeon Lake Cycle (Figure 4a). The ESE-trending units dip steeply and young to the south. Geological mapping of the entire property was completed by Cunningham, Smith and Masson (1983, 84) and more recently by Robinson and MacLean (1991) during regional government mapping. Limited
REGIONAL GEOLOGY
FIG.Aa PROPERTY GEOLOGY
WILLIAMS ZONE t-fSK MILE LAKE VOLCANIC C
CRYSTAL TUFTLAPiuj TUFTAGGLOMERATE
PYROCLASTICSVOLCANICS/!?!^/
* ^^ ^*'*.V
I:V STURGEON LAKE
NORTH STXJRGEOK LAKE VOLCANIC CYCLE
\f. MWMU.V
noranctaCUNNINGHAM PROJECT
spot mapping during 1992 was completed by Norex staff on the detailed grid area and on Line 1600E approximately 1.6 km east of the detailed grid (Figure 4b).
Felsic rocks covering the north half of the property are comprised predominantly of crystal to ash tuff, agglomerate and pyroclastic breccia, with lesser amounts of lapilli tuff, lithic tuff and quartz sericite schist. The felsic pile displays an upward (southward) and eastward fining sequence from a proximal to a distal setting.
Primary volcanic features are obliterated in the strong Fe-carbonate-sericite schist zone near the top of the felsic pile. Uppermost felsic lithologies include quartz-eye bearing crystal/lithic tuffs containing chert fragments and 0.2 to 0.5 cm round quartz eyes.
Massive to thinly bedded siliceous rocks near the top of the felsic pile may represent metamorphosed exhalite horizons. The sulphide zone appears to be hosted in a laterally discontinuous cherty horizon. Isolated exposures of clastic metasedimentary rocks (siltstone, argillite and greywacke) also occur near the top of the felsic sequence. These units are more abundant in the east part of the map area.
Mafic volcanic rocks of the North Sturgeon Lake cycle stratigraphically overlie and are locally interfingered with felsic pyroclastics along the lower contact. These rocks cover most of the southern half of the claim group. Fine to medium grained massive to pillowed flows predominate with lesser amounts of plagioclase phyric flows. Hydrothermal alteration has produced ubiquitous chlorite- amphibole mineralogy. Pillowed flows are often characterized by silicified pillow interiors and epidotized and chloritized rinds.
The volcanic stratigraphy on the Cunningham Option property has been intruded by a variety of late mafic to felsic dykes, sills and stocks. Narrow gabbro dykes and sills are present throughout the map area. A slightly irregularly shaped gabbro stock occurs in the northeast part of the property. Narrow quartz-feldspar porphyry and quartz-porphyry dykes are sparse. A late syenitic stock (Williams Syenite) has intruded the contact between felsic pyroclastic rocks and overlying mafic volcanics in the northeast part of the property.
7.2 Structure
The volcanic stratigraphy on the Cunningham Option property is steeply south-dipping and south facing as indicated by pillow top and graded bedding. Well developed east to east-northeast trending schistosity characterizes felsic pyroclastic rocks. Flattening of pillow structures and coarse fragments in mafic flows and felsic pyroclastic rocks is also generally easterly-trending. North to northwest trending faults with < 100m displacement have offset lithologic contacts along the main felsic-mafic contact.
7.3 "GC" Sulphide Zone
Sulphide mineralization in the CC zone was traced over a 1200 m strike length by IP, surface trenching and diamond drilling (10 holes-1520m) completed by Santana Petroleum Corp. This work determined that the mineralization occurs in a siliceous pyritic-sericitic-graphitic unit hosted with a stratiform, Fe carbonate-altered and deformed felsic crystal tuff horizon. The Fe-carbonate horizon persists for approximately a 9 km strike length at the top of the Six Mile Lake Volcanic cycle.
The immediate stratigraphy hosting the sulphide zone, as outlined by drilling, includes footwall lithic tuff, rhyolite porphyry and agglomerate and quartz-crystal sericite tuff and lapilli tuff in the hanging wall. Sulphide concentrations are often confined to massive siliceous to foliated sericitic tuffs and
locally to weakly bedded cherty and graphitic intervals. Clastic sedimentary intervals within the felsic pyroclastic sequence are restricted in strike extent and cannot be traced between drill holes.
The sulphide mineralization consists of blebs and stringers of pyrite and lesser amounts of pyrrhotite, ranging from 1 0*)ti py/1.5m to 25*^ py76.2m. Massive pyrite is absent, however narrow intervals of semi-massive pyrite (SO-60%) are present. Anomalous base metal values returned from previous drilling are insignificant, reaching only 550 ppm Zn. Gold assays returned from this drilling reached 0.055 opt Au/9 ft (1.88 g7t72.7m).
An examination of the footwall stratigraphy during the 1992 program revealed the presence of a weak alteration zoning. Strong silica-Fe carbonate-sericite alteration within the sulphide zone grades down stratigraphy into strong Fe-carbonate-hematite-sericite alteration, moderate Fe-carbonate-sericite alteration and finally weak Fe-carbonate-chlorite alteration. The same general alteration zoning occurs moving along strike to the east, corresponding with decreasing sulphide concentrations.
Although strong Fe-carbonate and moderate sericite alteration are both pervasive throughout the upper part of the felsic pyroclastic pile, the alteration zoning noted above is very limited in extent. Chlorite alteration characteristic of VMS footwall stratigraphy is very sporadic.
The abundance of fine lapilli and ash tuff and the matrix-supported nature of the coarser pyroclastic rocks suggest a somewhat distal setting for the sulphide zone. While the pyroclastic rocks at the top of the Six Mile Cycle generally exhibit an eastward fining sequence from proximal to more distal, a disruption of this pattern occurs on the Cunningham property. Mapping suggest a general increase in fragment size within agglomerate and tuff breccia horizons proceeding eastward on the Cunningham property indicating a change to a more proximal setting.
7.4 East Sulphide Zone
The East Sulphide Zone occurs approximately 2.4 km east northeast of the CC Zone. The mineralization was discovered in 1970 by Mattagami Lake Mines while drill testing a Questor AEM anomaly. A conductive zone situated on the north flank of a weak magnetic high was tested by 2 drill holes drilled from south to north. The holes encountered felsic pyroclastic rocks from the top of the same horizon which hosts the "CC" showing. Lithologies include felsic flows (rhyolite, dacite), crystal- lithic tuffs and graphitic crystal tuff. Weak chlorite alteration within rhyolite flows was noted in the drill logs. Mineralization consisting of pyrrhotite, sphalerite and pyrite is present locally within the sequence. Highest sulphide concentrations occur in conductive graphitic tuff horizons, where weak Au (0.14 g/t over 0.9m or 0.004 opt/3') was returned from core samples. No significant base metal values are reported.
Limited surface mapping in the vicinity of the conductor shows that the sulphide-bearing graphitic horizon occurs between 150 to 200m north of the felsic pyroclastic/mafic volcanic contact and is therefore in the same stratigraphic position as the "CC" sulphide zone. Limited outcrop exposure in the vicinity of the drill holes indicates the presence of quartz-eye bearing lithic tuff containing chert fragments and weak chl/ser alteration.
8.0 LITHOGEOCHEMISTRY
8.1 Reconnaissance Sampling
A total of 27 surface grab samples collected during 1992 were geochemically analyzed for major and trace elements (Appendix l, II). An additional 4 samples collected by OGS mapping crews from the vicinity of the Cunningham option property were acquired by Norex and submitted for whole rock analysis. Two samples from 1991 OGS mapping previously analyzed for whole rock geochemistry also occur on the property.
Approximately 7396 of the samples collected display Si02 values > 66 wt96 with 2496 containing in excess of 75 wt96 Si02 . Analyses show a lack of significant Na20 or CaO depletion in the area of the CC showing, with only one sample near the easternmost end of the showing returning < 1 wt96 Na20 and CaO.
