GEOL RPT ON BIGWATER PROP · 2017-01-17 · basalt Polarized light P132-93 Photo 21 - Photomicrograph, pillow basalt, boudind quartz veinlet. P132-93. Polarized light Photo 22- Bock

1-15*1 MJMW 010

Jt. 15461

GEOLOGICAL REPORT

ON

BI6WATER PKUPtKIY

MURPHY TOWNSHIP

TIMMINS AREA

January 1994 K. M. Gunnison

D. R. Pyke

Introduction

Present Survey

Previous Work

Regional Geology

Property Geology - Summary

Property Geology

Mofic Volcanics Komotiites Sedimentary Rocks

Structure

Geochemistry

Alteration, Mineralization and Mineral Chemistry

Microprobe Analyses - Mineral Chemistry

Recommendations

References

Map 1 - Geology Mop - in pocket at back .

Appendix A - Sample descriptions for 1903-84 and 1993 samples

Appendix B - Geochemical Analyses

List *f Ft Poge

Figure l. Figure 2. Figure3. Figure 4.

Figure 5a Figure 5b Figure 60 Figure 6b Figure 7o Figure 7b Figured Figure 9o Figure 9b Figure 10 Figure 11 Figure 12 Figure 13 Figure 14 Figure 15

Locotion hop-Property cloims. Claim Map——Locotion of conductors ond drill holes—— (previous work)Si02vsNo20*K20 - 1963-64 samples.. Si02 vs No20 * K26 - 1993 samples—. Si02vsK26 - 1983-64 samples. Si02vsK20 - 1993 samples—— Cation Plot - 1963-64 samples. Cation Plot - 1993 samples™Chondrite normalized REE plot (P 139-93). A1203vsTi02 - 1963-64 samples——— A1203vsTi02 - 1993 samples—————Mica microprobe data plot of Cr203 vs K20. Mica microprobe data plot of Ha20 vs K20- Mica microprobe data plot of BaO vs K20—Feldspar microprobe data plot of No20 vs CoO— Chlorite microprobe datsa plot of Cr203 vs FeO. Chlorite microprobe data plot of MnO vs FeO—

List of Tables

Table 1 Table 2 Table 3 Table 4 Tables Table 6 Table? Table 6

Summary of diamond drill hole log BW92-2— Description of microprobe samples analysed.Description of mica microprobe analyses. Mica microprobe analyses———————Description of Feldspor microprobe analyses. Feldspar microprobe analyses.Description of chlorite microprobe analyses.. Chlorite micr

List if Phatos Page

Photo 1 - Swamp tractor rood

Photo 2 - Pillowed ondesite-bosolt

Photo 3 - Variolitic pillow bosolt

Photo 4 - Voriolitic pillow basalt, (drill core)

PhotoS - Photomicrograph^ verioles. PI 16-93

Photo Go - Photomicrograph, variolitic pillow basalt P l-93.

Photo Gb - Some, polarized light

Photo 7o - Photomicrograph, matrix of ultramafic conglomerate. P10-93

Photo 7b - Some, polarized light

Photo 80 - Photomiuugmph, porphyroblastic biotite in pillow basalt P21-93

Photo 8b- Same, polarized light

Photo 9a - Photomicrograph, porphyroblastic biotite in basaltic komatiite. P274-64.

Photo 10 - Ultrvnofic closts in conglomerate/debris flow

Photo 11 - Ultrvnofic ond felsic clasts in cgl/debris flow

Photo 12 - Conglomerate/debris flow - heterolithic

Photo 13 - Close-up of photo 12

Photo 14 - Photomicromicgraph, porphyroblastic biotite in debris flow. P10-93.

Photo 15 - Graphitic argillite, drill core

Photo 16- Sheared debris flow

Photo 17o - Sheored komotiitic flows

Photo 18o - Photomicrograph, doric red spholerite from trench debris f low. Plone light P83-83

Photo lOb - Some, reflected lite

Photo 19o - Photomicrograph, weakly altered pillowed andesine basalt Plane light P139-93

Photo 19b - Some, polorized.

Photo 20 - Photomicrograph, strongly corbonotized pillow basalt Polarized light P132-93

Photo 21 - Photomicrograph, pillow basalt, boudind quartz veinlet. P132-93. Polarized light

Photo 22- Bock scatter electron image. P132-93

Photo 23- Back scatter electron image. P132-93

Photo 24 - Drill core ( Sample P135-93) from main alteration zone in Hole BW92-2.

Photo 25o - Photomicrograph, nrico-cartranote "regime". P134-93. Plane light

Photo 25b- Same, polorized light

Photo 26 - Photomicrograph, coarse groin corhonote-olbite- quartzvein. P135-93. Polorized light

Photo 27 - Photomicrograph, coarse groined, rBcrystollized carbonote-olbite vein. X-nicols. P135-93.

Photo 28 - Photomicrograph, quortz-albite-carbonate vein with sulphides. P137-93. X-nicols.

Photo 29o - Quertz-albite vein with 531 interstitial sulphides. Polorized light P137-93

Photo 29b- Some, plane light

Photo 29c- Some, reflected light

Photo 30 - Photomicrograph, Interstitial sulphides in quartz olite vein. P137-93. Reflected light

Photo 31 - Photomicrograph, Interstitial sulphides in quartz- olbiteveirt P137-93. Reflected light

Photo 32 - Photomicrograph^ blebs of pjplte and chalcopyrite in pyrrhotite, interstitial to quartz-olbite. P135-93. Reflected light

Photo 33 - Bock scatter electron image. P137-93

Photo 34 - Bock scatter electron image. P137-93.

Bigwater Lake Property - Horth Murphy Project

Introduction

The property, located 17 km north northeast of Timmins (Figure 1), consists of 44 contiguous claims which straddle part of the Murphy-Wort Township boundary (Figures 2 and 3). The claims comprising the propertyore os follows:

107319510731961073197107319810837501083751108375210837531083754108375510837561068294108829510882961088297111481311148201114621111497711149781114979

112770011277011127702112770411277051126039112604011260411126042112804311260441131376113137711152411115294111529511152961115297111529811152991156101

D. Pyke and K. Gunnison ore co-owners of the property.

The property is readily accessed via sand logging roods extending east from Highway 655 into the south port of the claim group. The turn-off from Highway 655 is 13.2 km north of the junction of Highway 101 and Hiyhwoy 655. The logging rood is driveable ta Just south af the claim

^X x

\ \*Kidd Creek Mine

LEGEND

claim block

poet and present gold producers

Figure 1Location of Murphy TownaMp proparty In relation to major ffauK-Hneamenta hi the north Hmnrtna area

faults (largely interpreted from airborne magnetics

Destor Porcupine fault

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^

\\

WARK TWP.

\

MURPHY TWP

Bigwoter Lake

K31376 l 1131377 ' 1088897 11088896__ i_ i _j-M p 1 p !p | p1188043 11188044 j 1088894 11088895

T ip - ,P1188048 j 1188040 j!083755 ' 1083756

i—.i—,L-.. IP JP1188041 pi 1083754 b083757 1115898

115899

.U14978 , lfc610i J1114880 j 1073198 (10731951^ J1114977 11115897

1 l____l______l____ l

n 'P ' P T 11115841II II NM*3C*I j1114881 .U14813.1073197 ,1073196 .1114979 l \ .1115896

I l l l i \ l-——i——i———i——-i__,--X-J__- p ip l i JP ,p \i1083751 1083750(1187700 Ill87703 11137704 1111539-4 11115895

II l i ' ' VIP"

l l l l 1083758 |1083753| 1187701 j 1187708 11187705l

Scale: 1:20.000

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boundanj; from there, e swamp tractor road (Photo 1) extends west to the OHR railvray which traverses the central portion of the claim group.

PresentField wort conducted over the period June 12 to September 23,1993

included cleaning out end re-establishing portions of old grid lines, prospecting, sampling and geological mapping.

The area was mapped at a scale of 15,000. Portions of the claim group had been previously mopped by Pjjce and Gunnison in 1983-84 when part of the property wes held by Comstete Resources Ltd. Detailed mopping was therefore largely conducted on those portions of the property not previously mopped or where the geology was least understood - notably the outcrop areas in Lot 4, Concession 6 of Nvpiiy Township.

The main objectives of the survey were to delineate the major structures and lithologies underlying the property and to outline areas of alteration and mineralization. As the property affords both o base metal and gold potential, particular attention was paid to the style of alteration and its relationship to the interpreted structural components.

A total of 64 bedrock samples were collected from the property. Sample descriptions ore given in Appendix A. Twenty-four thin sections and 2 polished thin sections were subsequently cut and examined in detail. Four polished thin sections were prepared for electron microprobe analysis of mica, feldspar, chlorite and carbonate mineral compositions. Whole rock major, trace and nre earth element analyses were carried out on four of the samples; in addition, 12 samples were analyzed for gold, copper and zinc.

Forty-five whole rock analyses submitted from the area in 1985 by Comstote Resources Ltd. for assessment work purposes were compiled in order to more fully define the geochemistry and alteration of the rocks underlying the property.

Ptioto 1. Swamp tmctor rood thnt leads to south pert of property. View

looking SW near south boundary of claim 1083753.

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Previous WorkThe oreo was first mopped by Derry (1939) as port of eight townships

comprising the Bigwater Lake area The geology of Murphy Township was subsequently compiled and updated by Ferguson (1964 and later formed part of a large scale reconnaissance by Bright and Hunt (1971). Recently, the Ontario Geological Survey completed on airborne magnetic and electromagnetic survey of the Timmins area, which included Murphy and Wark Townships (DBS, 1968).

The following summary of exploration work performed on the claims is based on information obtained from assessment files available from the Ministry of Northern Development ond Mines. Figure 4 summarizes the approximate location of known HLEM conductors ond drill holes.

In 1964, Texas 6ulf Sulphur Ltd drilled five holes totalling 54D m. Four holes in the south half of Lot 5, Cone 6 intersected largely felsic to intermediate volcanics with minor graphitic tuffs; one hole in the north half of Lot 4, Cone 5, was largely within sediments.

In 1964, National Explorations Limited conducted magnetic and VLEM surveys over the north half of Lot 4, Cone 6, Murphy Township, with no encouraging results.

In 1964, Conwest Exploration Limited conducted on airborne EM-magnetic survey in Murphy and Wark Townships; no follow-up work was undertaken on the present claim group-

In 1964, North American Rare Metals Limited conducted HLEMN, magnetic and seismic surveys in Lots 4 ond 5, Cone 1 t Wark Township. No conductors were located.

In 1964 Victoria Algoma Mineral Company Ltd diamond drilled two holes near the south half of Lot 4, Cone 6, and one in the north half of Lot 5, Cone 5, Murphy Township; aggregate length of holes totalled 408 m.

5OO lOOOMtre* JFigure 4Sketch showing location of HLEM conductors, previous diamond tiilUng and humus anomalies

Anomalous Zn/Au in humusAnomalous Zn in humusBodrock value at 77Oppm ZnHLEM conductor

Diamond drill holecpy - chalcopyrite

py - pyritepo - pyrrhotite

sph - sphalerite

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In 1969, Hollinger nines Limited conducted VLF and magnetic surveys in the south half of Lots 4,5 and 6, Cone 1, Work Township. Two diamond drill holes totalling 370 m were subsequently sunk in the south half of Lot 5, Cone 1. Hollinger also conducted geological mapping and VLF, HLEM and magnetic surveys in Lot 4, Cone 6, Murphy Township. In 1971, this was followed by one diamond drill hole totalling 153.6 m.

Norando Mines Limited held the north half of Lot 6, Cone 5, the south half of Lot 5, Cone 6, and the north half of Lot 4, Cone 5. During 1969 to 1971, magnetic and VLEM surveys were completed and followed by two diamond drill holes totalling 357 m in lots 5 and 6.

