diamond drilling report pick lake project schreiber …

42D14NW8887 63.4713 PAYS PLAT LAKE 010

CORPORATION FALCONBRIDGE COPPER

DIAMOND DRILLING REPORT

PICK LAKE PROJECT

SCHREIBER AREA, ONTARIO

NTS 42 D/14

on 8s-i2.trOMEP Designation No: OM85-4-P-125

February 1986

P. W. A. Severin

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INTRODUCTION

Corporation Falconbridge Copper began exploration in the Winston

Lake area in 1978. The zinc-rich Winston Lake massive sulphide deposit

was discovered in mid-1982 and has been delineated by underground

diamond drilling during 1985. Including 2070 dilution, the mineral

inventory of this deposit is estimated at 3,100,000 tonnes of 170 Cu,

16.07o Zn, 30.0 g/t Ag and 1.0 g/t Au.

Another promising high-grade zinc occurrence, the Pick Lake deposit,

located approximately 1.9 km southwest of the Winston Lake shaft, was

discovered by surface diamond drilling in late 1984. The Pick Lake

deposit, which occurs as an extensive narrow sheet of zinc-rich massive

sulphides, has been tested by drill holes on 200m centres. This report

summarizes the results of diamond drilling completed during the autumn

of 1985 which investigated the possibility of thicker zones of economic

interest within the Pick Lake deposit.

LOCATION AND ACCESS

The Winston Lake area is located in northwestern Ontario approxi

mately 145km northeast of Thunder Bay. A 20km gravel road links the

property with the Trans-Canada highway at a point about 9km west of

Schreiber, a town of approximately 2,000 people,

PROPERTY AND OWNERSHIP

The Winston Lake property consists of 253 claims wholly-owned by the

Corporation and 32 claims that were optioned from Zenmac Zinc Ltd.

(formerly Zenmac Exploration Ltd.). The Corporation has exercised this

option. Upon a production decision, Zenmac is entitled to elect either

a 207o participating interest or a royalty of 1070 net proceeds of

production. The Winston Lake deposit occurs on claims subject to the

above-noted royalty or interest.

The Pick Lake massive sulphide prospect occurs on claims wholly-

owned by the Corporation.

HISTORY

Exploration in the area began in the late 1800's when the Zenith

zinc deposit was discovered. This deposit was mined by Zenmac Metal

Mines Ltd. during the period 1966-1970 producing 180,000 tons of ore

grading 16.570 zinc.

The Corporation acquired the property during 1978-80. Geological,

geochemical and geophysical surveys were completed and culminated in

discovery of the Winston Lake massive sulphide deposit in June of 1982.

Extensive surface drilling outlined the deposit. Results were suf

ficiently encouraging to commence a program of underground evaluation in

early 1984. The underground exploration program was completed by June

1985. On September 23, 1985 the Company announced its intention to

bring the Winston Lake mine into production as a substantial zinc

producer at an estimated capital cost of $52.5 million. Unfortunately,

on November l, 1985, the Corporatioon was forced, by economic and

political events beyond its control, to announce a suspension of the

Winston Lake development. The decision was made because of sharply

deteriorating zinc prices, combined with higher smelter charges.

During this period, surface exploration continued elsewhere in the

project area. The Pick Lake zone was intersected by diamond drilling in

late 1984.

GEOLOGY AND MINERALIZATION

The Winston Lake property is located near the west end of the Big

Duck Lake greenstone belt, an east-west trending sequence of Precambrian

metavolcanics and metasediments.

The Winston Lake massive sulphide deposit occurs at the top of

felsic volcanics overlain by a series of mafic flows. The contact

between these two sequences has been intruded by a complex gabbro sill

which forms the hanging wall for the massive sulphide deposit.

The Pick Lake massive sulphide occurrence, an extensive but, to

date, narrow sheet of zinc-rich massive sulphides tested by drill holes

on 200m centres, occurs within volcaniclastic rocks towards the base of

the Winston Lake stratigraphy. The best intersection assays 1.497,. Cu

and 21.957o Zn over 1.5 metres. The deposit has a strike length of

300-400 metres and is open down-dip.