Sporadic Na20 and CaO depletion occurs 1400m east of and along strike of the CC zone within sheared lithic-crystal tuffs (qtz-sericite schists) which are footwall to the pyritic/graphitic East Zone. The host rocks contain well developed quartz eyes and exhibit moderate to intense carbonatization and sericitization. Alteration indices (F20 + MgO7F2O 4- CaO * Na20 . 100) are highly variable from 16.7 to 70.2, indicating local Na20 depletion and Na2O enrichments.
A second area exhibiting Na20 depletion occurs within a chert fragment bearing quartz eye lithic tuff situated approximately 300m southeast of the CC Zone. This unit occurs stratigraphically above the CC Zone and contains weak to moderate carbonate-sericite and chlorite alteration. These rocks contain > 7596 Si02 and Na2O values as low as G.54%, however CaO depletion does not accompany those samples with *c 196 Na20. Alteration indices range from 31.6 to 61.6 but in general are < 60.
Trace element signatures suggest that felsic volcanic rocks on the Cunningham property which host the CC showing have been derived from deeper more primitive magmas. Compositionally, these rocks plot as F1 felsic volcanics (open circles, Fig. 6) on a Zr-Ti-Y Ternary diagram (Lesher et al 1985).
Felsic volcanic rocks collected from outside of the CC zone (solid circles, Fig. 6) appear to be more evolved, plotting in the Fll and Fill fields. These latter compositions are typically associated with rocks derived from high level magma chambers, and they are more likely to be associated with VMS mineralization. Although some of these rocks plot as Fill volcanics, the abundances of Y (28-54 ppm) and Zr (90-190 ppm) in these samples are generally lower than typical Fill highly evolved rocks (Y^80 to 150 ppm; Zr > 200 ppm).
8.2 CC Zone
Whole rock geochemical analysis was completed on 36 drill core samples from the 1985 Santana Petroleum Ltd. drill holes (Appendix II). Results from 36 samples spaced throughout the holes indicate a lack of significant VMS style alteration, such as Na20 and CaO depletion or MgO + K20 enrichments in the vicinity of the sulphide zone. Only one third of the samples contain Si02 in excess of 6696 wt96, and none of these display Na2O values of < 1.0 wt96. A felsic intermediate lapilli tuff located 82m below the sulphide zone in hole 85-7A returned G.63% Na2O however, CaO does not appear depleted in the same sample.
The drill core samples of Cunningham felsic rocks hosting the CC sulphide zone contain trace element abundances which plot in the FI and Fll fields on a Zr-Ti-Y Ternary diagram (Fig. 7). Again, as in the case of surface samples the compositions are more primitive than typical VMS-hosting felsic sequences. It should be noted that the majority of drill core analyses display a very high loss on ignition (LOI, Appendix II) indicating abundant hydrous phases are present.
6
FIG.6
L if H o s AM PL E S
o CC
"r -'"l fi ^x -- .k u
31)00
9.0 GEOPHYSICS
A magnetometer survey and a moving transmitter time domain EM survey were conducted on the Cunningham Option property by Northwest Geophysics Ltd. for Noranda between August 10-Sept. 1, 1992. The area surveyed consisted of a cut grid with 200m spaced tie lines extending 800m north of and 400m south of the baseline. The baseline is centered on CC sulphide zone.
The CC zone is situated within a broad magnetic low approximately 250m in width bounded by an area of elevated magnetics to the north and south. The area of higher magnetics to the south corresponds with the contact of the North Sturgeon Cycle Mafic Volcanics which overlie the Six Mile Lake Cycle. The zone of elevated magnetics to the north contains oval mag highs corresponding to lake gabbroic stocks, dykes and sills which have intruded the Six Mile Lake Cycle Volcanics.
The time domain EM survey was completed with a 5m diameter transmit loop and a Protem receiver, utilizing a 25m transmitter-receiver separation. All anomalies detected on the grid are single point and characterized by small amplitudes (see Appendix III). Anomalies at 37 * SON on Lines 0 + 00 and 6 * OOW correspond to the mineralization of the CC Zone. A third anomaly at 62 * SON on L 10 * OOW occurs 200m to the west of the CC zone mineralization but probably represents the along strike continuation of the zone. All anomalies are too small to be related to economic mineralization.
10.0 CONCLUSIONS AND RECOMMENDATIONS
The Cunningham Option property is situated at the top of the Six Mile Lake Volcanic Cycle within a pyroclastic-dominated stratigraphy which appears favourable for Mattabi-type VMS deposits. Initial similarities between the Mattabi deposit setting and the Cunningham property stratigraphy include the following:
1. Felsic pyroclastic sequences are dominated by bedded to massive quartz eye crystal tuffs and finer ash tuffs.
2. Semi-conformable footwall alteration zones comprise Fe-carbonate, quartz and sericite.
3. Absolute ages of the volcanic sequences at Mattabi and Six Mile Cycle are similar at 2735 my and approximately 2745 my respectively.
Data collected from the 1992 Exploration program lead to the conclusion that the main sulphide showing (CC Zone) and immediate host rocks do not constitute a significant VMS target. The reasons for this are as follows:
1. Footwall alteration zones are dominantly Fe carbonate and sericite and lack significant chlorite. Moreover, Na30 and CaO depletion which is characteristic in VMS footwall alteration zones is not present at the CC Zone.
2. A time-domain EM survey completed over the known sulphide mineralization failed to return any anomalies of significance, returning only weak single point anomalies indicating very small sources.
The second conclusion to be drawn is that the 1992 exploration work, although limited in extent, failed to detect any new targets on the Cunningham property. While features such as the extensive Fe carbonate and sericite alteration along a 7 km contact zone of felsic pyroclastics may still be indicative of hydrothermal mineralization, the following observations suggest that an economic VMS deposit does not likely occur on the Cunningham property.
1. The characteristic aluminous mineral assemblages of the Mattabi footwall alteration zone have not yet been detected on the Cunningham property. Strong chlorite alteration typical in most Mattabi-type /MS deposits is lacking.
2. Major element (Na 2O, CaO) depletions and enrichments (MgO) typically associated with VMS-hosting sequences are sporadic and do not define continuously altered horizons.
3. All airborne EM anomalies on the property have been drill tested with no significant base metals present in any conductor.
Future work on the Cunningham Option property should be oriented to outlining new targets for base metal mineralization. The program of lithosampling and geological mapping which was initiated in 1992 was terminated due to early snow cover. This work should be extended to cover the northeast part of the property. The work will have to be completed as soon as snow cover disappears, as a large option payment is due on June 1, 1993.
Respectfully Submitted,
NORANDA EXPLORATION COMPANY, LIMITED(no personal
Thunder Bay, Ontario February 1, 1993
A) Smith Project Geologist Northwest Ontario District
REFERENCES
l^unningham, L. J. 1989: Report on the Sturgeon Narrow property of Swansea Gold Mines Inc. and Northex Management, Sturgeon Lake area, Ontario; Assessment Files, Resident Geologists Office, Sioux Lookout District.
Cunningham, L. J., Smith, A. R. and Masson, M. W. 1984: Report on the Sturgeon Narrows property, Canadex Resources Limited, Playfair Resources Limited, Santa Maria Resources Limited and Swansea Gold Mines Inc.; Assessment Files, Resident Geologists Office, Sioux Lookout District, 18p.
Davis, D. W., Krogh, T. E., Hinzer, J. and Nakamura, E. 1985: Zircon Dating of Polycyclic Volcanism at Sturgeon Lake and Implications for Base Metal Mineralization; in Canadian Journal of Earth Science, v. 80, p. 1942-1952.
Davis, D. W., Sutcliffe, R. H. and Trowell, N. F. 1988: Geochronological constraints on the tectonic evolution of a late Archean greenstone belt, Wabigoon Subprovince, northwest Ontario, Canada; in Precambrian Research, v. 39, p. 171-191.