In 1981, Comstate Resources Ltd completed an airborne magnetic - INPUT survey of Work and Murphy Townships. From 1983 to 1988, Comstote performed ground exploration near the Wark/Murphy township common boundary. In 1963, a geochemical (humus) survey was carried out in Lots 4 and 5, Cone 1, Wark Township and Lot 4, Cone 6, Murphy Township. Magnetometer surveys were conducted in 1983-84 in Lot 4, Cone 5 (north half; Lot 5 Cone 6 (south half), and Lot 6, Cone 5. These were followed by magnetic surveys in Lots 4 and 5, Cone 1, Wart Township. Also, in 1983-84, Comstote geologically mapped parts of Lots 4,5 and 6, Cone 6, in Murphy Township and the south part of Lots 4 and 5, Cone 1, Wark Township. In 1988, on HLEM survey was conducted in Lot 6, Cone 5, and the north half of Lot 4, Cone 5, Murphy Township; no follow-up work was undertaken.

During 1988-90, the present property was aquired by the co-owners, and subsequently optioned to Noranda Exploration Company Limited in 1990. toronto carried out magnetic and H^M surveys, and subsequently sunk two diamond drill holes (BW92-1 and BW92-2; Figure 4) totalling 349 ra The option was terminated in 1992.

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Reqionel BeolopifThe volcanic package in north Murphy Township lies within what hos

been termed the Hoyle assemblage (Jackson and Fyon, 1991), which

consists largely of sedimentary rocks intercalated with lesser ultramafic,

mafic and felsic volcanics. The close spatial relationship between

komotiitic volcanics and rhyolite suggests a possible correlation with the

volcanic suite at the Kidd Creek Hine, 10 km to the northwest.

Property Geology - Summanj

The property is underlain by o complex assemblage of northeast

trending mafic volcanics, komotiitic flows and conglomeratic or debris

flow sedimentary rocks which has been folded about o northeast trending

anticlinal axis (Hop 1) Two major northwest, sinistral faults offset the

stratigraphy and appear to post-dote on earlier series of northeast

trending faults. Massive to foliated rhyolite outcrops immediately

northwest of the property. A band of graphitic argillite (interpreted from

airborne input conductors) occurs in the southern portion of the property,

intercalated with conglomerate/debris flows. Another northeast trending

graphitic argillite unit underlies the western portion of the claim group,

immediately east of the proposed northeast trending fault This unit wes

intersected in diamond drilling (DDH BW-92-2) and there is intercalated

with strongly altered mafic volcanics and komotiites.

Foliations and pillow elongation directions are almost entirely

northwest-southeast oriented, in marked contrast to the mopped northeast

striking lithologies. This may be due to pronounced northeast-southwest

compression, during which time northwest trending faults were - developed.

A 20-50 metre wide zone of fairly intense green

mica-cartramte-elbite-quartz alteration flanks the graphitic argillite

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neor the west central boundary of the property (intersected in ODH BW-92-2). This zone appears to extend into on outcrop oreo in Work Township, one kilometre to the northeast One to five percent pyrrhotite end pyrite occur within quortz-olbite veins within the zone.

Grab samples carrying anomalous copper and zinc values were obtained from o trench within the conglomerate/debris flows near the central part of the property. Sulphide bearing clasts within this unit may perhaps be of proximal derivation.

Property Seoloqu:

ftafic VolcanicsThe mafic volcanics are dominontly an assemblage of pillowed and

massive flows that are typically vesicular, weather light grey and are light grey green on fresh surfaces (Photo 2). Some of the pillowed facies are variolitic, with varioles being concentrated near the pillow margins and varying in size from 2 to 15 mm, (Photos 3-5).

The flows generally contain 5-201 sub-idioblastic to idioblastic aggregates of clinozoisite, 5-30* actinolite (as bladed to shredded, generally weakly to non-foliated masses), trace to locally 20* pale green chlorite, 20-40* anhedral (and clear) untwimed plagioclase, 10-20* interstitial fine grained quartz and traces of sphene, apatite and sulphides. Plagioclase generally occurs os fine grained, anhedral interlocking grains with quartz. Occasionally, however, the feldspars exhibit relict lath shapes and the optical continuity of the original twinning is retained. Carbonate occtrs os fine grained zenoblests and veinlets and constitutes three to locally twenty percent of the rock (Photos 60 and 6b).

Medium to coarse grained poikiloblastic biotite occurs occasionally (Photos 8o,b). Biotite is most strongly developed in the mafic flows

Photo 2. Pillowed, vesicular ondesitic bosolt in vicinity L25+50N-12E.

Photo 3. Variolitic pillow bosolt otL21N-1 It

Photo 4 Drill core sample P116-93 of variolitic pillow rim. Hole BW92-2,85nt

PhotoS. Photomicrograph of variolitic pillow basalt Sample P116-93, drill hole BW92-2,85 m. Variolitic texture. Circular variole has a rim of crystalline clinozoisite and core of fine plogioclase/quartz. Groundmass is anhedral plagioclose-quartz and pale green chlorite which elsewhere in slide appears to be retrograded of ter hornblende. Plane light, length of slide fs

3.6mm

c(

Photo 60. Photomicrograph voriolitic pillow basalt Sample P l -93, near L19+50N-12E. Photo illustrates the obindant development of clinozoisite and minor epidote common to many of the jnofic volcanics. The pale colored minerals are mainly carbonate with lesser quartz which largely forms diffuse vein material extending diagonally across the photo. This cartonate-quortz veining/alterotion appears to have caused retrognMting of the clinozoisite ond associoted plagioclase to minor chlorite (6-10 percent). Plane light; length of photo 2.3 mm.

Photo 6b. Same as 6a; polarized light. Note blue Interference color of

clinozoisite.

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Photo 7ft. Photomicrograph, Semple P120-93. Boudiragedquortz-cartonote veinlets rimmed by retrograde chlorite in surrounding groundmass of coarse clinozoisite-actinolite - oligoclose - quartz and chlorite. Polarized light, length of photo 0.6 mm.

Photo 7b. Some, Plane light

Photo 80. Photomicrograph of pillowed andesitic basalt Somple P-21-93

at L27N-13E. Porpharoblasts of biotite ovei yi owing

clinozoisite ond plagioclase. Plane light; length of photo 2.3 mm.

Photo 8b, Some; polarized light

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proxinrwl to the contact with the conglomerate on clolms 1003754 end

1063756.

Groundmess plogioclose compositions (os determined by microprobe onolysis) ore oligoclase-andesine. The occurrence of idioblostic clinozoisite, calcic feldspar and actinolite within the groundmass matrix indicate that the mafic volcanics attained a metamorphic grade of upper greenschist.

The mafic volcanics are generally moderately to strongly deformed and weakly carbonatized. Localized zones of shearing and carbonatization occur adjacent to lithologlcal contacts and in proximity ta faults. Quartz and quartz-carbonate veinlets, where developed in these zones, ore commonly boudinoged with letioyiadB chlorite occurring ot the margins of boudinoged lenses (Photos 7e,b). Chlorite occurs os fine grained, foliated,anastomosing bonds, and the percentage of amphibole and clinozoisite

* diminishes markedly.

On claims 1083757,1114977 and 1115241, clinozoisite is not os pervasively developed and the flows consist predominantly of soussuritized feldspar, actinolite, chlorite quartz and leucoxene.

Doric green, massive basalt forms a series of outrops south of the

pillowed volcanics near the south boundary of claim 1083756. In thin section, these rocks ore more mafic than the overlying pillowed volcanics, containing 40-45 percent actinolite. Geochemically, the massive basalts plot well within the tholeiitic field, whereas most of the flows exhibit o decidedly calc-alkalic signature (see section on Geochemistry). The unit is likely a sill, or perhaps a emulate base to a thick calc-alkalic flow, containing ilmenite.

Komatiites Komatiitic rocks weather light to dork grey, commonly display

polygonal jointing/polysuturing ond locally preserve fine relict spinifex

textures. Pervasive talc-carbonate alteration is common to many of the

outcrops. In a few of the thin sections examined, textures of serpentine

pseudomorphing cumulate textured olivine was preserved. One thin section

(P274-84) of basaltic komatiite in Wark Township, consists of tremolite,

talc, chlorite, saussuritized plagioclase, quartz, carbonate and minor chrome spinel ond magnetite. Two to three percent poikiloblastic brown biotite occurs in many of the samples examined, overgrowing o matted

groundmass of tremolite-tolc-chlorite-zaisite (Photos 9a,b).

Sedimentary RocksSediments underlying the property consist largely of heterolithic

conglomerate, herein interpreted to be coarse, unsorted debris flows. These units mag contain dominontly komatiitic clasts within an ultramafic matrix (Photos 10,11), or may contain a very varied assortment of clasts (eg. komatiitic, gabbro, felsic, clastic, chert and sulphide) within

an ultramafic matrix (Photos 12,13). The debris flows are invariably

poorly sorted ond clast supported, with clast size varying from several mfllemeters to two meters or more, but generally averaging 10 to 30 cm.

Talc-carbonate alteration of the rock is common, particularly when the ultramafic component is significant. Coarse grained, inclusion-rich, poikiloblastic biotite commonly occurs within the matrix to the clasts, overgrowing felty talc-tremolite-carbonate-quartz mats (Photo 14).

On claims 1073197 and 1073193, in the southwest portion of the property, the debris flows immediately north of (overlying) the komotiitic unit consist almost entirely of komotiitic fragments within an ultramafic matrix, suggesting a very local derivation from the underlying komatiites.

Basaltic fragments become noticoble only higher up in the sequence; in the vicinity of TL10E-1550N, basaltic clasts dominate.

Photo 9o. Photomicrograph of bosoltic komatiite. Sample P-274-84, Werk

Township. Porphyroblosts of biotite overgrowing talc

(colorless), tremolite, sousstrite and plagioclase. Length of

photo 23 mm

Photo 9b. Some; polarized light.

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o

Photo 10. Ultramafic conglomerate/debris now consisting wholly of

ultramafic fragments in on ultramafic matrix. Fine spinifex texture common to lorge clast in centre of phota thitcropat

L28+50N-11L

Photo 11. Ultramafic conglomerate/debris flow forming outcrop beside railway track at L19*50H-7*75E. Large ultramafic clast (under pick axe) partially replaced by buff carbonata Moderate shearing near pick handle. Numerous felsic and basaltic clasts near top of photo.

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Photo 12. Conglomerate/debris flow at TL10E-15*70N, containingnumerous white weathering felsic volcanic fragments within a

strongly foliated matrix of largely finer mafic and ultramafic clasts.

Photo 13. Close-up of port of Photo 11, showing felsic, ultramafic, mafic

and some rusty sulphide bearing clasts. Pencil tip points to

spinifex clast.

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o

Photo 14 Photumici oymih of inclusion-rich poikiloblastic biotiteovergrowing the tolc-tremollte-cartmnote-quortz matrix in conglomerote. Sample P10-93 from railway cut in central portion of property.

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Hossive, thickly bedded, fine to medium grained, medium grey weathering greywacke outcrops near the Warfc-Murphy township boundary. Minor interbeds of siltstone, up to 5 cm in width, rarely form more than four to five beds within on outcrop area. Biotite generally comprises 5-101 of the rock. Primary structures observed include graded bedding, scouring. Home structures and soft sediment slumps. Flame structures indicate north tops near the Wark-Hurphy Township boundary.

A northeast trending unit of graphitic argillite was intersected in DON BW-92-2 an claim 1112041. The rock is generally finely bedded and fine grained, with less than 20* greywacke component (Photo 15). Light grey to white millemeter wide bonds of chert or cherty siltstone occur, and commonly display of f sets and boudinage structures. Nodular pyrite-pyrrhotite is locally present within specific beds; quartz pressure shadows ore ubiquitous at the margins of the deformed nodules. Minor flecks of dork brown-red sphalerite were observed within the unit in the vicinity of more sulphide-rich bands.