RESULTS OF DIAMOND DRILLING - SEPT. TO DEC. 1985

Five diamond drill holes (3118 metres) were completed to investigate

the possibility that thicker areas of economic interest could exist

within the narrow masive sulphide sheet. The results, which are

summarized below and included on the appended sections, were generally

disappointing.

TABLE: PICK LAKE MASSIVE SULPHIDE INTERSECTIONS

HOLEWL27WL28WL29WL30WL31

DEPTH708586854460510

FROM667.85555.20830.05432.20476.00

TO668.555.830.433.476.

4550154010

METRES0.60.30.11.20.1

7o Cu1.712.900,140.930.03

7o20.9.6.

16.16.

Zn9644970237

gm/tAg52.058.04.915.912.3

ppbAu130508

1110

DRILLCONTRACTORSt .LambertSt .LambertSt .LambertMcKnightSt . Lambert

Copies of the drill logs, including assay sheets, are enclosed.

SUMMARY OF EXPENDITURESThe following costs are based on Corporation Falconbridge Copper's

Thunder Bay office records.

1. Period; September 12-30th, 1985Drilled WL-27 0-309 metres (Sept. 12-30th)Total meterage drilled during September: 512 metresLow productivity due to mechanical problems.Costa) Contract Cost - St. Lambert invoice #666-ONT-85-15

$18,254.03b) Salaries, travelling, field expenses, assays, etc.

Total for September |12,790.51 Share for WL-27 (309/512) x 12,790.51 ^ $7 ) 719.27

Total Cost Related to WL-27: $18,254.03 + $7,719.27 ^ 325,973.30 (Sept.)

2. Period: October l - December 31, 1985Drilled WL-27 309-708 metres

WL-28 0-586 metres WL-29 0-723 metres WL-30 0-460 metres WL-31 0-510 metres

Costa) Contract Cost - St. Lambert invoices

#666-ONT-85-16#666-ONT-85-17#693-ONT-85-2#693-ONT-85-3#666-ONT-85-18#693-ONT-85-4#666-ONT-85-15#666-ONT-85-16#666-ONT-85-19#693-ONT-85-5#693-ONT-85-4#693-ONT-85-5

Sub-Total

McKnight Drilling Co.Nov. 19, 1985 invoice

$$1$1$

(|(1$1$$$

$

33,518.526,343.0020,050.413,641.0029,252.7022,645.56

423.60)423.60)

10,970.5912,820.65

215.05215.05

138,825.33

27,114.02

WL-27 A WL-29WL-29WL-28WL-28WL-29WL-28 S* WL-31credit WL-27credit WL-27WL-29WL-31WL-28WL-31

__________ WL-30$ 165,939.35

travelling, field expenses, assays, etc.$ 14,845.64

November ($22,376.86)Of a total of 2822 metres drilled in November, 786 metres (part of WL-29, 30 and 31) relates to this application. Pro-rated share (786/2822) x |22,376.86 ^ $ 6,232.53 Total Cost Related to WL-27-31 $165,939.35 + $ 14,845.64 * $ 6,232.53 = $ 187,017.52 (Oct-Nov)

3. Entire Period: Sept. 12 - Dec. 31, 1985(Drill program actually completed by the end of November)

Total Contract Costs $ 184,193.38 Costs of salaries, field costs ^ 28,797.44 TOTAL l 212,990.82

This total does not include any costs related to the operation of Falconbridge Copper's Thunder Bay regional exploration office.

b)Total

Salaries October

TB 519245

TB~5I9248

PICK LAKE DRILL PLAN100 50 O

metres

20.96VoZn SZ.Og/TAg I3O ppb Au ov*f 0.6m

EOH 708m

PICK LAKE DRILL SECTION

MS 2.90*7oCu 9.44 0XoZn 58-Og/TAfl 60 ppbAu ovtr 0.3m

EOH 586m


100 50 O 100-iH-

metres

TB 519247 TB 386770

TB 386767

WL- 29

305 m

4.9gXTAg 8 ppb Au over O. l m


100 50 O 100

metres

TB 519248 TB 519247

W L- 30

MS 0.93 07oCu

EOH 460m

IS.Sg/TAg II ppb Au ov*r 1.2m


4 TB 519247

WL- 31O

ALT

MS 0.03 0Xo Cu !6.37 07oZn I2.SJ/T Ag 10 ppb Au ov*r O.lm

EOH 510m


100 50 100

metres

-IDLE NUMBER: UL-27CORPORATION FALCONBRIDGE COPPER

BRILL HOLE RECORD IMPERIAL UNITS: METRIC UN US

f P ROJECT: PN o?o FIELD COORDS: LAT: 3 -t 70 s COLLAR BRNG: 300 " CONTRACTOR:

c CLAIM t;LOG

DEP: A * 10 E COLLAR DIP: -8?" CORE STORAGE:GRID: EELCO ELEV: 42im HOLE SIZE: BO CASING;UMBER: SURVEY COORDS: LAT: " FINAL DEPTH: 708. o M PLUGGED:AT ION: DER:

DATE STARTED: SEPTEMBER 21, I9S5 ELEV: ROD LOG: MULTISHOT SURVEY:t

C

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*

DATE COMP

COMMENTS:

Depth (M)

3 50

100 150200297309324375425475525575625675

HOLE NO:

LEIED: PULSE EM SURVEY: COLLAR SURVEY:

ACID TESTS TROPARI TESTS MULTISHOT DATACorrected Corrected

ftnsle Depth (m) An9le Depth (m) Azimuth Dip Depth (ra) Azimuth

-87" -86" -86" -84"-83'-BO"-78"-75"-74"-72. 5 0-70" DOUBLE ETCH-68"-67"-65"-62"

285 301 345 306 405 309 465 305525 306585 308645 309705 309

__ .. __ . . .... __ .., ,. .

UL-27 LOGGED BY: R.

SI. LAMBERT DRILLINGCLEAVER LAKE0.8 M BU

X

Dip

-SO" -75" -74" -71"-69"-71*-67"-66"

C. SIM

DRILL HOLE LOG

FROM10

0 to0.8

0.8to179.3

ROCKTYPE

CASING

PATCHYALTEREDOFF

COLOUR

Mottledblue-grey

GRAINSIZE TEXTURE AND STRUCTURE

119 Moderate to well foliateddefined by micas atMatrix sugary to 31 ffi15X qt" eyes *; 3 mtl

ANGLE TOCORE AXIS ALTERATION SULPHIDES REMARKS

Moderate to intensely altered IX Py clots (locally up to50-55" to " 31 B. 3X)

+X- 20X corderierite20X biotite2X -3X garnet (euhedral)3X - 5X muscoviteQts recrystallised

3.3 - 2 cm carb vein

11.2 - 11.5 - shearedchlorite slip plane (sone) at 45"

21.3 - 21.5 - Buscovite rich felsic dyke at 45"

26.0 - 26.7 - massive f.g. int/gabbro dyke at 40"

Mottled fg At " 31 m - gradational grey to change over l - 2 ra into and ng siliceous (silicified) .OFF white massive to moderately

foliated at 50 0 Commonly t 25X QTZ eyes

31.4 - 32.1 - pink stainedfeld. phyric (7X) int. dykedyke at 45"Massive pink/white graniticpegmatite dyke tind clots at32.G - 32.732.9 - 33.334.1 - 34.534.8 - 34.935.0 - 35.6

Shear sone

Generally weak .3^..2X - 4X biotiteIX - 4X muscoviteQts has Milky look to it

2X Diss. Py Silicification probably due to numerous gran itic dykes.

35.1 - 35.5 green epidote stained.

36.3 - 3G.4

HOLE HO: UL-27 LOGGED BY: S.C. SIM

DRILL HOLE LOG

PROM 10

ROCK TYPE

GRAIN COLOUR SIZE TEXTURE AND STRUCTURE

ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS

0.8 to179.3 cont'd

green/

and white

36.5 - 36.837.3 - 37.537.6 - 38.2

fg 41.1 - 42.7 - Massive Int/ gabbroic dyke, same as 26.0 at 15"

49.4 - 50.0 - 602 graniticclots over section at "50"

Green/grey chloritic aaficdykes at50.4 - 5 cm50.7 - 50.9 at 45 s51.2 - 5 cm

52.7 - 52.9 - Granitic dyke 6 50"

53.3 - 53.6 - Rotten, grungychlorite/carbonate healedfault at 35 0

55.7 - 57.1 - Several chlor itic patches similar to above over section.57.1 - 57.1 - Carb/chlorite partially healed fault sone B 35"