Lesher, C. M., Goodwin, A. M., Campbell, l. H., and Gorton, M. P. 1986: Trace Element Geochemistry of ore associated and barren, felsic metavolcanic rocks in the Superior Province, of Canada; Can. Journal of Earth Sci., V23, 222-237.
Robinson, D. J. 1992: Geology of the Six Mile Lake area; Ontario Geological Survey Open File Report 5838, 93p.
15
APPENDIX l
LITHOSAMPLE DESCRIPTIONS AND LITHOLOGIC UNIT DESCRIPTIONS
CERT. NO.
NORANDA EXPLORATION COMPANY. LIMITED
PROJECT NO. /336 PROPERTY
GRID REFERENCE N)g)r*ex 6-r*.J
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N.T.S.
DATE
SAMPLE REPORT
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NORANDA EXPLORATION COMPANY, LIMITED
PROJECT NO. 1 33 (p PROPERTY C
GRID REFERENCE Nlo*-grf fiW/J
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SAMPLE REPORT
SAMPLE DESCRIPTION TYPE WIDTHA.QSAVS
c.^)* CO-ORDINATES•AMPLE*
4^ {La s b
lapilli T-WTT JZ- AH-. SS LIH-9SWWO
Felsi c . u/k 3 r-db —rF* Is; dtT"t* n M7 0+15 +J
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DATE ^-K '"1*2
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NORANDA EXPLORATION COMPANY. LIMITED
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NORANDA EXPLORATION COMPANY. UMITED
PROJECT NO. l?g^ PROPERTY
GRID REFERENCE '
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SAMPLE REPORT
N.T.S. 52 G X'S"
DATE 0^\ '
SAMPLE DESCRIPTION TYPE WIDTHASSAYS
CO-ORDINATES•AMHM
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Lithologic Unit Descriptions
lafic Volcanics: - fine to medium grained, light to dark grey-green.- predominantly massive and pillowed flows with minor pillow breccia and flow
breccia.- locally plagioclase-phyric.- ubiquitous chlorite-amphibole mineralogy with local epidote and silica-rich
intervals.- minor disseminated euhedral pyrite.
Intermediate Volcanics: - fine to medium grained, light grey-green.- predominantly massive to pillowed flows of limited geographic extent
intercalated with mafic flows.- generally weakly carbonatized with local moderately chloritized and/or
silicified intervals.
Felsic Volcanics: - variable fine to medium grained, light grey to white.- predominantly fine ash tuff (quartz-eye bearing) with lapilli/lithic tuff
agglomerate and pyroclastic breccia.- generally quartz or quartz-feldspar phyric with heterolithic character (fragment
compositions include felsic to mafic volcanic, pumice, and chert (ash tuff?).- alteration typically moderate carbonatization with local zones of sericite,
hematite and epidote.- upper part of sequence is dominated by an iron carbonate sericite schist zone
where primary volcanic features are no longer obvious.
Mafic Intrusives: - medium to coarse grained, green-brown colour.- predominantly gabbroic sills and dykes.- generally massive, with locally pyroxene-phyric phases.- alteration generally moderate to strong chloritization and carbonatization.- chilled aphanitic contacts locally visible.
14
APPENDIX II
GEOTECHNICAL ANALYSES AND ASSAY RESULTS
MORANDA EXPLORATIONraumni MY n-2136*TTM:8M1TK
SAMPLE f
4-B4-P
4-O
4-M
4-1
4-J
4-K
4-L
5-H
5-1
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VLaboratoiros TSL/ASSAYERS Laboratories
780 M . Ml CVIVRI C. P. 669 KWVH-NOIUUIM OJUIMC J9X 9C6 nnm t: 819-797-4693 HkX ffi 619-797-4901
I.C.A.P. WHOLE ROCK ANALYSISLlthlua H*t4tBorot* Fusion
•wort MO. i T2194F*9* Ho. : l of lFi l* Ho. : N019IA
: NOV-25-1992
8102*
64.9872.9170.5770.6754.03
44.0178.0876.7063.2079.16
75.1375.8782.70
A1203K
14.8612.5412.4415.2310.53
9.4312.0011.297.50
12.53
13.088.65
11.93
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4.064.066.051.85
21.84
30.312.824.272.741.66
3.522.310.50
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ft
3.072.381.741.963.94
2.210.571.450.291.19
0.224.630.21
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0.470.510.610.272.26
1.960.420.900.120.30
0.380.920.19
M20*
4.391.693.014.660.23
0.203.932.220.731.02
2.650.541.58
X20t
1.422.960.921.060.10
0.261.302.121.323.24
2.561.961.10
T1O2t
1.070.240.210.150.31
0.330.090.180.240.12
0.390.120.20
ttoO9
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1.450.060.090.120.02
0.060.09
40.01
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0.460.080.080.040.10
0.080.040.040.060.04
0.080.020.04
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21571
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63
4457698039
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2601*8
68
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2228
644
1436281494
3246
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136324
73992
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2.941.981.991.916.11
7.421.171.511.601.62
1.974.131.75
TOTAL
t
97.8299.4097.6897.66
100.04
97.6*100.46100.3297.92
100.9O
100.2799.02
100.16
L/92•IONIC
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: BI9-7f7-4*59 HUC ffi Bl*-7f7-4SOl
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141
141
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l.C.A.P. WHOLE ROCK ANA1Y8I8
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•o. i*71. Ol 50.91 47.4* 7*. 63
173
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100.41
100.6* 6.37^ M..90
TSL LABORATORIES2-302-48th STREET, EAST
SASKATOON. SASKATCHEWANS7K6A4
l (306) 931-1033 FAX: (306) 242-4717
CERTIFICATE OF ANALYSIS
SAMPLE(S) FROM Noranda Exploration Company Limited 960 Alloy Drive Thunder Bay, Ontario P7B 6A1
REPORT No. S4962
INVOICE #: 20297 SAMPLES) OF Rock P.O.: PN:82023XTB2138
ASSAYS
Cu Zn ppm ppm
214-E 22 39214-F 21 140214-G 24 81214-H 26 30214-1 19 100
214-J 21 76214-K 11 40214-L 8 44215-H 10 43215-1 22 100
215-J 3 34215-K 19 76215-L 2 3
COPIES TO: R. Felix, A. Smith INVOICE TO: Noranda Expl.- Thunder Bay y- J
•tpttSZNov 13/92 7 y ' JS/. . 7 C TA
SIGNED .
For enquiries on this report, please contact Customer Service Department. Page l Of l Samples, Pulps and Rejects discarded two months from the date of this report.
OCT23 TSL LABORATORIES2 - 302 - 48th STREET, EAST
SASKATOON. SASKATCHEWANS7K6A4
l (306) 931-1033 FAX: (306) 242-4717
CERTIFICATE OF ANALYSIS
SAMPLE(S) FROM Noranda Exploration Company Limited 960 Alloy Drive Thunder Bay, Ontario P7B 6A1
SAMPLE(S) OF Rock/Core
REPORT No. S4912
INVOICE #: 20240 P.O.: PN:820847TB2113
ASSAYS
UJV o u
o?o
x/vUJ
i lO
H85-3-23.0H85-8-16.7H85-8-63.1H85-8-119.6H85-3-72.0
H85-7-50.5H85-8-148.1H85-2-65.7214-A214-B
214-C214-D215-A 215-B 215-C
Cu ppm
6140
12001846
2526305
56
5102741
140
Zn ppm
1050
13010065
8085847
30
1341553839
215-D 215-E 215-F 215-G
19223718
35478827
COPIES TO: INVOICE TO:
Oct 23/92
A. Smith, J. Sullivan Noranda Expl.- Thunder Bay
SIGNED nLyt<<^^^x*•CTA
For enquiries on this report, please contact Customer Service Department.Samples. Pulps and Rejects d iscarded two months from the date of this report.