StructureThe structure of the property is poorly understood and there remain a

number of factors which, as get, are not adequately explained.At present, the main structure is interpreted to be o northeast trending

anticline, disrupted by northwest cross faulting. A pervasive foliation strikes northwest and dips steeply northeast Pillows also strike northwest, and where taps could be determined with some confidence, the facings ore WSW. It was first thought that perhaps the discrepancy in the trend of the stratigraphy with the facings of the pillowed flows may signify on unconformity along the south contact of the komotiites just north of the pillow determinations ie. - on claims 1083754 and 1083/57 in the northeast part of property and similarity through claims 1083750,

Photo 15. Drill core sample of grophitic argillite showing boudind quortz

(chert?) bonds with pressure bonds. DDH - BW92-2.

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1127700,1127703 ond 1114979 in the southern port of the property. However, this does not appear to conform with either the ground or airborne geophysics, or the apparent continuity of conglomerite units within the southerly basalts. Therefore, a fold axis is proposed, whereby the NW striking - SW facing pillows ore outcropping at the nose of the fold. This onticlinol axis is supported by the morphology of the flows in diamond drill hole BW92-1, on cloim 1114813, which indicate that tops ore down hole ie.- to the northwest As well, the strong oirborne conductor (OGS, 1988) at the south margin of the property is interpreted to be o graphitic argillite, correlative with the graphitic argillite intersected in diamond drill hole BW92-2, on cloim 1112041. At present, this interpretation, although not wholly satisfactory, appears to be the most viable.

Two northwest trending faults cross the property, as indicated by offsets in the stratigraphy and locally intense shearing, particularly evident in some rode exposures along the roilwoy trade (Photo 16 and 17). A northeast trending fault is interpreted to extend roughly parallel to the graphitic orgillite/conductive zone in the west port of the property. This is supported both by shearing noted within the graphitic argillite and by the occurrence of strongly deformed, green mica altered and quartz albite veined rocks intersected in Nonndo DDK BW-92-2, and from previous diomond drill logs noting shearing ond alteration along this some zone (Figure 4). Regional aeromagnetic data (Barlow, 1988) supports the presence of this fault, which extends southwest to the Mattagami River fault in Godfrey Township and northeast through the northwest portion of Gowon Township. Weak, subporallel HLEM conductors on the eastside of the property (Figure 4 and flap D which are transverse to the stratigraphy may reflect overburden conductors along related fault scarps.

Photo 16. Sheared ultramafic conglomerate/debris flow in outcrop beside

railway track at L16N-11+70E.

Photo 17. Sheared komotiitic flows with numerous vetnlets of buff

cartMNWte parallel to shearing. Outcrop along side railway track

nearTLIOE-19+SON.

l00

C

(

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Whole rock and trace element analyses were determined for four of the samples collected from the property during the 1993 field season

(samples PI, P105, P107, P139-93). In addition, rare earth elements were

determined far sample P139 and a further twelve samples were assayed

for gold, copper and zinc. The samples were analyzed at X-Ray Assay Laboratories Ltd. in Willowdale, Ont

Forty-five lithogeochemical analyses obtained during 1983-84, and

submitted by Comstate Resources for assessment purposes, were compiled in order to more fully define the geochemistry and alteration of the rocks

underlying the property. Sample descriptions for both the 1993 and compiled 1983-84 specimens are given in Appendix A; the geochemical

data are presented in Appendix EThe volcanic racks underlying the property ore subalkaline (Figs. 5a,5b),

dominantly low-K andesite*, basaltic andesites and basalts (Figs. 6a,6b). The Jensen cation plot (Figs. 7a,b) readily breaks out the two main volcanic suites observed: 1) a calc-alkaline sequence varying in composition from basaltic through rhyolitic and 2) an ultramafic -mafic

komotiitic suite. Only minor tholeiites are present, occurring as a narrow band of dork green, massive flows (sills?) in the northeast part of the property (samples P261,262).

A chondrite normalized plot of the rare earth element (REE) abundances (Fig 8) in a sample of pillowed andesite (P 139-93) from diamond drill hole

BW92-2 confirms the calc-alkaline affinity of the mafic to intermediate volcanics (Condie, 1984. The REE pattern exhibits generally moderately

elevated abundances, a moderately negative slope and a weak negative

europium anomaly.The intercalation of dominantly komotiitic and calc-alkaline volcanics

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trli elM

t

AC03

g g

Jensen CATION PLOT, Murpfy 1993 SAM Cation*Jenten 1976 (fig 1)

FeO'*Ti02

AI203

Koaatlitti

BM

iltiU

Mlv

t

variolitic Pt-tholilit*

i Nlil? V

:::i-i:,

utrii

clijt

A•T O

T—l l Mill————l——l—l l l l ll|————l——l—l l l l II

La

Ce

Nd

Sm

Eu

Tb

Yb

Lu

i iii i i i l____i i i i i i i 11

O 33

tsJD O O

e

S

FIGURE 8 O K.O

-l

"x

underlying the property is unusual for the Timmins area north of the Porcupine-Destor Fault. The volcanic stratigraphy within the Timmins gold camp, as well as that occurring within the Kidd Creek and Kamiskotia VMS base metal deposit areas, is characterized by tholeiitic or tholeiitic-komotiitic geochemical signatures.

During the course of the mopping it appeared that many of the clasts in the conglomerate/debris flow (mop unit 4) were locally derived. For example, on claims 1073197 and 1073196 in the SW part of the property, the debris flows immediately north (overlying) the ultramafics consist of ultramafic fragments in an ultramafic matrix, suggesting a derivation fnrni the underlying ultramafics. Basaltic fragments only become noticable higher (north) in the sequence and in the vicinity of TL10E-15 SON, basaltic clasts dominate. Platted values of A1203 vs. Ti02 onhdrous weight percents for all samples are shown in Figure 9. The plot suggests that basaltic closts (P75 and POO) occurring within the conglomerate/debris flows ore not derived from the flows underlying the property area - the clast compositions do not plot on the some geochemical trend as the boselt-andesite flows. Whether the conglomerate/debris flow clasts are locally derived or ore from a distal source raises many implications os to the tectonics surrounding the emplacement of the fragmental. The conglomerate was initially envisaged as a fault scarp - talus slope type deposit However, if the fragments ara not locally derived, then either a turbidite-type deposit or possible fault emplacement is suggested. A more detailed study of the clast types, sedimentological structures and fabric occurring within the conglomerate/debris flow units is warranted, and may well have o bearing on the economic potential of the area of the area (ie. - the Interpreted tectonic setting).

S NO V

O t

l**) 91

ffidn SLd

l B -

9dB

'

*OZ

d*

O

19&U

9

l1 2l P-

00 e

r J

9' Z' 100000

8'

L0000

06'

l

TO2

—* ro

OGL*

O ro

iCO

S:

ens

a,2

FIGURE 9b

-50-

Alteration. Mineralization and Mineral Chemistry

Grab samples containing anomalous copper and zinc values were obtained from a 75 meter long, partially water filled east-west trending trenched area occurring near the central part of the property, immediately west of the railway (Mop 1). The trench occurs within the conglomerate/debris flow. Here, clast types are more commonly felsic to intermediate in composition and bear two to locally twenty percent extremely fine disseminated pyntwtite and pyrite.

Samples P78 and 83-93 were obtained from o large, ovei grown rock dump pile/area occurring immediately south of the trench. Sample P-81 returned assay values of 252 ppm copper and 1090 ppm zinc, and sample P82 assayed 273 and 093 ppm copper and zinc, respectively. Sample P79 returned a value of 22 ppb gold.

In sample PB2-93, medium to coarse grained anhedral, dark red sphalerite is intergrawn with abundant (5-10 percent) subheAnl pyrrhotite bands and trace chalcopyrite in o foliated corbonate-chlorite-clinozoisite matrix (Photos. 18a,1Bb).

A thirty to fifty meter wide zone of moderate to locally intense green mico-carbenate alteration (with associated quartz-carbonate-albite veirring and shearing) was intersected in Nonmdo diamond drill hole BW92-2, near the west central boundary of the property (Mop l). Thiszone con be traced northwards into on outcrop area occurring one kilometer to the northeast, in Work Township. A major northeast trending fault is interpreted to parallel closely the alteration zone (see Structural Geology section).

A brief summary of the diamond drill log for hold BW-92-2 is given in Table 1. The alteration and veining are hosted within mafic to intermediate pillowed volcanics, and occur on either side of o band of graphitic metasediments (Photo. 15). A seventeen meter wide section of

Photo 18a Photomicrograph, sample P62-93. Coarse to medium grained anhedral dark red sphalerite intergrown with subhedral pyrrhotite bands and truce chalcopyrite in a foliated carbonate-chlorlte-clinozoisite matrix. Plane; length of photo 3.6 mm.

Photo lOb. Same, reflected light.

))

TABLE1

0-13 m

13.0-56.2 m

58.2-127.0 m

63.0-127.0 m

127.0-163.1

163.1-180.0

163.1-180.0

180.0-185.0

Summany of Log for DDH BW92-2

Cosing

Spinifex textured komatiite, locally strongly serpentinized. Minor quartz-magnetite veining.

Pillowed mafic to intermediate volcanic

moderate to locally strong alteration zone. Patchy. diffuse development of green mica-carbonate alteration zones throughout 6-10 percent narrow Quartz-albite-carbonate veiirinq.

Locally sheared graphitic argillite

Pillowed mafic to ultramafic volcanic

Major alteration zone with 70 percent ouartz-albite-carbonate veining and moderat strong green mica- carbonate alteration of wallrock. 1-4 percent combined pyrrhotite - oyite and sphalerite in veins.

Komatiite? - highly cartranatized and foliated. Minor quartz-carbonate veining.

185.0 END OF HOLE

highly altered ond f olioted rock, bearing 70* quortz-carbenate-albite

veins to 0.4 meters in width, occurs within the zone near the bottom of

the drill hole (ie. from 163.1-100 metres).

Six thin sections ond two polished sections were prepared from

representative samples taken across the zone. In addition, mineral

compositions were determined on f our carbon coated polished sections

using the JEQL JAX-0600 Electron Microprobe at the University of Western

Ontario. The minerals analyzed include white micas, feldspars, chlorite

ond carbonate; f oir spectrometers were employed ond the unit was run

with an excitation voltoge of 15 kv. Descriptions of the microprobe

samples analyzed ore given in Table 2.

Where the volcanics are least altered, they ore fine grained, hard and

pale grey in colour. The mineralogy consists of clinozoisite,

oligoclose-andesine feldspar, actinolite, quartz, lesser chlorite, calcite

ond traces of sphene and rutile (Photos. 19o,19b).

As alteration becomes more intense, carbonate modal percentages

increase considerably (Photo 20). The rock takes on a distinct emerald

green hue due to the presence of varying proportions of pole green mica.

Mica generally occurs as fine to medium groined foliated mosses

interstitial to quartz, carbonate and feldspar, and varies from five to

locally twenty-five percent (Photo 22). Clinozoisite becomes

progressively replaced by carbonate, quartz and mica (Photo 23). Quartz

veinlets are often recrystallized and boudinoged, with abundant coarser

grained mica developed at their margins and in later cross-cutting

fractures (Photo. 21).

Photograph 24, of drill core from the zone, well illustrates the style of

alteration ond veining observed. Green mica alteration displays a very

patchy distribution, even where veining is intense (lower portion of photo).

Distinct "regimes" of green mica-carbonate alteration occur within less

-55-

TABLE2

Description of rticroprobe Samples Analysed from Main Alteration Zone DOH BW92-2

P 132-93 (ot

Green mice-carbonote altered volcanic. Fine grained, strongly foliated with common quartz-colcite veinlets. One percent fine disseminated sulphides and rutile. Alteration is moderate.