57.8 - 58.1 - Very blocky chloritic fault sone at 40"

Granitic clots at: 62.2 - 5 cm 62.4 - 62.5 S2.7 - 62.8

63.1 - 63.9 - Massive grey,f.9. int. dyke at 60"

Healed fault

Fault

Fault

9

9HOLE NO: UL-27 LOGGED BY:R. c. SIM PAGE: 3

DRILL HOLE LOG

O

C

.' - l

C

c

r

r

r

r

FROM 10

ROCK TYPE COLOUR

Hue/ grey

GFJAIN SIZE

fs

TEXTURE AND STRUCTURE

Gradational change from 74 - 75 n) to more altered QFP

ANGLE TO CORE AXIS ALTERATION

Increase alt. to: )' 20X. cord." 3X biotite

SULPHIDES REMARKS

Dark fg 81.1 - 83.5 - Massive f.3.green/ int/gabbroic dykegrey Sharp contacts at 50"

84.9 - 85.8 - M.9. gradingto f.g. at 85.5, massiveint. dyke at 50"

Mottled mg At 85.8 - QFP becomes weak 3rey/ to unaltered, massive with white cloudy GIZ eyes and feld- with spars K 4 rum) in f.g. matrix pinktinge 88.7 - 88.9 - 60X pyritic

clots over section

Variable var- 89.2 - 99.4 - Granitic and iable intermediate dyke swarm in

pink stained very weak to unaltered QFP

Grey fg 89.2 - 93.0 Massive int. dyke with 30X granitic pegmatite clots and dykes Sharp contacts on dyke at 55 0

Similar interned, dykes at: 93.4 - 93.5; 93.7 - 94.2 96.1 - 97.4; 97.9 - 98.3; 98.5 - 99.4: All separated or containing xenoliths (?) of unaltered QFP

2X anhedral garnets (commonly sones of pink sugary garnetiferous web enveloping Qts grains) - occasional fibrous texture noted.

Up to 2X biotite Rare trace garnet cut by numerous granitic veins, dykes and clots.

Trace - IX fine diss. pyrite

fine diss. magnetite

IX - 2X diss. pyIX - 2X magnetiteRare trace diss. cp.

89.2 - 99.4 Dyke swarm

*

c

e

0

9

f

HOLE NO: UL-27 LOGGED BY: R. C. SIM PAGE: 4

DRILL HOLE LOG

FROM ROCK TO TYPE

0.9 to 179.3 cont'd


Granitic dykes at 101.6 - 101. S 103.5 - 103.9

Fg massive magnetic inter mediate dykes at: 103.9 - 104.7 at 105.7 - 105.9 107.7 - 108.0 at 109.5 - 109.6 at


55"

60 0 50"

*9mg

109.9 - 110.4

112.5 - 113.6 - Pink/orange granitic/syenitie dyke at

Massive

50 0

At * 110 ut magnetite is gone in QFP

At " 115 DI QFP noderatelyaltered:* 30X cordierite10Z biotiteLocalized O - 3X garnetTrace -2X muscovite

118.2 - 118.6 -Eg massive chloritic mafic dyke at

Salt eg 119.0 - 121.5 - Ueak foli-and ated grandiorite dyke withpepper sharp contacts at

122.7 - 123.0 and 124.3 -124.5 - Fg massive gabbroicdykes.Sharp contacts at

125-2 - 126.2 - Massive fg feldpyhyric int. dyke at Irreqijlar granitic clot at 125.6 - 125.7

60'

SO 0

50" 60*

55"

2X -3X biotite

HOLE NO: WL-27 LOGGED BY: R. C. SIM PAGE: 5

UK ILL HOLE LOG

o

t

o

FROM ROCK GRAIN ANGLE TO 10 TYPE COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

0.3 to 175.3 coni 'd

126.4 - 126. S - Granitic /pegmatite dyke at

126.3 - 127.2 - Magnetic chlorite int/nsafic dyke at 127.2 - 127,5 - Granitic/ peg, dyke, same as 126.4 at

55"

60"

"60"

9

•9

128.5 - 128.7 - Granodior- itic dyke at

Pink and white granitic pegmatite dykes at: 131.6 - 131.7 132.7 - 133.0

135.3 - 135.4 - White QTZ vein with irregular contacts

Well foliated at

SO"

55"- 60"

144.1 - 144.2 - Well foli ated weakly chloritic int/ afic dyke at

149.7 - 150.1 - Pink and white grantic/peginatite dyke at

60 0

148.5 - 3 cm possible shearnone (.7) carbonate rich at 50"

At * 138.0 gradationalincrease in alterationin QFP to:502 cordierite10* - 15X biotite5X muscovite (locallyup to 10Z)Patchy garnet, trace -3X

Rare trace diss. Py.