Page l of l
APPENDIX III
GEOPHYSICAL INTERPRETATION REPORT AND PROTEM PROFILES
GEOPHYSICAL INTERPRETATION REPORT
PROJECT: CUNNINGHAM 1326
SURVEY: Time Domain EM (Protem)
DATE: January 14, 1993
FROM: Greg Hodges
A moving transmitter time domain EM survey was conducted on the Cunningham property in September, 1992. The survey employed a 5m diameter transmit loop and the Protem receiver. Transmitter- receiver separation Was 25m, and the pulse rate was 30Hz.
The survey was conducted on lines 200m apart, from 0H to 1000W, and final coverage was from about 400S to 600N. Three components of the secondary field were measured.
Due to the lack of background signal, the data are plotted at a greatly expanded scale, which enhances the noise level.
The anomalies observable in the Cunningham data are all single point and very small amplitude. The only ones which merit a second look are at 37.5N on L0, 37.5N on L600W, and 62.5N on L1000W. Even these are very small, single station anomalies whose only significance is that L0 and L600H lie on the previously detected showing. The anomalies all show late channel decays, but no early time response. The small size of these anomalies is in discordance with their strong (20-channel) decay, which usually results from a large, conductive body.
The L600W anomaly is single point, and reversed from the expected anomaly. The reversal may be due to aliasing caused by the reading interval being too long, but even if this is so the source could only be very small. The L0 anomaly is only in the Z component, and although it was repeatable, it too is hard to accept as real. If it is real it is also caused by a very small source.
To summarise: The anomalies observed in this data are very small and questionable in nature. If they are real they are due to very small sources, below the threshold of interest considering the other work and results on this part of the property.
The rest of the property has very little to encourage interest for further work. The contact has been surveyed with Helicopter EM, and shows no interesting anomalies. The lithogeochemical results do not show strong alteration typical of the alteration envelope around a large deposit. (Al Smith) The only remaining cause to be there is a favourable contact with poor lithogeochem, no strong conductors above 100m and no past producers or deposits along strike. The only geophysics which could detect new targets would be deep search EM, the cost of which does not appear warranted by the results to date.
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(meters)
CUNNINGHAMMoving Coils TEM
L200 WMULTIPLE COMPONENTS
Property : CUNNINGHAM Proj# : 1326 Date : Sept, 1992 Files: tcun2wa
tcun2wc
no ran daExploration Company LJmltad
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CUNNINGHAMMoving Coils TEM
L400 WMULTIPLE COMPONENTS
Property : CUNNINGHAM Proj# : 1326 Date : Sept, 1992 Files: tcun4wa
tcun4wc
norandaExploration Company Umlt*d
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CUNNINGHAMMoving Coils TEM
1000WMULTIPLE COMPONENTS
Property : CUNNINGHAM Proj# : 1326 Tx Loop : Date : 1992NTS :
no ran daExploration Company Limited
APPENDIX IV
LIST OF PERSONNEL
List of Personnel
Felix 101 Essex Court, Thunder Bay, ON P7A 7N4
Al Smith 251 London Drive, Thunder Bay, ON P7A 7Z6
Craig MacDougall 522 Dalhousie Ave., Thunder Bay, ON P7C 5P8
List of Contractors
Vytyl Exploration Services 1529 Rankin St., Thunder Bay, ON P7E 5Z2
Northwest Geophysics Ltd. Box 3263, Thunder Bay, ON P7B 5E8
Address of Claim Holders
Mr. L. J. Cunningham 1 McPhee Avenue, Kirkland Lake, ON P2N 1M1
13
APPENDIX ill GEOPHYSICAL METHOD AND RESULTS
MAGNETICS
A magnetic survey measures alterations in the earth's naturally occurring magnetic field caused by changes in the magnetization of the rocks in the earth. These changes are due mainly to the presence of the magnetic minerals: magnetite and to a lesser extent pyrrhotite and ilmenite. Mapping these minerals can be an aid to geologic mapping.
The magnetic data were collected with a proton precession magnetometer, which measures the absolute value of the total magnetic field of the earth to an accuracy of .±.0.1 nTesla. Readings are normally taken at 12.5m intervals. Correction for diurnal drift was by reference to a base station magnetometer.
The magnetometer used was a EM Omni IV.
PROTEM TDEM
PROTEM is a time domain electromagnetic system, which transmits a 30Hz square wave pulse with a 150usec ramp turn-off (the primary field) to induce currents in conductors. The response from the decaying currents in the conductor (the secondary field) is measured at surface or in a borehole at 20 logarithmically based time windows for 7msec after the pulse. The receiver utilises an air-cored coil of 100m3 dipole moment, which is carried to each station on the grid. The transmitter is a 5m diameter loop with 8 turns of wire, driven at 15A by a 600W motor generator, placed 25m from the receiver at each station. Three components of the secondary field are measured, the vertical (Z) and horizontal along-the-lines (X) and cross-line (Y), to enable the best interpretation of the geometry of the conductor.
Conductor geometry is determined from the secondary field shape, and conductivity thickness from the time decay characteristics of the secondary field.
SURVEY STATISTICS
The field geophysics was carried out by personnel from Northwest Geophysics Ltd. of P.O. Box 3263 Thunder Bay, Ont. P7B 5E8. In charge of the field work was Alfred Lambert, of NWG. Supervision of the geophysics was by John Gingerich of Noranda Exploration, 960 Alloy Dr. Thunder Bay, Ont. P7B 6A1. Interpretation of the results was by Greg Hodges, also of Noranda.
A total of 16.93km of lines were cut, on which the geology was mapped (20 man- days) and 7.8km of magnetics and 7.8km of time domain EM were surveyed. Ten man-days of supervision were required.
INTERPRETATION
Due to the lack of background signal, the EM data are plotted at a greatly expanded scale, which enhances the noise level.
The anomalies observable in the Cunningham data are all single point and very small amplitude. The only ones which merit a second look are at 37.5N on LO, 37.5N on L600W, and 62.5N on L1000W. Even these are very small, single station anomalies whose only significance is that LO and L600W lie on the previously detected showing. The anomalies all show late channel decays, but no early time response. The small size of these anomalies is in discordance with their strong (20-channel) decay, which usually results from a large, conductive body.
The L600W anomaly is single point, and reversed from the expected anomaly. The reversal may be due to aliasing caused by the reading interval being too long, but even if this is so the source could only be very small. The LO anomaly is only in the Z component, and although it was repeatable, it too is hard to accept as real. If it is real it is also caused by a very small source.
CONCLUSIONS AND RECOMMENDATIONS
The anomalies observed in this data are very small and questionable in nature. If they are real they are due to very small sources, below the threshold of interest considering the other work and results on this part of the property.
The rest of the property has very little to encourage interest for further work. The contact has been surveyed with Helicopter EM, and shows no interesting anomalies.