PI34-93(at 120.2m)

Pillowed volcanic exhibiting patchy and diffuse green mica- carbonate alteration. Green mica-carbonate "regimes" often exhibit coarse

foliated mica at their boundaries.

P155-93 (at 96.2 m)

Doric grey-white "chicken-feed" textural cerbonate-quartz-albite vein. Vein margins bear abundant foliated fine green mica and bonds of dork green chlorite.

P137-93(at 167.2m)

Quartz-albite vein with coarse mica, sulphides and chlorite interstitial to main grains. Wallrock margins ara highly foliated and sericitized. Minor ankerite in veins

Photo 19o Photomicrograph, sample P139-93. Weakly altered pillowed

ondesitic basalt, containing 51 clinozoisite,

oligoclose-andesine feldspar, actinolite, quartz and lesser

chlorite, calcite and traces sphene, rutile. From drill hole

BW92-2,87m. Plane light, length of photo is Z3 mm.

Photo 19b Same. Note anomalous blue birefringence of clinozoisite.

Photo 20. Photomicrograph, sample P132-93. Strongly carbonatizedpillow basalt containing abundant carbonate, fine grain shreddy mica and interstitial quartz, feldspar and rutile. Polarized light, length of photo is 3.6 mm

Photo 21 Photomicrograph, sample P132-93. Boudinaged and recnptollized quartz veinlets with coarse grain mica developed at vein selvages. Mica also occupies cross-cutting micro shears. Polarized light, length of photo 3.6 mm

-59-

O

Photo 22 Dack scatter electron image, sample P132-93. Highly altered basalt Central bright chlorite grains intergrown with feldspar (medium grey), anhedral quartz (darlcer grey), anhedral carbonate (very light grey) and medium grey shreddy foliated mica (5-101). Note carbonate pressure shadows on albite groin.

Photo 23 Dock scatter electron image, sample P132-93. Shows original clinozoisite grains being progressively overgrown/replaced by mica-quartz and carbonate. One percent disseminated sulphides.

-61-

Photo 24 Drill core (semple P135-93) from main olterotion zone in hole

DW92-2 (semple ot 96 m). Illustrotes style of alteration end

veining commonly observed throughout the zone. Note the

distribution of green mico-corbonate and f eldspor-chlorite

regimes. -

))

l Os

-64-

altered "regimes" containing feldspor-chlorite-quortz and only minor amounts of mica and carbonate. Regime boundaries vary from very sharp to rapid gradotionol (Photos. 25a,25b); minor bonds af coarse mica ore eccessiemrily developed at these interfaces.

Veins are commonly compositionolly zoned (Photo. 24). They often display a granular tortured, greyish coloured outer border of medium to coarse grained ferroan dolomite-minor quortz-albite (uppermost portion of core in Photo 24; Photos. 26 and 27), and a central zone of quortz-albite with miner ferroan dolomite. Central quortz-albite veins are characterized by a pronounced ribbon fabric, expressed by irregular 1-4 mm. wide seams af foliated emerald green mica wall rock occumng within the veins, parallel to the vein walls. These seams are believed to reflect the periodic dilotent opening af the veins under conditions of high fluid pressure (Romseg and Huber, 1963).

Vein quartz and albite are commonly 0.2-3.0 mm crystals showing ubiquitous defarmatianal textures such as undulase extinction, suberain boundaries and bent twin planes. Coarse grained laths of vein mica commonly occur interstf tel to quartz and albite (Phota 28). One ta locally 4-5X sulphides occur as sinuous interstitial aggregates in the veins (Photos 29o, 29b, 29c). Sulphide mineralogy is largely pyrrhotite and pyrite with minor sphalerite, chalcopyrite avid galena (Photos. 30,31). An unidentified opaque mineral, brown in reflected light with a pronounced 90 degree cleavage, also occurs in minor amounts within the veins (Photo.31), intergrown with pyrrhotite and pyrite. Fine blebs af chalcopyrite and pyrite commonly occur within more massive anhedral pyrrhatite (Phota32).

Micranroha Analyses - Mineral Chemistn)Descriptions of mica microprobe analyses are given in Table 3 and the

analytical results are presented in Table 4. The micas were found to be

Phot o 25o Photomicrograph, semple P134-93. Displays subtle, rapid

gradotionol boundary occurring betwreen mica-carbonate

"regime" (upper left corner) and coarse grained

f eldspor-chlorite "regime (lower right).

Photo 25b Same, X-nicols

-66-

C

C

Photo 26 Photomicrograph, sample P135-93. Coarse grained f erroan dolomite-olbite-quortz vein (upper portion of photo) bordered by fine grained strongly foliated mica-carbonote-quartz- feldspar wall rode. Polarized light, length of photo 3.6 mm

Photo 27 Photomicrograph, sample P135-93. Coarse grained, partially recnjstallized ferroan dolomite-olbite vein. Note extremely fine groined f olioted mica (light) and dark crenuloted chlorite bonds at vein margin.

\CO

C

C

Photo 28 Photomicrograph, sample P137-93. Quartz-aHrite-carbonate

vein containing coarse grained interstitial vein mica and 5S sinuous

interstitial sulphide growths. Brains commonly exhibit undulose

extinction, lobate to subgrained boundories and local granulated textures.

Sulphides are pyrrhotite and pyrite: pyrrhotite contains minor blebs of

chalcopyrite and sphalerite. X-nicols, length of photo 3.6 mm.

Photo 29o Photomicrograph, sample P137-93. Deformed quartz-albite

vein containing 5X of sinuous interstitial aggregates of

sulphide. Sulphide mineralization is largely pyrrhotite and

pyrite with minor sphalerite, chalcopyrite and galena:

Polarized light, length of photo 3.6 mm.

1 o

Photo 29b Some, plane light. Note sinuous interstitiol aggregate textures of sulphides.

Photo 29c Some, reflected light

-ZL-

Photo 30 Photomicrograph, sample P137-93. interstitial sulphides in

quortz-olbite vein. Vein sulphides ore largely pyrrhotite (very

pole yellow), pyrite (darker yellow) and minor pole grey

sphalerite at margins of sulphide groins. Reflected light,

length of photo 0.6 mm.

Photo 31 Photomicrograph, sample P137-93. Interstitial sulphides in

quortz-olbite vein. Vein sulphides are pyrrhotite (light yellow),

pyrite (darker yellow), sphalerite (pole grey). An unidenified

opaque mineral, brown in reflected light with o pronounced 90

degree cleavage developed, occurs in minor amounts intergrown

with pyrrhotite and pyrite. Reflected light, length of photo 0.6

mm.

Photo 32 Photomicrograph, sample P135-93. Shows fine anhedral blebs

of pyrite (light bright yellow) end cholcopyrite (strong yellow)

in more massive brownish yellow pyrrhotite interstitial to

coarse grain quartz- albite in central vein. Reflected light,

length of photo 0.6 mm.

)

i â Os

-77-

remarkably chrome poor, considering the emerald green colour of the

mica-carbonate alteration observed. The highest chrome values observed

were less than 0.5 wt X Cr203 (Figure 10), considerably less than the 1-4

wt X Cr203 values generally displayed by fuchsitic micas. The green

colour of micas observed in hand specimen may perhaps be due, therefore,

to elevated contents of barium or vanadium. Unfortunately, vanadium was

not analyzed in these samples; however, barium contents were

consistently found to be anomalously high. Even fine groundmass micas

were found to contain up to 1 wtX Bad (Figure 12).

Doth vein and groundmass micas are very weakly to weakly paragonite

in composition (Figure 11). Na20 content in micas analyzed is generally

less than 2.5 weight percent

Dackscatter electron images of coarse hydrothermal mica grains within

quartz-albite veins show complex zoning (Photos. 33,34) and contain much

higher boriun contents than do the surrounding groundmass micas (Figure

12). Analyses of vein mica from a quartz-albite vein (sample P137, Photo

34) yielded DaO weight percent values as high as 1.5-2 wt X. Vein forming

hydrothermal fluids were therefore enriched in barium; the complex zoning

observed likely indicated occassional fluctuations in fluid composition. It

is interesting to note that the Hemlo gold deposits, located near

Marathon, Ontario contain similarly zoned and barium-rich hydrothermal

micas.

Descriptions of feldspar microprobe analyses are given in Table 5 and

the analytical results are presented in Table 6 and Figure 13. The data

clearly indicate that groundmass phase feldspars are andesine-oligoclase

in composition and are therefore likely of upper greenschist metamorphic

origin. In contrast, coarse feldspars within the hydrothermal

quortz*feldspar-carbonate veins are almost pure albite in composition,

strongly suggesting that sodium was highly mobile during vein formation.

TAB

LE

3 PC

SCft/

PTJO

N Of

MIC

A M

ICfl

QP

RO

BS

AN

ALY

SE

S

BIQ

WA

TER

PR

OP

ER

TY, M

UR

PH

Y T

OW

NS

HIP

ANAL

YSIS

SA

MPL

E AN

ALYS

IS D

ESCR

IPTI

ON

1 a 3 4 B 0 7 a 9 10 11 13 13 14 IB 10 17 16 10 20 21 32 23 24 26 26 27 26 20 30 31 32 33 34 36

138

134

134

1U4

134

134

134

134

liM 134

134

134

137

137

137

137

137

137

137

137

137

137

137

137

137

137

137

137

137

137

132

132

132

131

132

mlo

i al o

irtao

nale

vain

talva

gafei

. coa

rse

mlea

al a

JbJle

*gre

en m

loa lo

na im

trlae

alo

t. eo

art*

mie

* al

alta

)* g

i**o

mle

a io

n* m

lw f w

:*tot

eoa

ria m

iea a

l alb

iit-g

raan

mica

ion*

iiiiw

faoa

(ma

grain

ad m

toa m

albi

te ra

na(m

a gr

ainad

mtoa

In a

lbite

xena

dna

griin

ed m

toa

in a

lbite

lena

ooar

ta m

toa In

gra

an m

ea to

neoo

ari*

mica

gia

m m

gia

an m

ea to

namt

oa tn

iaraU

uaJ l

e alb

ita In

gre

en m

oa lo

nelin

e gr

eund

maa

e mt

oa In

gre

en m

toa to

nefin

e gro

undm

aaa

mto

a In

gra

an m

toa

ion*

oear

to m

toa in

qu*

itt-W

*p*i

vain

eoaf

ta m

ea m

que

rti-te

ldip

ar v

ainda

rkar

ean

lral lo

ne in

eea

rae

qli-M

dtpa

r vain

mtoa

Mghla

r rim

on

tarn

* mtoa

gra

inMt

o. Pt

ol, i

. dar

k eor

a to

ne m

Inte

rn. q

ti-fti

oV v

ain m

toaMi

e. Pu

t. i.

light

er m

Mdt

o oo

io e

l aam

a gr

ainMt

o. Pu

t. i,

dark

er e

ulerm

eal lo

ne o

feam

e gr

ainMt

o. Pt

ol.

, ipot

A. t

oned

vein

mtoa

, dar

kar e

ora

el g

rain

Mie.

Ptol.

. s

pel 8

. len

ad va

in mt

oa, d

arke

r eer

a el

gra

inMi

e. Pt

ot.

, ape

t C. l

oned

vein

mtoa

, mar

gin o

l dar

kar O

OF*

Mie.

Ptot.

, i

pei 0

, ligh

ter m

ldoJe

ion*

el la

me

grain

Mto.

Plot.

, s

pot E

. ligh

ter m

Wdle

zon

e of

fam

e gr

ainMi

e Pt

ol.

. ipet

f, li

ghte

r mld

dl* i

on*

ef aa

ma g

rain

Mlo.