60"

HOLE HO: UL-27 LOGGED BY: R. C. SIM PAGE: b

DRILL HOLE LOG

FROM 10

ROCKTYPE COLOUR

GRAIN SIZE TEXTURE AND STRUCTURE


0.8 to179.3 cont'd

150.1 - 150.6 - Yery wellfoliated zone in QFP.QTZ eyes stretched at 60 0

151.0 - 152.5 - 10X grani tic clots and veins over section.

152.8 - 153.3 - Well foli ated f.g. chloritic mafic dyke. Sharp contacts at 55"

Muscovite rich (3X -7X) granitic to granodiorite dykes at:153.3 - 153.6 at 55" 153.8 - 154.1 at 50" 154.7 - 155.6 at 50"

156.6 - 157.9 Fg moderatelyfoliated chloritic maficdyke, same as 152.8 at 60"

Similar dyke at166.3 - 166.9 at 60"

170.7 - 170.8 - Granodio-ritic dyke at 60 0

174.5 - 174.9 - Massive fg gabbroic dyke at 55-60"

Conmonly IX -3X Py in granite

179.3 GABBROto285.9

Greenwithwhitsspots

mg Generally massive tolocally weak/moderatelyfoliated at

IX QTZ - QTZ/carb veining(< 1 cm)

55-60"

Trace diss. pyrite.

Sharp upper contact (no chill) at 55 0

HOLE NO: UL-27 LOGGED BY:R. c. SIM PAGE: 7

DRILL HOLE LOG

FROMTO

ROCK TYPE COLOUR


ANGLE 10 CORE AXIS ALTERATION SULPHIDES REMARKS

179.3 to235.9 cont'd

181.5 - 183.1 - Wellfoliated f.g. int. dykeSharp contacts at 45"

185.1 - 185.3 - Int dykesame as above at 45"

189.3 - 189.4 Int dyke at 45"189.4 - 189.5 Irregular QTZ vein

Fg, moderate to well foli ated intermediate dykes, sane as 181.5 at: 195.0 - 195.6 at 50' 197.4 - 198.9 at 65" 199.8 - 201.0 at 55"

202.0 - 202.4 - Numerousfractures over sectionalong QlZ/carb/hem veins at *30 C

202.9 - 203.0 - Hematiterich QTZ/carb vein at 55"

204.4 - 204.7 - Fg massive int. dyke very blocky and grungy over top 0.15 n. Possible fault at 30"

205.4 - 205.5 - Fractures along QTZ/carb/hem veins, same as 202.0 at *40 0

Similar fractured zone at213.3 - 213.5 at 35"

184.1 - 184.8 - 5X py, IX Cp in clots and veins associated with chlorite and quartz veining.

3X Py fro* 185.3 - 185.5 in vein and clots similar to above.

Fault ?

HOLE NO: UL-27 LOGGED BY: R. C. SIM

DRILL HOLE LOG

FROM 10

ROCKim COLOUR



179.3to285.9

213.9 - 214.2 - Massivegranitic/granodioriticdyke at 45"

216.2 - 3 em GTZ/carb/hen/vein/vug similar to 202.9at 25"

218.3 - 218.8 - Granitic/granodiorite dyke, saneas 213.9 at 50"10 cm int. dyke in graniteat 218.6

221.1 - 221.4 - f.g int.dyke at 55"

pink ng 227.5 - 230.4 -Moderate to and well foliated granitic dyke.white Sharp contacts at 55-60"

Gabbro xenolith/dykeat 229.5 - 229.7 st 55-60"

231.0 - 231.2 - Eg int/wafic dyke. Sharp contacts at 60"

Granitic dykes, sane as 227.5 at 232.5 - 232.7 233.0 - 233.6 (40X intercolated intermediate dyke material )

235.4 - 235.7: Blocky, grungy chlorite/carbonate rich fault zone 'at "45 0

236.1 - 236.6 - Chlorite/cart. rich sone similar to above but less blocky.