Respectfully Submitted,
Greg Hodges, Geophysicist
COST BREAKDOWN
Linecutting
Geophysics:
Protem: Magnetometer:
Wages:
Labour Supervision
16.93 km
7.78 km 7.78 km
Total
20 mandays 10 mandays
Total
Total
48,750.00
46,000.001.150.00
47,150.00
45,914.003.147.00
49,061.00
c:\wp61\e.n*rt*lu*ow .00*
7
2
9
6
5
4
2
I
2
2
9
3
9
5
9
2
9
2
ey.T-
XLINE 1 X
9203
9203
9203
9203
9203
LINE 2 Y9203
9203
9203
9203
9203
LINE 3 Z9203
9203
9203
9203
9203
LINE 4 T9203
9203
9203
9203
9203
y
20
30
40
50
60
20
30
40
50
60
20
30
40
50
60
20
30
40
50
60
STN Priiary CH1
20 -18152.1 -1717.35
30 -15834.1 -1588.22
40 -12296.4 -1107.3
50 -9779.97 -863.634
60 -7879.89 -634.194
20 -0.0 -116.250
30 -0.0 -102.166
40 0.0 -47.868
50 -0.0 -92.723
60 -0.0 21.692
20 -5576 1239
30 -1667 1302
40 2818 1243
50 4926 1128
60 5798 1004
20 18989.2 2120.835
30 15921.62056.231
40 12615.2 1665.369
50 10950.5 1423.673
60 9783.1 1187.724
CH2
-334.028
-268.893
-69.596
-46.254
36.500
-2.055
-59.070
19.321
-42.649
-13.214
462
482.3
459.6
402.4
341.5
570.108
555.343
465.241
407.289
343.699
CH3
79.926
102.548
166.711
153.040
185.505
-9.654
-7.051
9.619
-11.700
-8.655
389.7
197
184.6
139.4
72.72
206.076
222.204
248.922
207.342
199.437
CH4
108.827
120.628
165.808
147.310
159.701
-9.739
-9.557
13.454
-7.098
-5.112
86.21
77.18
77.41
39.6
-19.34
139.378
143.524
183.482
152.705
160.949
CHS
105.301
102.968
176.964
125.121
129.000
-8.318
1.843
47.547
0.502
-2.928
38.83
43
31.32
-2.129
-56.51
112.540
111.601
185.898
125.140
140.865
CH6
83.382
88.217
149.781
105.996
113.659
-2.585
-1.229
38.701
-4.295
-1.604
15.93
18.46
3.042
-23.64
-71.12
84.930
90.136
154.730
108.685
134.086
CH7
74.627
74.797
133.804
86.689
101.778
-4.070
-2.464
39.240
-4.972
-1.764
7.206
2.366
-5.902
-30.66
-66.86
75.084
74.875
139.564
92.086
121.788
CH8
60.103
61.738
106.735
75.499
81.360
0.859
-9.282
28.258
-0.467
-0.818
1.909
1.082
-10.13
-37.2
-69.73
60.140
61.748
110.876
84.166
107.156
CH9
50.131
55.735
90.477
63.737
72.332
-0.751
-5.550
18.615
-1.404
-1.375
-2.339
-3.827
-11.47
-31.07
-64.85
50.191
56.142
93.082
70.920
97.156
CH10
43.158
43.947
84.896
55.002
57.510
-3.973
0.515
25.239
-3.815
-1.310
-1.261
-3.829
-12.92
-30.31
-56.82
43.359
44.116
89.596
62.916
80.855
etc.
31.56
35.69
45.63
43.99
45.91
-1.67
-3.81
0.53
-0.16
-1.60
-1.82
-3.27
-12.1
-28.4
-53.8
31.65
36.84
47.23
52.39
70.80
l MULTIPLE COMPONENT, MULTIPLE CHANNEL TIME DOMAIN EH DATA 6EOSOFT SAMPLE FILE Eron Greg Hodges, Noranda Exploration Co. Ltd l This is the foriat for lulti-channel data settled on within Noranda Exploration. The problei Mith TDEH data is the lany channels l and the mltiple spatial conponents that comprise a reading at a single location. Geosoft cannot handle non-nuieric data (eg X,Y,Z), l and storing the coiponent as a nuiber in the data lakes it difficult to access the information Mith standard software to control l plotting. Host current IDEM software (Geotervex, Crone, Ouantech) uses a single survey line per file foriat, and the lost coiion l p lot foriat is a all-channels, single line, single coiponent profile per plot sheet, so that is continued here. To divide the l coiponents they are defined as separate lines, LINE 1:X, LINE l^d 3=2, and 4:T(otal Field). The X position currently holds the line l nuiber, or in this case the drill-hole nuiber.l T his is an easy foriat froi which to access the desired coiponent for plotting single line profiles with a HAPPLOT. It keeps l a ll of the data for one line (and anoialy) together, rather than broken into coiponents. It does not allow for easy lap plotting and l contouring of data. Ideally all of the data for a grid would be stored in one file, perhaps with a designator in the LINE label to l i ndicate the coiponent. This could be a variation of the LINE, TIELINE, etc. capabilities, and would fit in with the current systei
j/ for selecting data types to plot. The current 22 data fields is just long enough for the PROTEH's 20 channels (plus station andl i - -.•-.....I l..,t. ..-t f,, f,*^*i* ..A,..'...,. ~ l tt A ll -it . .. —.t -J4..,.. ,,~~J Tnry .-.^-^l^no y^^,,l,n .-.^.. -~r* ^k.^^^l^________________
/CUNNINGHAM 1326 PROTEH57 HCTEH Si x Si l 25n,15A Line l X
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8.0 162.5 162.5 8.800 7.170 .634 0.773 -8.098 0.406 0.015 -0.606
0.0 137.5 137.5 0.066 -7.310 .817 -0.128 0.287 -0.195 -0.261 8.684
0.0 112.5 112.5 0.000 -12.080 .824 0.415 -0.669 1.039 -6.235 -6.322
0.0 87.5 87.5 0.600 -1.107 .384 0.259 0.348 0.102 -0.456 6.235
0.0 62.5 62.5 0.000 9.628 .051 -0.392 0.496 -1.467 1.381 -0.121
0.6 37.5 37.5 0.000 7.754 .789 -3.714 0.516 0.454 0.052 -0.078
6.6 12.5 12.5 6.000 -0.696 .984 -0.133 0.115 0.342 -0.291 -0.025 Line 2 r
0.0 587.5 587.5 0.000 -4.734 .375 1.644 0.138 0.474 -0.328 6.643
8.8 562.5 562.5 8.008 -3.909 .931 -1.021 0.262 8.765 -0.163 0.269
8.0 537.5 537.5 8.008 11.890 .581 8.332 -0.373 0.062 -0.680 0.060
8.8 512.5 512.5 0.000 3.581 .391 1.068^-0.108 -0.446 0.023 -0.046
6.8 487.5 487.5 6.808 -1.594.962 6.266 -0JB3 t.814 -e.022 9.133
____g a j i") c, ILI c. flflflfl o ma
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-208.0 537.5 537.5 0.000 -16.930 21.968 4.881 -14.888 5.192 8.528 -8.354 -8.343 -8.358 8.475 -8.861 8.658 8.127 0.195 0.128 0.217 -8.219 8.024 0.028 0.223
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-288.0 612.5 612.5 0.888 9.484 16.818 3.612 -13.318 5.458 3.895 1.319 2.832 -1.786 -8.475 -0.346 0.468 0.343 -0.724 0.320 0.156 0.093 0.019 0.251 -0.139
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Line 2 Y-268.0 12.5 12.5 8.
.588 -8.526 8.812 8.814-200.8 37.5 37.5 8.
.567 8.881 -8.285 -8.425-208.8 62.5 62.5 8.
.067 8.217 -0.150 8.208-200.0 87.5 87.5 t.
.371 -8.835 0.024 -0.046-200.8 112.5 112.5 8.
.168 -8.369 -0.012 -8.228-208.8 137.5 137.5 8
.221 8.162 -0.009 -8.858-288.8 162.5 162.5 8.
.899 -0.182 0.669 8.269-288.8 187.5 187.5 8.
.223 -0.369 0.169 -0.293-280.0 212.5 212.5 8.
.059 -0.241 -0.257 0.025-200.0 237.5 237.5 0.
.622 -8.788 -8.887 -8.434-200.0 262.5 262.5 0.
.382 -8.005 0.011 8.365-200.0 287.5 287.5 0.
.006 0.124 -8.219 -8.895-208.8 312.5 312.5 8.
.024 -0.099 8.523 -8.277-208.0 337.5 337.5 0.
.550 -0.083 -8.532 -8.388-208.0 362.5 362.5 8.