Ptol.

, t

pet Q

. eule

r mar

gin o

f llgh

tar m

idela

tone

Mto.

Ptol.

. s

pot H

. dar

k ou

ter r

im e

l mtoa

gra

inM

lo. P

tol.

. spo

t 1. d

ark

eule

r rim

et m

lea g

rain

Mie.

Ptot

, too

t J. d

irh e

uler r

im e

l mlea

gra

inMl

o. Pt

ol, 2

, ipo

t J-t.

dar

k mt

oa g

rain

ad)a

eant

to le

nad

moa

grou

ndm

att m

lea In

gra

an m

loa*b

*arln

g re

ekMt

o Pt

ol. S

. tot

aled

gre

undm

aH m

toa w

ithin

albitto

-gre

en m

na lo

nemt

oa g

rain

with

in gi

ound

mai

e el

albi

te-g

roen

mtoa

moa

gra

in wi

lhm g

reun

dmaH

el a

lbila-

grae

n m

leamt

oa g

rain

with

in gio

undm

aeo

ef a

lblie-

grae

n mt

oa

00 l

-79-

8 w — — bobdobdooooooobodddbooo

2 ^^222*5^^22*222^22^5

a

- iMl kw o

ls S 8 ** tsg

p

i

0 adbdbddobdbbbd—' — d — dddd—~~ — — dddddbdbd

S 885852Si8S9^988888888888888888858p88O ddbbd~ddd — ddoddddbddddobdbbddddobbo

t A v d tt ^ tt ^T ^ 9 ^ 9 ^ tt M M in A ^ ^ ^ 9 A tt ^ a 9 ^ 9 fi X ^ ^ X fl A^ A A ^ tt A ^ ^ A ^ A ^ A ^ Y A A A A ^ tt A M A A A ^ A A A ^ ^ A O tt

w^Wci^ — ô— '•: —'ri — — — b—^bbb — — — •; ^ — ^ — ^—d — o

M. ^W--*-'--b---'--obbob-ddboobb* — bd---^-

9 8o8Sop888S8S88888888a55888o88388888S dddddddbobbdbbbdbbbbdbbdbddddbdbbbd

g ddodddbbbbbbboddoobbobodooddddbdbbb

^ ddddddddbddboddodddbdddbebdddddddoo

Jt Ali Aifc jfc A* jfc MB vv *A hJ B **i *i jtti aa Am ^h Alb Ait fc^ î AkT Am Am A& Am Ali AW Am AW m^ Am Am Am m^ ^ft

i

-80-

0.5-

MICA MICROPROBE DATA PLOT OF Cr2O3 vs. K2O

0.45-

0.4-

035-

O25-

O 01o

0.1-

0.05-

&00 7.00

CO0T90 ffllCfl flf

green mica regime i112

-35

Q12

.16

10•NIB -,anW -127

'-^f u8

33ci22

8.00 9.00 IQuOO

K2Owt%11.00 12.00

FIGURE 10

-81-

MICA MICROPROBE DATA PLOT OF Na2O vs. K2O

4.5

4-

as-

3-

2-

-11

1-

c-aoO5-

• 16

6.00 7.00 8.00 9.00 10.00 11.00 12.00

K2Owt%

FIGURE 11

Photo 33 Somple P137-93. Microprobe picture 1 (nice onolyses

17,18,19). Bock scotter electron image of complexly zoned

coarse rnico within quortz-albite veia Middle, brighter zone of

grain is enriched in borium (oil vein mico ore somewhat

enriched in barium). Mico is overgrowing albite (dart grey).

Photo 34 Bock scatter electron image. Microprobe picture *2. Somple

P137-93. Complexly zoned coarse vein mico in quortz-olbite

vein. Description of spot analyses A to J-1 are given in Tables

3 and the onolyses are presented in Table 4. Spot analyses D, E,

F ond G ore analyses of the barium enriched bright middle zone

of the mica grain. The dor* grey anhedral grains within the mica

ore albite.

)o

oo

u l

NDCA MICROPROBE DATA PLOT OF BaO vs. K2O

1.4-

1.2-

1-

CD

0.6H

0.4-

O2-

18

t;16

brigft mdUb

(-i23

026

013

31 030

012

r 6U2I-

-10

o 20

aoo 7.00 8.00 9.00

K2Owt*fc10X10 11.00

FIGURE 12

TABL

E 5

. MUR

PHY

TOWN

SHIP

ANAL

YSIS

NO.

SA

MPL

E AN

ALYS

IS D

ESCR

IPTI

ON

1 PI

34

olrolo

3, g

roun

dmttt

Mdi

par w

ithin

•Ibid

rtgl

mt

2 P1

34

elre

lt 3, g

roun

dmm

Mdf

lpw

withi

n al

bltt

rtglm

t)

P134

ol

rdt 3

, gro

undm

tM M

dipt

r with

in tJ

bttt

rtglm

t4

PI 34

ol

roli

l.ftW

iptr

withi

n gr

ttnm

tet r

tglm

t6

PI 34

ol

relt

1 . ftW

ipw

wltM

n grtt

n m

lot r

tglm

t6

PI 37

ee

mt t

wlnn

td M

dipi

r wHN

n qu

irtz-

Wdi

p*/ v

tln7

PI 37

flp

et K

, Mio.

Plet

urt 2

, Ino

hltlen

In it

ntd

mte

t8

P137

ftM

flpw

lnqu

tm-ta

ldflp

vvtln

9 PI

37

ftfdf

lptr

In qu

trtt-f

tldflp

vvtln

10

P 1 32

M

io. P

lot S

. ftld

flptr

evtrg

rew

n by

poU

dloblM

Ue tp

ldet

t11

P1

32

Mio.

Plot

S. f

tldtp

ar e

vtrgr

ewn

by p

elklle

WM

do tp

ldet

t

TABL

E 6

aiQ

WA

TE

R P

ftOPg

ftTY.

MU

RP

HY

TO

WN

SH

IP

ANAL

YSIS

NO.

SAM

PLE

8tO

2AQ

03Na

20K

20Ca

OB

*0TO

TAL

1 2 3 4 8 6 7 8 9 10 11

P134

P134

P134

P134

P134

PI 37

PI 37

P137

P137

P132

P132

63.76

62.62

62.84

62.2

683

.26

70.0

772

.16

70.6

470

.16

62.78

81.8

3

24.7

924.43

24.13

24.84

26.22

19.72

19.78

19.79

19.62

26.46

24.8

6

7.21

6.47

6.61

8.42

7.23

11.88

6.84

12.14

11.78

7.06

8.27

0.04

0.06

0.04

0.08

0.07

0.03

0.07

0.04

0.02

0.01

0.04

6.86

6.44

6.87

6.03

6.18

0.14

0.13

0.11

0.11

6.61

6.89

0.08

0.11

0.01

0.01

0.01

0.01

0.08

0.02

0.06

0.01

0.04

101.81

101.32

100.

88101.61

101.

96101.62

101.

0810

2.68

101.

6810

1.94

100.94

FELD

SPAR

MIC

ROBR

OBE

DAT

A PL

OT O

F Na

2O vs

. CaO

p

15 14-

13-

12-

11-

10-

0- 8- 7- 6- 6- 4- 3- 2- 1-

aibltlG

feld

spar

gra

ins

with

in q

uartz

-alb

ite

lato

veins

andw

lna-

olig

oGla

aa fe

ldsp

ar

aa g

roun

dmas

s pha

se

i 00-1

0

0.00

1.

00

2.00

3.

00

4.00

5.

00

6.00

CaO

wt0X

o7.

006.

009.

0010

.00

-88-

Description of chlorite microprobe analyses are given in Table 7 and the analytical results are presented in Table 8 The few chlorite grains analyzed were all fine grained groundmass grains intergrown with albite, quartz, carbonate end mica Chrome contents ore low, with the highest values being less than 0.5 wUC Cr203 (Figure 14). The chlorites ore compositionolly classified os ripidolites (Hey, 1954. Slight variations in Fee and MnO contents of chlorites between the two samples analyzed may be due to bulk rock chemical differences (Figures 14 and 15).

RecommendationsThe style, intensity and extent (over 50 meters) of the alteration and

veining encountered in DDH BW-92-2, and the possible correlation of this zone with the quartz veining and green carbonate developed in outcrops on claim 1131377 to the northeast in Work Township, suggests o potentially extensive gold mineralized target To determine the extent of olteration and mineralization occuring along this zone, it is recommended that on IP survey be conducted between the Baseline and L6E along lines 15N to 33U Follow-up work would be dependent on the results. Although no significant assays have been obtained from the zone to dote, elevoted barium contents occurring within the hydrothermal micas and the occurrence of common sulphides with the quortz-albite veins may suggest an analogy to Hemlo-type mineralization.

TABL

E 7

DeSC

ft/Pr

/OM

Of

•W

WW

BN

fWH

Ti

ANAL

YSIS

NO.

SA

MPL

E AN

ALYS

IS D

ESCR

IPTI

ON

1 PI

34

flno g

raine

d gr

ound

mass

chlor

ite2

P134

cir

cle 4,

oea

n* M

lvaga

ohlor

it* b

ttwaw

i albt

tt an

d ml

oa lo

ntt

3 P1

34

rando

m gr

eund

maai

ehlor

ita4

P132

Mi

e. Plo

t. 4.

ehlor

lto In

ttrgr

own

with

quar

tz. a

lMto

and

mlea

B P1

32

Mie.

Plet

. 4. o

htor

tt* In

torg

rown

with

qua

rtz, a

lblto

and

mle

a

TAB

LE

8

BtQ

WA

TIR

PftO

PIftT

Y. A

IOP.

PHY

TOW

NSH

IP

AN

ALY

W N

O.

SAM

RJ

HO

t TO

I A

BO

* O

f809

M

nO

P*0

M

0O

CtO

f*

0

KM

N

tfO

FI

CI

TO

TAL

i . 1

114

l 1*

4l

194

4 III

9 1*

8

91.8

7M

. 19

11.4

199

.91

H.4

4

ae*

au aar

ao9

aot

91.9

799

.11

99.4

4M

.97

99.7

9

AM

O.M

0.99 aw O.M

AN

0.41

O.M

0.99

0,84

19.9

918

.94

17.7

891

.99

91.7

1

19.1

914

.94

19.0

919

.79

19.7

4

0.01 ao

t0,

4*0.

04 aw

0.04

0.11 an 0.08

0.04

0,01 1.99

0,01

0.09 aog

0,01 an a 7

90.

010.

01

an 0.11 au air

0.54

0,01 ao

iao

iao

iao

i

99.8

797

.89

88.9

497

.91

97.9

4

CHLO

RITE

MIC

ROPR

OBE

DA

TA

PLO

T O

F CR

2O3

vs. F

eO

0.9- t 0.6-

0.7-

0.6-

0.6-

0.4-

0.3-

0.2-

0.1-

w tn

m it

mft

t HM

- 1

04=

6

1012

1416

18

FEO

2022

24213

g 3

1

0.9-

0.8-

0.7-

0.6-

0.5-

0.4-

0.3-

0.2-

0.1-

0 1012

CH

LOR

ITE

MIC

RO

PRO

BE

DA

TA

PLO

TO

FMnO

vsFc

O

03

analy

B0s f

rom

sam

p/* P

f34

1416

18

FEO

; 4N)

1

analy

ses f

rom

sam

ple P

132

20i 22

2426

-93-

References

Berry, L. G.

1939: Geology of the Bigwoter Lake area; Ont. Deportment of nines. Vol. 48, pt 2, l Ip. Scale r r 1 mile.

Barlow, R. B.

1988: Totol magnetic field colour image developed from digital

archives of the Ontario Geological Survey, Timmins area, hop

8113a Scale 1:100,000.

Bright, E. G., and Hunt, D. S.1971: Pamour Sheet, District of Cochrane; Ont. Deportment of Mines

end Northern Affairs, Geol. Compilation Series, Prelim nap P698, scale l" r 2 mile.

Condie,K.C.1984 Archean Greenstones Belts; Developments in Precambrian

Geology 3: Elsevier scientific publishing Company, 434p.

Ferguson, S. A.

1964 Murphy Township, District of Cochrane; OnL Department of Mines, Prelim, nap P255, scale r r 1/4 mile.

Hey, M. H.

1954: A new review of the chlorites; Min Mag., Vol 30 p.277. *

Irvine, T. N. and Barager, W. R. A.1971: A guide to the classification of the common volcanic rocks;

Can. Jour. Earth Sciences, vol 8, p. 523-548.

-9*-

Jockson, 5. L, and Fyon, A. J.

1991: The Western Abitibi Subpnmnce in Ontario; in Geology of

Ontario, Ontario Geological Survey, Special Volume 4. Part 1,

p. 405-484.

Jensen, L. S.197& A new cation plot for classifying subalkalic volcanic rocks;

Ontario Division of Mines, Misc. Paper 66,22 p.

LeMoitre,R.W.(ed)1989: A classification of igneous rocks and glossary of terms;

Blackwell Publishing, Oxford, England, 193p.

Miyashiro, A.. 1974 Volcanic rock series in island arcs and active continental

margins; American Jour. Sci., vol. 274, p. 321-355

Ontario Geological Survey (OGS)

1980: Airborne electromagnetic and total intensity survey. Timmins

area. Murphy Township - Wark Township; by Geoterrex Limited,

for Ontario Geological Survey, Maps 81071 and 81063, scale 120,000.

Romsey, J. 6.1983: The techniques of modern structural geology; Volume 1, Strain

Analysis. Academic Press Inc., 307p.

Winchester, J. A. and Floyd, P. A.1977: Geochemical discrimination of different magma series and

their differentiation products using immobile elements;

___ Chem. Geology v. 20, p. 325-343._______________

APPENDIX A

Sample descriptionsfor

P-83,84 and P-93 Series

BIGWATER PROPERTY Murphy Township, Timmins Area

DESCRIPTION OF 1983-1984 GEOCHEMICAL ROCK SAMPLES

P364 P444 PS64 P13-64 PI 4-84 P1&64 P4044 P41-64 P4244 P50-83 P5&63 PS4-83 P5&63P5643P57-63 P56-63 P90"93 P60-93 P70-83 P71-83 P73-63 P7S63 P7643 P78-83 P7IW3 PSO-83 P64-63 P93-63 P94-83 PI 07-63 PI 0*63 P1 14-64 P1 17-64 P12064 P12QA64 PI 21 -64 P26044 P261-84 P2B^64 P26&64 P26&64 P27364 P27464

Basal, massive, meo^m grained, medum grey Basal. pOowed. ight grey Basal, massive, ight gray Basal. pBowed. vesc&aBTKomabBic clast in cut iglomerateBasa*, massive ight brf orange weaftenng Basal, pitowed. medun green

basal. pBowed vesictaar. ight grey

Basal, massive. iQht to motfiun grey Basal, massive, madun to coarse grained

Peridotiuc Koma&e, caihfMVrti/pd, orange brown we marinrjV ViKHMIIH* nWIIMIMVi ViB KMM lollClÛ

PemkriiiiL kuuimiie, ukx^rbuiuiB seipeiwJiie. veiy lisX'tnmPMiriniilir fcnmatiia tylrn^ 5fa^? ipMfaif riarfr yiimii fcaah SMfaCft

Basal, plowed, vesioaar Basalt, massive, imxlHmiHly toiated. MI nil t tm Basal, pBowed. vesioaar. we! foaeiaed. ajiTN greyBasaltic clast in conglomerate Foeated ukmmafc matrix of conglomerate Peridottic komatiteBasamc fcomatite. rusty woathoring

UPjaniaacinaliixc4coripômerate

BasaUc. peridotibc kornatito. minor talcPttuuuuu KOfnaoNe. poiysubMed Rhynito rim: ito, bUI weamering. grey trashRhyotte-dacito. minor sericite Rhyoite. ight weatheringRhyoite. weakly foJraod. minor vesicles Rhyoite, massive Peridottic komatite. mecSun grey, iremoilic Fe-thotoito. dark green Tn mntoim, dark green Basal, massive, fght grey Basalt pitowed. varioittc ight grey Basaltic tonalite, medium grey, miniiun Peridotitic komabBB. minor biotiie. woaJJy tohated

Sample Descriptions (1993) for whole rock chemical analyses, geochemical analyses, thin sections, polished sections

P1-93 Variolitic pillow basalt, light to medium green, light grey weathering, vorioles to lent

P4-93 Basalt, massive, medium green weathering end fresh.

P5-93 Basalt, strongly foliated, light grey fresh.

P6-93 Basalt, massive, medium-light grey, weakly foliated.

P7-93 Variolitic pillow basalt, light grey green.

PB-93 Basalt, massive, moderately carbonated.

P9-93 Basalt, komotiitic, sheared, tremolite-talc olteration

P10-93 Conglomerate/debris flow, largely ultramafic matrix, minor biotite.

P16-93 Basalt, silicified, pillowed, vesicular, dark grey.

P17-93 Brown weathering, well foliated hyaloclastite matrix to silicified pillow basalt

P20-93 Basalt, well foliated, medium to dork green, vesicular.

P21-93 Basalt, pillowed, light grey, weathers light grey.

P25-93 Granodiorite, massive, medium grained equigranular, licjrt. grey, white weathering.

P26-93 Quartz vein - smokey

P30-93 Basalt, massive, silicified, dark grey, white weathering.

P31-93 From rusty zone within silicified massive basalt, containsP32-93 3-5 percent disseminated po-py.P33-93

P35-93 Basalt, massive(?), dull grey weathering, non-silicified.

P36-93 Quartz vein

P37-93 Hyoloclostitic(?) looking moteriol ossocioted with o pill bx.

P3B-93 Minor py-po in poorly exposed rusty weathering pillowbasalt, non silicified.

P39-93 Seme

P46-93 Basalt, pillowed, vesicular, silicified, dork grey, white weothering

P50-93 Bronodiorite, massive, white weathering, biotite 15*, quartz 20*

PSI-93 Basalt, pillowed, vesicular, weak (?) silicification.

P52-93 Quartz vein, dark grey to block, barren

P53-93 Basalt, pillowed, vesicular, silicified

P54-93 Basalt, pillowed, weak to non-silf elfied(?), minor pyrite

P56-93 Basalt, massive, silicified, highly fractured

P57-93 Float, 30 by 15 cm, rusty weathering, amphibolitized and contains spotty patches of sulphide (po * sp?).

P58-93 Basalt massive, white weathering, moderate silicification

P59-93 Float, rusty, 50 by 20 cm, mafic volcanic, possible green malochite(?)stoining.

P60-93 Rusty weothering pillow rim containing 3-4 percent pyrite

P61-93 Narrow rusty weothering zone in silicified pillow basalt

P62-93 Basalt, pillowed, non-silicified, dull grey green weothering.

P64A-93 Basalt, massive, weakly vesicular, dark green

P67-93 Variolitic pillow basalt

P68-93 Quartz vein, 10-20 cm wide, minor po-py-sp(?)

P70-93 Quartz vein, minor po * cp?

P71 -93 Conglomerate/debris flaw, sample of ultramafic matrix

P72-93 BasalU?), massive, light grey, minor biotite

P73-93 Debris flow/conglomerate, 3-4 percent pylte.

P74-93 Basalt, massive, fine grain, light grey, 2-4 percent pyrite

P78 to 83 Series of sulphide bearing samples taken from nibble pile at-93 edge of a trench within poorly exposed conglomerate/debris

flow.

P66 to 86 Basalt, light grey, massive, locally containing 3-5* biotite,-93 2-5* pyrite and minor malachite stain.

P93-93 Highly silicified pillow breccia fragment

P95-93 Matrix ta pillow breccia, dull grey green weathering

P99-93 Rusty zone in pillow basalt, l - 0.5 m wide, 2-3 * py-po.

P100-93 Amphibolitized pillow basalt

PI 01-93 Variolitic pillow basalt

P102-93 Rusty (pa) zone at variolitic pillow margin, 15 cm wide.

P105-93 Drill core, basalt, massive, med-daric green, 2-3* leucoxene. Hole BW92- 1 (59m)

P107-93 Drill core, basaltic komatiite, abundant tremelit/actinelite, Ho1eBW92-1 (117m)

P108-93 Drill core, basaltic komatiite, pymene spx texture. Hole BW92-1 (122m)

Pill -93 Drill core, peridotite komatiite. Hole BW92-2 (28 m)

P115-93 Drill core, quartz vein. Hole BW92-2 (58 m)

P116-93 Drill core, variolitic pillow basalt Hole BW92-2 (110 m)

P131-93 Drill core samples of light grey ondesitic pillow basalt fromP132-93 hole BW92-Z Samples taken ot 112m, 113m, 106m, 120m,P133-93 96m respectivelyP134-93P135-93

P137-93 Drill core, quartz vein containing emerald green mica and minor pyrrhotite. Hole BW92-2 (167m)

P139-93 Drill core, ondesitic pillow bosalt os P131 etc. Hole BW-2 at 67m.

APPENDIX B

6EOCHEMICAL DATA

BIGWATER PROPERTY, MURPHY TOWNSHIP

-J -J Ok Ok Ok Ok O* M M M *— ** O O * W A O 41 (D -J Ok W W

b)UIUI**U* W* Ok Ut* t* M WMU^ A m EM * Ok :B U :* A. l* A I* IB•- bf 0 Ok *- -J vO i- M 0 U * Ui -J W W Ok M M O* -J O O UBJ i- M -J ** o* W ;* M W M O Ok S O A 4* A M ~ 31

~ - * - -----* ™

. Ok O O i- WOkOkAOk0UI*-J*. WOMOKO WOOtOUOOkUI — — 1*4 O M *- Ot Ji -J O * -^ O 4k

* 3* 31 m i* t* 4) IP Ui Uk A 3k ^ A V -J O -4 9k —

* OOÔO^tUIOOtÔO O

IO

aaooooooo0mv*

*— •~MM*(**-OOOOOf* MMfM 3f A •ir*' M Ok W 0U* * 3k ^j o A 3B A A3 S A — A 3k * A 9 3B M Q

O Ok M W Ui * *- O O t- O O O W M * i- -*J * * OkM Ok *- M M *0 -J "J W *- M M * Ok *- W Ok M -J

•^ Vi Ok i- 0 Ok O 0 0 f 0 J Ok M | * W W W - 0 *- OJ **- M * O Ok U OJ W ** 0 * O UI W O J*. UI i- U OJO O Ui M -J M *- O ft* 0 -J Ui U O O W *— O 0 O O O O Ui **-J O O O O O O * 0 O O -J O 0 * O *O 0 0 Ok O

O* -J -J 0 "J O -J *- ** M M M lO 0 * 0 0 M * M Ui U V *OOk Ok -J 0 tt A O O O O 0 0 O 0 p *O Ok V ** 0

t* O * W ^J l- 000 W O O M O Ok O Ok Ok i* 1 *D Ok A. OK* W M W O U U W W U -J W 0 UJ ^ O; O0 O j;

W M *- W P- O O W W dfc. *- Ui O O k— M O M O O O O 0 *-Ui *- O O O O O *— t— * O U M O *— O * M f- W J

^ Ok Ok OJ * W ^ *^ ^ 0 l* Ok O O Ok Ui U M O ^ ^ — M O * M *-O O 0 *-^ 2! W--M UI 0 0 O W 0 t-O J* MUIÛOWWA-ogAÔkfWUiUMAOM -J * * *—Ui *O t* O tf W Ok O Ok O) *- UI * 0 Ok W ** UI 0 O O

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TELEX: 06-986017 FM: {416)445-4152

REPORT

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TO: D.R. PYKE 6 ASSOCIATES ATTN: D.R. PYKE 31 DEIAIR CRESCENT THORNHILL, ONTARIO L3T 2M3

COSTOHER No.