.356 -0.209 0.086 -8.658-200.0 387.5 387.5 0.
.211 -8.208 0.463 -0.896-208.0 412.5 412.5 8.
.873 8.285 0.096 0.417-208.0 437.5 437.5 0.
.949 8.868 8.154 -8.096-208.0 462.5 462.5 0.
.582 1.808 0.125 -8.131-208.0 487.5 487.5 0.
.773 -0.191 0.686 -8.193-288.0 512.5 512.5 0.
.256 0.602 0.082 0.105-200.8 537.5 537.5 8.
.498 -0.198 -0.333 0.137-200.0 562.5 562.5 8.
.436 8.871 8.125 8.482-200.0 587.5 587.5 8.
.544 0.101 -8.458 0.117-200.0 612.5 612.5 8.
.428 0.261 -0.168 -0.287-208.8 637.5 637.5 8.
.861 1.821 -8.189 -8.166-280.0 662.5 662.5 8.
.564 -8.232 0.088 8.928-208.8 687.5 687.5 8.
.428 0.499 -0.143 -8.272-200.0 712.5 712.5 0.
.817 -0.220 1.032 8.151-208.8 737.5 737.5 8.
.215 8.192 -8.156 -8.292 Line 3 Z
-288.0 ^2.5 12.5 7218. .350 -0.163* -8.178 -0.879-m. B 37.5 37.5 9UB.
.777 -0.601 -0.340 -0.4!0
m 8 .518-0.225 -0.018 m - 11.598-8.882 -8.869 808 -1.9110.003 -0.140
888 -3.2320.268 -0.392
888 4.8728.189 -8.165
888 0.148-8.143 -8.137 888 1.135-8.226 8.886 888 -6.583-8.313 -8.839 888 8.571-0.427 0.210 080 -5.556 0.176 -0.143
008 -2.711-8.192 8.888 888 -4.664-0.084 -8.801 800 -12.188-0.882 -8.194 888 -2.435 8.817 -8.117
888 2.484-8.197 8.315 888 1.268-8.363 8.274 088 -8.9710.142 8.245
000 2.5638.822 -8.188
800 -3.4020.129 -0.831
008 -6.9690.256 -0.052
000 -9.7970.423 -0.352
888 8.015-0.152 -8.556 888 7.816 8.558 -8.478
888 -7.189-8.284 8.214 888 8.178-8.867 -8.850 088 4.378-8.119 -8.382 888 -13.378-0.247 -0.176 880 -8.323-0.865 -8.898 888 -5.737 0.045 -0.132
088 -2.988-0.125 -8.328
888 12.488-8.847 -8.888 m -J2.880-8.343 -0.281
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-1.686 -1.344 -2.961 0.537 3.408-0.088 0.010 -8.106 -0.0353.339 6.445 -3.650 4.087 -3.697
0.124 -0.067 0.055 -0.050-8.942 -6.797 7.639 -8.330 -3.838
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6.712 1.698 -1.479 1.459 -8.7240.189 -0.120 -0.012 8.029
-5.784 2.294 -1.736 1.702 -1.0490.127 -0.004 0.002 -0.047
5.887 -12.230 1.497 6.224 -1.083-0.038 -0.096 -8.004 -0.0817.692 -1.746 -1.236 -4.345 2.462
0.051 0.083 -0.190 -0.053-5.734 0.487 5.681 0.382 -8.046
-0.020 8.055 8.018 -0.147-1.863 6.680 -7.066 1.483 1.188
-8.032 8.259 8.145 -8.804-6.256 0.499 -2.468 1.955 -4.153
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0.874 -8.346 -8.858 -0.8885.248 3.343 -2.283 1.186 1.938
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8.179 -8.038 -8.828 0.0837.188 1.637 -2.975 1.851 0.073
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8.898 8.239 -0.131 -0.04718.988 -9.954 -7.591 2.461 4.583
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6.658 1.853 8.889 -3.575 -0.-0.000 -0.000 8.000 -0.008
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-8.896 -8.739 -8.877 -8.510
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-288.8 662.5 662.5 7888..898 -6.166 8.427 8.157
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186 -6.394-8.497 -8.307900 39.890-8.243 -8.163988 38.180-8.168 -0.092808 -7.8218.423 8.259
980 32.4668.368 6.221
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6.124 8.198888 -13.778-8.234 -0.134000 -6.889
8.267 0.118008 -4.244
0.298 0.294
13.410-8.289
-2.844-8.898
-1.143-8.649
18.7668.227
2.8846.144
4.869-6.1135.849-8.8747.8628.866
-1.174-8.1479.699-8.3175.967
8.8839.624-6.1167.872-8.2198.564-6.3458.878-8.841
-8.531-8.2788.798-6.210
-8.191-8.2896.111-8.1638.443
8.6644.712
8.1515.544-6.1648.833-8.199
-8.813-8.8387.532
6.6650.118-6.156
14.2468.156
13.9488.177
••Mi-2.245-8.157
1.546-8.0823.884
-6.8933.2868.1284.3828.8652.189
-8.894-2.115-6.8761.968
-8.886-1.868-6.162-2.342-8.196-2.423
8.8891.789
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-8.2188.766
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-8.106-3.317-8.139-2.352-8.6144.2528.185
-8.282-6.0832.7558.8928.9276.145
VBVMi-1.950
-8,154-8.393
-8.828-4.782
-0,0431.695
6.1412.124
8.1338.745
-8.827-2.134
-8.8568.431
0.638-1.389
-8.878-3.379
-8.1122.871
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-8.126-1.4188.081-1.529
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-8.894-8.8236.0586.543
8.857-3.822
-8.619-6.684
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-6.092-1.1788.058-8.6788.154
-2.158-8.185
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1.996-0.839
8.9586.866
8.4858.836-1.321
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0.825-2.321
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0.8478.748
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0.0118.646
6.866
•^M^M-2.266
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1.888
8.716
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1.531
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-8.816
-0.161
1.386
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1.273
8.951
-8.971
1.968
0.515
mmmnmm -6.831
-8.918
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8.971
0.977
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8.559
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8.588
8.689
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8.212
8.648
mmmmm -1.273
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1.468
8.744
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8.417
1.878
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6.765
6.881
-8.764
8.669
8.468
•^•IVHM
-8.971
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8.838
8.763
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6.168
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8.239
8.949
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6.585
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-8.895
8.394
8.632
••••RVB
-1.875
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8.353
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8.297
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8.393
8.736
6.827
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1.853
8.484
M-0
-8
-8
8
6
-0
-0
-0
-8
-0
-8
-0
-0
-3
0
-0
-0
-1
-8
0
8
-8
-8
6
0
-8
0
8
/CUNNINGHAM 1326 PROTEK57 HCTEM 5n x 5* ! 25i,15A NORTHUEST Line l X
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-280.0 -362.5 -362.5 0.000 -3.801 -6.008.115 -0.232 0.211 -0.249 0.100 0.177 0.026
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/CUNNINGHAM 1326 PROTEHS7 HCTEH Si x Si l 2Sl,lSA NORTKUEST 1992 RaM File:stur3.dat
5
2
2
8
8
4
5
3
4
1
7
5
7
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5
3
9
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8.431 ^.442-m m. 5
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8 2.397.278 8.222