DATE SUBMITTED l-Nov-93

754

REF. FILE 16625-D6 Total Pages 6

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O - QUALITY OWraOL DUPLICATE

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Ministry ofNorthern Developmentano^Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

nt and Mines. FourthjJ \ -k

Personal information cotacted on thto form Is obtained under the aiithority of ttw Mining Act. Thte information wiH^this cotection should be directed to the Provincial Manager. Mining Lands. Ministry of Northern Development and Mines. Fourth Floor. I^.Cedar Street.Sudbury. Ontario. P3E 6A5. telephone (705) 670-7284. v

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for n

Recorder.- A separate copy of this form must be compfet- Technical reports and maps must accompany- A sketch, showing the claims the work is assi I MURPHY 900

diem No.Rsconfod Holttoifs)

^ TBtophofW No.3 s

Mining DMskm

- WARKM or Q Plan No.

-J weWork Perlbrmed (Check One Work Group Only)

WorkGroup

Geotechnical Survey

Physical Work,Including Drilling

Rehabilitation

OD KM Authorized Work

Assays

Assignment fromHeserve

Type

GeoJoQ/Gc*X

J

"ÊCEnTprT"K)

II IW 1 T 1QOJ*JUM j. o lyyH

MINING LAN^.....^

RFP.ORnED

—— UAV Q 1 1QQA ——in A T o J. iaa*t

RpTPipt

Total Assessment Work Claimed on the Attached Statement of CostsNote: The Minister may reject for assessment work credit all or part 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 Address

f /•)d 7O7 f)

^Mlt^M^ft A H

^ 4 n n M^HKA^^^h^. i on reversel certify that at the lime the work was performed, the chums covered in this work report were recorded in the current holder's name or held under a

Certification off Wmk ReportJ sumo durino Butflfor fliter

AodnMS of Person Certifying

POlXUPI^MtMNQQMSrON

l certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or \ Its completion and annexed report to true.

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Total Value Work Total Valua Total Assigned Total Raaarva

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mwCredits you are claiming in this report may be cut back. In order to minimize the adverse effects of such oUetiora, please imiicate from which claims you wish to priorize the deletion of credits. Please mark (**) one of the following:1. D Credits are to be cut back starting with the claim listed last, working backwards. 2. D Credits are to be cut back equally over aH claims contained in this report of work. 3. D 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.

Hotel: Example) to themhilna claims.

n fl0p06flMfitef mBmoffWMiiin of •QroontwitS) 0tc.9 with ntspoct

Note 2: M work ha* been performed on patented or complete the following:l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature

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VP to bo ed tt re Dato

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 (^) one of the following:1. D 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. D 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.

Hotel: Examples of beneficial Interest are unrecorded transfers, option agreementa, memorandum of agreemenU, etc., with respect to the mining claims.

Note 2: If work l i been performed on patented or leased land, complete the following:

l certify that the recanted holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Date

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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 (f) one of the following:1. D CredHs are to be cut back starting with the claim listed last, working backwards.2. DCredHs are to be cut back equally over all claims contained in this report of work. . ,3. HCredHs are to be cut back as priorized on the attached appendix. CVv-fcj^/s f**~i" //, frc? /C

In the event that you have not specified your choice of priority, option one will be implemented.

Motel: Examples of lto the mining claims.

2* Iff work lias been performed on patented or

etc., wNIi respect

l certify that the recorded holder had a bl or leoaod land at Hw time Hw work was performed.l ^*m —^B*

tffcfctf

t in the patented D—,VJ J.///4ij3vfa

Ministry ofi Dovofopfiwnt

and Minos Ontario ~

? lore du

et des mines

Statement off Costs for Assessment CreditEtat des coOts aux fins du credit devaluation

Mining Act/Loi sur les mines

Personal Information coiocted on this form te obtained under the authority of the MMng Act This information wM be used to maintain a record and ongoing status of the mining ctomKs). Questiona 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.

Los renseignements personrecueiKs en vertu da la Lof ides concessions minleres. Adresser twite question sur la coitoce da irenseignemonls au chef provincial des terrains mMors. ministereDevetoppement du Nord et das Mmes, 159. nw Cedar. 4*j(Ontario) P3E 6A5. telephone (705)11*7264.,

1. Direct Costa/CoOts directs

Type

,/Viys

Contractor's and Con*Meftaiit*9 Fee* Drafts de

et de ('expert-

Description

Labour MaJn-d'oeuvreField Supervision Supervision sur le terrain

Typ*

Type

Typ*

Amount Montant

322.

73

Total Direct Costs Total des coOts directs

Totals Total global

/SO

2SJB2-

2. Indirect Costs/CoOts indkects* * "~*K When claiming Rehabilitation work Indirect coste ,ara not

nil,-....i."-l— î^ nnnnnnrnnttmtt *aM^*ôiiowaiNo as asoooafnoni wonx.Pour to rembouraement desjravaux de rehabiHation. tescoOts indlrects ne sont pas admissMea en tent que travauxd'evaluaUon.

Type

Food and Lodging NourrHure et

3 4 snot)

Amount

781

Sub Total of IndlrectCosts Total pattle! dss coOts Indlrects

Amount Aaowabte (not greater then 20* of Direct Coste)B^Lwstsatvt sMhsBaaieds)MBBi /H*aUM^sWlskefet sisasi **** (^ jtskA jvtalalsi e4b*M*teil

Total Vahw of (Total of Dfcect

Totate Total global

JBL660

Note: The recorded holder will bethis statement of coste within 30 verification is not made, the eJ or part of the

1. Work filed within hw years of the above Total Value of Ass

iinirn fciirhiimsSiat tflfHtini i f \lrlJrfUriiejnSFJBea ut wun

2. Work filed three, four or five years after completion is claimed at SOTb of the above Total Value of Assessment Credit. See calculations below:

Note: Le ttubire enregjstre sera tew de verifier tes c te present etat des coots da effet. Site verification n'est i is ou une perite des

tour achevernent wxmnBeducredld'

Remises pour depot

1. Les travaux deposes dans tes rembnnesalOOttdeb

2. Les travaux deposes tn^.qiiatreoudnqansapre8leur achevernent sont rembourees a 50 1* de la vateur totate du credit d'evaJuation susmentionne. Voir tes cateute cktossous.

Total Value of Credtt Total Ai nwntCteiinedx 0.50

Vateur Mate du credK d'Awaluattonx 0.50 -

EvaJuaHon taMa damandta

Certhlcsilon Verifying SUrtement of Costs Attestation de I'etat des coOts

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred white conducting assessment work on the lands shown on the accompanying Report of Work form.

that as(Re id Holder. Agent. Position hi Company)

J'atteste par la presents :que lee montants indiques sont le plus exact possible et quo ces depenses orrt ete engagees pour effectuer les travaux d'evaJuatton sur tes terrains indiques dans la formule de rapport de travail ci-joint.

l am authorized Et qu'a titre de. je suis autorisert. reprteentent. poeto occupe dane la compegnto)

to make this certification afairecetle

0212 (0*91) Nota i Dans cette fuuimlo. lorsou'H dsslgne des

OntarioMinistry of Ministere duNorthern Development Developpement du Nord Geoscience Approvals Section and Mines et des Mines 933 Ramsey Lake Road

6th Floor Sudbury, Ontario P3E 6B5

August 30, 1994

Telephone: (705) 670-5853 Fax: (705) 670-5863

Our File: 2.15461 Transaction /: W9460. 00138

Mining RecorderMinistry of Northern Development fi Mines60 Wilson Ave1st FloorTimmins, OntarioP4N 2S7

Dear Sir:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS OH MINING CLAIMS P. 1073195 BT AL IN MURPHY AMD WARK TOWNSHIPS

Assessment work credits have been approved as outlined on the original report of work form for the submission. The credits have been approved under Section 12, Geology of the Mining Act Regulations.

The approval date is August 29, 1994.

If you have any questions regarding this correspondence, please contact Chris Hamblin at (705) 670-5856.

t Yours sincerely,

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

Enclosures:

cc: Resident Geologist Timmins, Ontario

Assessment Files Library Sudbury, Ontario

OntarioMinistry of Ministere duNorthern Development Developpement du Nord. . .. . . v 7 Geoscience Approvals Sectionand Mines et des Mines 933 R^êy ê Road


August 30, 1994

Telephone: (705) 670-5853 Fax: (705) 670-5863

Our File: 2.15461 Transaction #: W9460. 00138

Dale R. Pyke 31 Delair Cres. Thornhill, Ontario L3T 2M3

Dear Sir:

Subjects APPROVAL OF ASSESSMENT WORK CREDITS OH MINING CLAIMS P. 1073195 ET AL IN MURPHY AND WARK TOWNSHIPS




Yours sincerely,


CH/jl Enclosures:

Ministry ofNorthern Developmentand-Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

Number l

0006 1

o iPersonal 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. 15^ Cedar Street.

Sudbury. Ontario. P3E 6A5. telephone (705) 670-7264. \) * l *~l

Instructions: - Please type or print and submit in duplicate. ~ *~~- Refer to the Mining Act and Regulations for n

Recorder.- A separate copy of this form must be comptel- Technical reports and maps must accompany- A sketch, showing the claims the work is assi. ^TTNEoowTiMeTiiuRpHY 900

Recorded Holders)diem No.

Totophono No.

73}Addressj/ M or G Plan No.

Mining DivisionM or G Plang-3^G .1*j

Dates W

Work Performed (Check One Work Group Only)WorkGroup

Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

&2&JOQ/G&S

1"ÊCpTvp?^

to 1 — JUNl 3 1994 —

MIN.NG LAN,!....^,^

RFCORDED

—— MAY ^ 1 1QQ4 ——ffi A T O J- 133*1

Rpr.Pipt

Total Assessment Work Claimed on the Attached Statement of Costs

Note: The Minister may reject for assessment work credit all or part 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 Address

3J

f- w- rji /l 7o7 S4n frcud /o e fsn±

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

l 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 Recorded Holder (Signature)

Certification of Work Reportl 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 Citifying

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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 (^) one of the following:

1. D 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. D Credits are to be cut back as priorized on the attached appendix.


Note 1 : Examoles of beneficial interest are unrecorded transfers, ootkm aareements. memorandum of anmomanta. ste., with raanactto the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

1 certify that tne recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Dale

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1. D 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. D Credits are to be cut back as priorized on the attached appendix.


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 certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Date

i

Total Numbtr Total Vtlut Work Total Valin Total Aaalgntd Total Rtttrvt ofWma Dona WorkApplltd From

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1. D Credits are to be cut back starting with the claim Hsted last, working backwards. 2. D Credits are to be cut back equally over all claims contained in this report of work. . i t 3. Hcredits are to be cut back as priorized on the attached appendix. C- ffdJt } * 0S~C- f O ^^ ^^ "^ * '


Motel: Examples of benefldaJ interest are unrecorded traraf ere, option agreement to the mining claims. s/

Note 2: If work has been performed on patented or leased land, please complet

1 certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

1 — —— . ————————— i ——— . ———————————————————

s, met]

?\/ ethil

•wiouoiiin wi i

5?olowlng:

igreements, etc., wtth respect

^Ti'^î/^ Date y, J .11

//MLl'doA

Ontario -

Ministry ofNorthern Developmentand Mines

! (ere du Devetoppement du Nord et des mines

Statement of Costs for Assessment CreditEtat des couts aux fins du credit devaluation

Mining Act/Loi sur les mines

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record arid ongoing status of the mining claimfs). 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 rcnseignements pereon *f vod**Hnr ifi"T 'B prffrBnte formuto sent recueilKs en vertu de la Loi —^"""^—^'—ir ft fcf- un registre des concessions minieres. Adresser toute quesiton sur la coltece de ces renseignements au chef provincial des terrains miniers. ministere du Devetoppement du Nord et des Mines. 159. rue Cedar. 4e etagoJSudbury (Ontario) P3E 6A5. telephone (705) Mk7264.