8 2.7541.145 -0.1300 5.6481.256 8.1398 -0.2581.347 -0.1570 -3.1281.427 -0.3270 8.1611.449 -0.3550 -22.7801.523 -0.355|0 0.8881.084 -8.81318 -6.4331.241 6.14618 -23.2781.337 -8.22418 -6.5781.861 -0.04410 -22.180).301 0.24610 -17.820J.552 -0.42810 -0.8591.875 -8.07410 4.5569.552 -0.41818 -11.7989.878 -0.83518 21.190
.753 -6.546 -8.453 -8.470 -8.343 -8.287-668.6 12.5 12.5 14668.6(
.541 -8.788 -8.416 -0.483 -i)0 1.0878.327 -0.222
3.986-0.2194.898-8.2862.673-8.8151.409-0.167
13.1800.204
10.0700.323
-1.948-8.282
-1.689-8.1714.939-8.8824.388
8.2182.8500.168
2.113-0.0891.369
0.892-1.869
-8.2748.614-8.2862.992-8.2761.229-8.2382.187
8.6163.416
8.1472.365-8.2863.764-6.8597.8188.127
3.189-8.3831.316-8.864
-8.875-6.3176.438-8.837
-5.587-8.192
-6.851-0.185
•^•M^M
-4.256-0.118-2.844-8.170-3.892-0.0030.285
-0.0972.7280.1118.2678.196
-2.658-8.146-1.945-6.124-2.785-8.1212.8888.1768.4888.698
-2.229-8.671-1.277
6.632-1.413-6.139-3.381-6.188-2.389-8.158-2.145-8.2128.7588.8170.6188.1368.782
-8.137-2.915-8.013
1.1788.696
-3.858-8.229-2.375-8.805-3.645-8.2876.462
-8.846-4.772-6.118-2.868-8.126
-3.397-8.891-1.988
-6.892-1.7418.068-6.565
-8.0741.536
0.8841.618
8.123-2.324
-8.885-1.782
-8.118-2.5786.6318.753
6.6941.384
8.896-1.149
-8.0580.771
6.685-1.213
-0.849-8.686
-8.691-1.141
-8.134-2.748
-8.6921.397
8.664-2.1746.018-8.758
-8.862-2.642
-8.0130.022
8.635-2.717
-6.143-3.892
-8.016-2.181
-6.165-8.2600.086
1.389-8.865-1.245
-6.682
-3.720-0.843
-2.436-8.662
-1.9418.068-8.552
-0.6352.289
8.8628.156
8.891-2.785
-8.849-2.089
-0.055-1.845
0.6831.462
6.0208.411
8.826-8.762
-6.834-8.133
-8.824-1.349
-8.871-2.624
-8.864-1.413
-8.054-2.472
-8.8808.179
8.861-8.582
0.831-8.583
-8.851-8.445
-8.6101.866
8.026-2.528
-8.874-1.856
-6.019-1.717
-0.1828.552
8.886-3.722
-8.855-1.960
-8.641
-2.818
-1.428
-1.454
-8.483
8.478
1.848
-2.415
-1.466
-1.698
1.277
1.464
-8.892
6,261
-2.234
-1.839
-0.721
-2,119
0.671
-0.358
-8.659
-1.673
1.829
-1 .786
-0.914
-1.681
-0.774
-1.135
-1.622
•^^•^^•^ -1.620
-1.715
-1.855
-8.927
8.321
1.848
-2.837
-1.891
-1.877
1.985
1.433
-8.934
8.596
-0.884
-1.088
-0.670
-1.520
6.633
-8.547
-1.493
-1.898
8.664
-1.479
-8.174
-1.288
-8.141
-1.881
-8.913
-1.676
-1.386
-8.824
-8.291
1,655
1.315
-1.581
-8.931
-1.218
1.555
8.936
-8.485
8.495
-1.373
-1.282
-8.553
-1.645
6.346
6.316
-0.712
-8.573
1.112
-1.347
-8.442
-1.315
6.683
-8.987
-1.248
P^MOTi^M
-1.470
-0.873
-0.687
-0.480
1.143
1.407
-1.415
-0.476
-8.934
1.461
0.583
-8.448
0.500
-8.926
-8.696
-8.521
-1.238
0.418
0.161
-8.527
-8.681
8.115
-1.488
-8.644
-1.148
8.356
-1.582
-8.755
mummm^m**
-1.148
-8.943
-8.624
-6.462
8.878
8.885
-1.148
-1.688
-1.235
1.126
6.962
-8.329
6.563
-8.846
-8.987
-8.583
-1.667
8.116
8.173
-8.798
-8.347
1.115
-1.115
-8.177
-1.866
-8.121
-8.881
-8.911
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52G15NW93aa 3.15138 S IXMILE LAKE
ntario 900
Geoscience Approvals section 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.15138 Transaction #: W9330.00037
Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines
January 4, 1994
Mining Recorder Ministry of Northern Development and Mines Queen and Fourth P.O. Box 3000 Sioux Lookout, Ontario POT 1C6
Dear Madam:
RE: APPROVAL OF ASSESSMENT WORK ON MINING CLAIMS PA 611504 ET AL. IN THE SIX MILE LAKE AREA.
The Assessment Credits for GEOLOGY and GEOPHYSICS, sections 12 and 14 of the Mining Act Regulations/ as listed on the above report of work/ have been approved as of DECEMBER 2 9, 1993.
Please indicate this approval on the claim record sheets.
If you have any questions please call Clive Stephenson at (705) 670-5856.
Yours sincerely
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
CDS/ls
cc: Resident GeologistSioux Lookout, Ontario
vXAssessment Files Office Toronto, Ontario
Ministry oft-f&rthern Developmentand Mines
Ontario
Report of Work Conducted After Recording Claim
Mining Act
Transaction NumberW9330. 00037
Personal Information collected on this form is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines. Fourth Floor, ^59 Cedar Street, Sudbury. Ontario, P3E 6A5, telephone (705) 670-7264. 2. 15138Instructions: - Please type or print and submit in duplicate.
- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining Recorder.
- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work Is assigned to, must accompany this form.
1326Recorded Holder(s)
L. Cunningham/Noranda Exploration Company, LimitedAddress c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1Mining Division Patricia
Dates Work From: Performed July 15, 1992
Township/AreaSix Mile Lake Area
Client No.123019/176208
Telephone No. (807) 623-4339
M or Q Plan No. G.2561
To: December 11,1 992
Work Performed (Check One Work Group Only)Work Group
X Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
Type -, ?*Geological, Time Domain EM, Mag Surveying and Linecutting ^ z ^
CUM^ ; (*EOJL - J&H - pflfr - oTfcfci? ^5O —o5- *"
^ ft /x,'/,,, o gg *R EOb 1 VED
AUG 3 1 1993
JvHNING LANDS BRANCH
* ' -5 fe Ow :oO m "i ?B -
Total Assessment Work Claimed on the Attached Statement of Costs S 29,372Note: The Minister may reject for assessment work credit all or parr of the assessment work submitted if the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name
Vytyl Exploration Services
Northwest Geophysics Ltd
Al Smith (Co-Author)
Reg Felix (Co-Author)
Address
1 529 Rankin St., Thunder Bay, Ont. P7E 522Box 3263, Thunder Bay, Ont. P7B 5E8
c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1
c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1(attach a schedule If necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder.
Date
Aug. 12/93Recorded Holder or Agent (Signature)
^*~*r~Certification of Work Report
l certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report is true.
Name and Address of Person Certifying
Cecilia M. Barrett, 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1Tetepone No.
(807) 623-4339
Date Certified By (Signature)
Aug.12/93
For Office Use OnlyTotal Value Cr. Recorded
4*
Date Recorded
13Deemed Approval Date
93 fDate Notice lor Amendments Sent
Ric-Md '"RECORDED.
AUG 13 1993
Receipt _
0241 (03/91)
rff
'3
[?
z cQ c"
Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (s) one of the following:
1. G Credits are to be cut back starting with the claim listed last, working backwards.2. D Credits are to be cut back equally over all claims contained in this report of work.3. O Credits are to be cut back as priorized on the attached appendix.
In the event that you have not specified your choice of priority, option one will be implemented.
Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.