1. Direct Costs/Couts directs

Type

Wages Satakes-73 /n/**

uOXiys

Contractor's and Consultant's Fees Droitsde

•t de I'expert-

Suppltes Used Foumttures utMissi

EcjulpflMfif Rental Locertlofi ite materiel

Description

Labour Main-d'oeuvreReid Supervision Supervision sur le terrain

Type Â/fityê^TTt/sy 9fV' Shtti xczt

Oro SJ/nat'J*Cf~cf:i'~cix^'

Type

&/T7J 1 ' J?'~CGC55")qs

tfcfar (^cryiC^f

Type

Amount Montan!

22*7^5

-/.75

4^2. 3^2.JO&

73

/s 7

Total Direct Costs Total des coOts directs

Totals Total global

^37^5

J2t*~J

/3o

2SJ&2-

2. Indirect Costs/CoQts indirectsNote: When claiming Rehabilitation work Indirect costs .are not

allowable as assessment work.Pour le remboursement des travaux de rehabilitation, tos couts indirects ne sont pas admissiWes en tant que travaux d'evaluation.

Type

Transportationy— m —— Minmtiranspon

Food flflQLodging Nournttm ctMbergementMODillUlHMI Wsd

Mobilisation etrlJîiliiH^^llj-t.KavmoDnmnon

Description

Type

2b(.\Sk** @

* 3tyk' t j

3 4 n*0t) Jrti/3(fr'ô/o/iy

Sub Total of Indlt Total partM des couta

Amount Montant

7&I

•ect Costsi Indirects

Amount Allowable (not greater than 20* of Direct Costs)MOflttnt 4KMH98iviv (n OXCvQMlt pett 20 9v QOS COUIS dlf9Gl8|

Total Value of Assessment Credit Vsteur tot* [Tolal of Direct and AMowsMa d'evshiatlo Indhvd costs) (Totri OM ci

toducredtt n tttdtadt

Totals Total global

78J

680

J461

ZLt*43

Note: The recorded holder will bethis statement of costs within 30 verification is not made, the M all or part of the assessment wort

Filing Discounts

1. Work filed within two years of co n the above Total Value of Ai

2. Work filed three, four or five years after completion is claimed at 50*fe of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

Note ; Lelituteire enregtstre sera tenu do verifier tes depenses demandfes dans le present etat des couts dameffet. Si la verification n'est f is J ou une partie des travaux d Avalu

Remises pour depot

1. Les travaux deposes dans lesremboursesalOO'K.detavateutJ tetesusr

U utipresentes.

31 1994

i arts suivant tour achevement sot Dnneeducredld'evaKatk i.

2. Les travaux deposes trois, quatre ou cinq ans apres tour achevement son! rembourses a 50 9* de la vatour totale du credit d'evaluation susmentionne. Voir les calcute d-dessous.

Vatour totale du credit d'evaluationx 0.50

ationtotate

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.

that(Recorded Holder. Agent. Position in Company)

to make this certification

Attestation de I'etat des coOts

J'atteste par la presents :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 indiques dans la formule de rapport de travail ci-joint.

l am authorized Et qu'a litre de ___________________ je suis autorise(Ittutaira enregistre. reprfeenlant. poste occupe dans la compagnto)

a faire cotte

0212 (0491) Nota : Dans cette formuto. torequ'il designe des le masculin est mMse au sens neutre.

Ontario

Ministry of Ministere duNorthern Development Developpement du Nord Geoscience Approvals Section and Mines et des Mines 933 Ramsey Lake Road


Telephone Fax:

(705) 670-5853 (705) 670-5863

August 30, 1994 Our File: 2.15461 Transaction /: W9460. 00138

Mining RecorderMinistry of Northern Development fi Mines60 Wilson Ave1st FloorTimmins, OntarioP4N 2S7

Dear Sir:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MIMING CLAIMS P. 1073195 ET AL IN MURPHY AND WARK TOWNSHIPS




4

Yours sincerely,


Enclosures :

cc: Resident Geologist Timmins, Ontario

Assessment Files Library Sudbury, Ontario

OntarioMinistry of Ministere duNorthern Development Developpement du Nord .

. ... j Vi- Geoscience Approvals Sectionand Mines et des Mines 9 33 Ramsey Lafce R0ad


Telephone: (705) 670-5853 Fax: (705) 670-5863

August 30, 1994 Our File: 2.15461Transaction /: W9460.00138

Dale R. Pyke 31 Delair Cres. Thornhill, Ontario L3T 2M3

Dear Sir:

Subject: APPROVAL OP ASSESSMENT WORK CREDITS ON MINING CLAIMS

P.1073195 ET AL IN MURPHY AND WARK TOWNSHIPS




Yours sincerely.


CH/jl Enclosures:

42A

11N

E007

4 2

1546

1 M

UR

PHY

200

JES

SO

P

.f-

o '-

"/)?

.——

.——

— ^—

— (B

^—

—

—l

HO

YLE

TW

P.

O O ?

P

i

H

G-2

880

0865

-9

li

.1'," tt'

00ro01io

X^REAS WITHDRAWN FROM DISPOSITION

M.R.O. - MINING RIGHTS ONLYft,R,0. - SURFACE RIGHTS ONLYM.+ S. - MINING AND SURFACE RIGHTS

" FM*

THIS TWP. IS 8U

ff : l

r':

100

THE INFORMATION THAT APPEARS ON 1MB MAP HAS tffEN COMPILED FROM VAHtOUS SOURCES, AND ACCURACY lg MOT GUARANTEED. THOSE WHtHWa TO STANpE MIN ING OUIM8 SHOULD CON SUL* WITH THf MININGRooojioea MIWSTRT OFNQPrTHERN bfViLQP-

'MINT AND MINES, POR AD DITIONAL INFORMATION ON THE STATUS Of THE LANDS SHOWN HERtoN

-V .', ,v'

oQ

PROSSER TOWNSHIP

—r-~-: vi

__ __ ^^.^.^.-. _ __^— — W"* if

(8 UNITS)

1155 e*'-' \

M2 UNITS)

———. ——. —— - H

6SM7 I 5590* II9IMS ' 1204723 i

- - - - -e- --

190922a

P . P 833449

riooi /; TIOOO

p7IOK j 7IO9I

•\I90I521190149e

(12 UNITS) 4 UNITSF e l d man

•78801 J P878502

~V 3*S7t4 J - ^

1186867

8 UNITS-\Bouchard1186866

— - — — IV — -~4 UNITS

IV o o

H O

X "D

— l

MURPHY TOWNSHIP

LtGENOHIGHWAY AND ROUTE NoOTHER ROADSTRAILS ~SURVEYED LINES

TOWNSHIPS. BASE LINES ETC ——LOTS. MINING CI AIMS. PARC*E LS. ETC -

UNSURVEYED LINESLOT LINESPAHCcL BOUNDARYMINING CLAIMS ETC ——

RAILWAY AMD RIGHT OF WAY -*— UTILITY LINES -o- NON PERENNIAL STREAM — FLOODING OR FLOODING RIGHTS ii SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKt-G MINES

TRAVERSE MONUMENT

nr .T-

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT

PATENT, SURFACE ft MINING RIGHTS ." .SURFACE RIGHTSONLY..- .

.MINING RIGHTSONLY_....LEASF. SURF ACE ft MINING RIGHTS..

" . SURFACE RIGHTS ONLY...... ," .MINING RIGHTS ONLY....,.—

LICENCE OF OCCUPATION .___..__.ORDER IN COUNCIL .. ............. ..RESERVATION ........................CANCELLED __...._____.........SAND ft GRAVEL __......_.__ ...

SYMBOL

...^ OC

. __ (J)

NOTE MINING RIGHTS IN PAMCFLS FATfNTEO fHlC'H T O "**V' 1 813 VESTED IN ORIGINAL PATkNTEE *V TMt. PUB1.

LAND* ACT. MS Q 1*70 CHAP MO. SEC *3. :UB*tC

MMrv*

Chain*

MO

10 n 40

MO O MOO 3000

SCALE 1:20 000

AND SURFACE RUNTS

THIS TWP IS SUBJECT TO FOREST ACTIVITY IN 1994/98 l FURTHER INFORMATION AVAILABLE ON FILE.

\

1994

TOWNSHIP

WARK

00Ol 6

I

[t* it

.154 6 l[Ali'

M N H. ADMINISTRATIVE T!STn;CT

TIMMINSMINING D IVISION

PORCUPINELAND TITLE3/ REGISTRY DIVISION

COCHRANEJ

Ontario

Ministry ofNaturalResources

Ministry ofNorthern Oevetopmentand

iS86

G-398900O)01lo

i

LEGEND

Archean

quartz veinmg.v^KM \ b\ green carbonate) (jr^Y,^ alteration,

trace

lN'

N 3PII4/

WARK TWPMURPHY TWP

P139193PII 2(93)

PIIK93)

108375^.

-.\\-P 6(93)^-.

P 83(93) Samples off dum

from nearby trench

2a f\-P*(93)

40 I073I96f I II48I3

CONC 6

graphitic argillite zone - interpreted from airborne Input conductors

rarea dominated by magnetic high (airborne) and interpreted to be largely debris flow material with lesser ultramafic and basaltic flows

end of dnveable road

FELDSPAR PORPHYRY6 Leucocratic fine-medium

grained feldspar porphyry

GREYWACKE - SILTSTONE 5a Massive greywacke 5b Minor interlayered siltstone 5c Graphitic argillite

CONGLOMERATE (DEBRIS FLOW) 4a Massive, poorly sorted, largely

ultramafic clasts and matrix 4b Largely Basalt-andesite clasts

in ultramafic matrix

FELSIC VOLCANIC ROCKS 3 Rhyolite - largely massive

MAFIC VOLCANIC ROCKS (BASALT-ANDESITE)

2a Massive2b Pillowed2c Vesicular2d Variolitic2e Flow breccia2f Tholeiitic basalt

ULTRAMAFIC VOLCANIC ROCKS (KOMATIITE)

1a Massive1b Polysutured1c Spinifex textured1d Talc-carbonate alteration1e Carbonate veining1f Basaltic komatiite

-o(D

o! o

o

SYMBOLS

5 Outcrop, outcrop area

Foliation60

Bedding (tops known, not known)

so Lineation

"^ Pillows; good, poor(top in direction of arrow)

Facing direction of flows from flow morphology

— — -~— Geological contact

— -——- HLEM conductor

J—— Anticlinal axis

Fault

Shearing

• pn(93) Sample location and number (1993 samples in brackets)

Claim post

A Survey pin-post

i———O Diamond drill hole (Noranda Expl.) [BW 92-1 A BW 92-1]

200 300 400 meters

Scale 1 : 5000

o 15^6 i

BIGWATER LAKE PROPERTYMURPHY-WARK TOWNSHIP

Timmins Area, Ontario

GEOLOGICAL MAP

Geology and compilation by

D. R. Pyke 4 K. M. Gunnison, 1993

Documents

GEOL RPT ON BIGWATER PROP · 2017-01-17 · basalt Polarized light P132-93 Photo 21 - Photomicrograph, pillow basalt, boudind quartz veinlet. P132-93. Polarized light Photo 22- Bock