Note 2: If work has been performed on patented or leased land, please complete the following:
l cenify that the recorded holder had a beneficial interest m the patented j Signature or leasod l and at the time the work was performed. j
Date
Drtails for Work Report ft 1326-GEOTECH Page 1
Work ^fcrtft for AjP^ing
Reserve
Claim Number (see note 2)
PA 0,611,504
PA 0,611,505
PA 0,611,506
PA 0,642,478
PA 0,642,479
PA 0,642,480
PA 0,642,481
PA 0,642,482
PA 0,642,974
PA 0,642,975
PA 0,642,976
PA 0,642,977
PA 0,642,978
PA 0,642,979
PA 0,642,980
PA 0,642,981
PA 0,642,982
PA 0,642,983
PA 0,642,984
PA 0,642,985
PA 0,642,986
PA 0,642,988
PA 0,642,989
PA 0,642,990
PA 0,642,991
PA 0,642,992
PA 0,642,993
PA 0,642,994
PA 0,642,995
PA 0,642,996
PA 0,642,997
PA 0,719,586
PA 0,719,587
PA 0,719,934
PA 0,719,935
PA 0,719,936
PA 0,719,937
PA 0,719,941
PA 1,195,805
ft OfClaim Units
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
4
•NORANDA
Value of Assesment Work Done
on this Claim
210.00
835.00
0.00
0.00
0.00
210.00
50.00
200.00
1,390.00
630.00
1,935.00
2,640.00
605.00
2,480.00
1,390.00
2,180.00
800.00
990.00
680.00
220.00
0.00
165.00
0.00
660.00
190.00
25.00
230.00
0.00
885.00
260.00
970.00
605.00
690.00
605.00
1,230.00
80.00
1,120.00
480.00
3,732.00
EXFLo:v~;o;i c900 Alloy l
Value Applied to this Claim
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
400.00
OMHANtf, Lif.'ilT ;rivO
ED
Value* Assigned from this Claim
435.00
990.00
230.00
1,535.00
1.450.00
'. * ~
5^?S
Onl,2 no(ft jj0 m
AA /yf " /^ iii /y) ,
Reserve:Uork to b* Claimed at
a Future Data
790.00
205.00
2,080.00
990.00
1,780.00
400.00
590.00
280.00
cu.
t^ 260.00
CO
to
3*
T?t-^ 485.00
———— — ** ———————————
570.00
605.00
690.00
605.00
1,230.00
80.00
1,120.00
480.00
3,732.00
^qfbr/^l/y n -7il 'Q l'
TV,,,,- rl-.r P P7B 6A1 f r* ? z .-, y;
Dfttal lit for Work Report f 1326-GEOTECH Page 2
Work AT" for AjQPing Reserve
Claim Number (see note 2)
39
Total Number of Claims
# of Claim Units
Value of Assesment work Done
on this Claim
Value Applied to this Claim
29,372.00 12.400.00
Total Value Work Total Value Done Work Applied
Values Assigned fro* this Claim
————————— .^ -z.
. .*. .-^-^^o0 3a— 5 53-J l-/l/) g1 S
Reserve:Uork to be Claimed at
a Future Date
to CO
b J
91CO* *
—
4,640.00 16,972.00
Total Assigned Total Reserve From
Credits you are claiming in this report may be cut back. In order to minimize the adverse affects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (x) one of the following:
1.[ l Credits are to be cut back starting with the claims listed last, working backwards.
2. j Credits are to be cut back equally over all claims contained in this report of work.
3. Credits are to be cut back as priorized on the attatched appendix.
A. x Credits are to be cut back starting with the claims that have reserve credits.
In the event that you have not specified your choice of priority, option one will be implemented.
Note 1: Exanples of beneficial Interest are unrecorded transfers, option payments, memorandum of agreements, etc.,with respect to the mining claims.
Note 2: If work has been performed on patented or leased land, please complete the following:
1 certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.
Signature Date
NORANDA EXPLORATION COMPANY, LIMITED X ^oJ Alloy Lirive
Thunder Bay, Ontario P7B 6AI
Ontario
Ministry ofNorthern Developmentand Mines
'e dueloppement du Nord
et des mines
Statement of Costs for Assessment CreditEitat des couts aux fins du credit devaluation
Mining Act/Lol sur les mines
Transaction No./N* de transaction
Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining cialm(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands. Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5. telephone (705) 670-7264.
Les renseignements personnels contenus dans la prosome formule sont recueillis en vertu de la Lol sur le* mine* et serviront a tenir a jour un registre des concessions minleres. Adresser toute quesiton sur la collece de cos renseignements au chef provincial des terrains mlniers, minister e du Developpement du Nord et des Mines. 159. rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/CoOts directs
Type
Wages Salalres
Contractor's and Consultant's FeesDrolts de ('entrepreneur •t d* I'expert- consell
Supplies Used Foumltures utlllsees
Equipment Rental Location de materiel
Description
Labour Main-d'oeuvreField Supervision Supervision sur le terrain
Type Unecutting
EM-57 tt Mag
Type Analytical
Type
Amount Montant
5,914
3,147
8,750
7,150
1,404
Total Direct Costs Total des couts directs
Totals Total global
9,061
-l ' . Jti .
15 900
1,404
-
26.365
2. Indirect Costs/CoOts Indlrects* * Note: When claiming Rehabilitation work Indirect costs are hot
allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en tant que travaux devaluation.
Type
Transportation Transport
Food snd Lodging Nourriture et hebergementMobilization and Demobilization Mobilisation tt demobilisation
DescriptionType
Ground
Accom. in field
Amount Montant
1,214
1,793
Sub Total of Indirect Costs Total partlel des couts Indlrects
Amount Allowable (not greater than 20H of Direct Costs) Montant admissible (n'excedsnt pas 20 H des coot* directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and Allowable devaluation Indirect coett) fToUI det coott dkeett
Totals Total global
1 r?14'1 : ' V - ^
. ,. . j -
1,793
3 007i
5,?73
29,372M Indirect! idmlMlMet
Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre pout rejeter tout ou une partie des travaux devaluation presentes.
Filing Discounts
1. Work filed within two years of completion is claimed at 1000A of the above Total Value of Assessment Credit.
2. Work filed three, (our or five years after completion is claimed at 50"Vb of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
3? f*z gRemises pour dep6t
1. Les travaux deposes dans les gqu^ans suivanW*ir achevement sont rembourses a 100 "to de la valeur totaTBs&mentionnee du credit d'evaluation.
P"J **~" i ' ^m
2. Les travaux deposes trois, quatteJxiQnq ans agres leur achevement sont rembourses a 50 Va de 2 val^tif totale^ credit d'evaluationsusmentionne. Voir les calcuScl-dajQous. .-~Z^ 30
Valeur totale du credit d'evaluation x 0,50 .
Evaluation totale demandee
Certification Verifying Statement of Costs
l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
'
to make this certification
Attestation de I'etat des couts
J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux d'evaluation sur les terrains indiqu6s dans la formule de rapport de travail ci-joint
Et qu'^ titre de je suis autoris6__________________(titulaire enregistre, representant, posts occupy dans la compagnie)
. faire cette attestation.
i Signature
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fc 40os CUNNINGHAMMAGNETIC SURVEY
5 TOTAL REIDPROJECT : CUNNINGHAM NUMBER : 1326
BASELINE AZIMUTH : 90 deg' \- .... - ^ . . ^— . ... . ., .. . .- . . ,. .. ,. . -.. . . -
DATE : Oct. 92 NTS : 52 J/10\ S URVEY BY : Noranda Expin
FSLE : m26c'ur,n
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FigureS CUNNINGHAMMAGNETOMETER SURVEY
PROJECT: CUNNINGHAM PROJECT # : 1326 BASELINE AZIMUTH : 90 Deg.
SCALE = 1 t 2500 DATE : 10/ 7/92 SURVEY BY : NTS : 52
FILE: MI326CU NORANDA EXPLORATION
S2G15NW9388 2.15138 SIXMILE LAKE 230