Fault

Fault?

LOGGED Bt: R. C, SIM PAGE:

e t

DRILL HOLE LOG

FfcOM 10

179.3 to 285.9

ROCK TYPE

GRAIN ANGLE TO COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION

237.8 - 239.0 - Fg tiassive int/gabbroic dyke. Contacts 8 GO 8

SULPHIDES REMARKS

239.3 - 239.5 - Siliceousbanded (crude) zone in gabbro l? 55"

Massive fs int. dykes at247.7 - 248.3 at 50"249.5 - 250.1 at 55"

250.1 - 251.7 - Graniticdyke similar to 227.5 at 50'

252.1 - 252.3 - Composite int. dyke with 40X granitic clots, contacts at 50"

252.6 - 253.3 Weak foliated int. dyke. Sharp cont's,top B 15'

bottom 8 35" 253.3-256.5:

Pink i mg Massive to locally uk. fol. white granitic dyke. Sharp con

tacts, top e 1 5" bottom 8 35"

256.5 - 257.3 - Fg int. dyke same as 252.6 at 50" 20 cm carb/chlorite part ially healed fault zone at 256.9 at "45"

258.8 - 259.5 - Eg weakly feldphyric int dyke at 65" also at 259.8 - 260.0 and 260.1 - 260.3 at 50"

260.3 - 260.8 Weak foliated int. dyke yith 7 '/. white rounded feldspar clots/pheno -crysts. Sharp contacts at 60"

22 -3X pyrite disseminated and in small clots.

3X muscovite

Fault

HOLE NO: WL-27 LOGGED BY: R. C. SIM PAGE: 10

DRILL HOLE LOG

FROM ROCKTO TYPE

179.3to285.9cont'd

GRAINCOLOUR SIZE TEXTURE AND STRUCTURE

262.5 - 264.1 - Chlorite,hematite, carbonate richslickensided fault soneatVery blocky.

ANGLE TOCORE AXIS ALTERATION

"50"

SULPHIDES REMARKS

Fault

266.4 - 267.7 - Fg massiveint. dyke with 202 gabbroicfragments.Contacts sharp at 50"

268.1 - 268.3 - Siliceousgranitic dyke at 60-65"

Well foliated bleachedintermediate dykes at276.0 - 276.2 and277.4 - 277.6 45"

278.9 - 5 cm carbonate rich vein/vug

279.5 - 280.9 - Weak foli ated fg int. dyke. Sharp contacts at 50"

282.7 - 282.8 - Well foli ated int. dyke, same as 276.0 at 50'

Associated int. dyking and granitic dyking at 283.7 - 283.8 284.0 - 284.2 284.5 - 5 cm 285.3 - 285.5

At 268.3 - Trace phlogpite begins occurring in gabbro increasing to 4X average at 273 M.

5X molybdenite

2X garnet in grardteO

e

e

Q

9

HOLE NO: UL-27 LOGGED EY: R. C. SIM PAGE:il

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



284.2 - 285.9 - Well foliated feldphyric (4X) intermediate dyke with 15X stretched chloritic mafic clots K l cm)

60"

285.9to267.9

287.9to331.0

TRANS ITIONZONEGABBRO

META-PERIDO-TIIE

Mottledgreenandbrown

Steelblue/grey

eg

mg- eg

Typical massive chloriticamphibole rich ultra-maficunit - no visible feldspar

Typical massive magnetiterich (+25X) ultramafic unit.Upper contact marked byinflux of magnetite

Locally up to 5X biotite Noneclots

295.7 - 298.9 - Pervasivebiotite zone with numerousshears along cleavage planesat 55-60"Contacts gradational intoP:;.Core angles crenulatedlocally to O" to C.A.

306.3 - 306.6 - Very blocky slickensided chloritic core. Fault Zone at "50"

310.8 - 312.6 - Massive, fg weak feldphyric (3X) inter mediate dyke. Blocky upper contact and very blocky and grungy from:312.3 - 312.6 - Fault Zone at "55"

Possible 'baked 1 Xenolith of volcanics in sill (?). Seen in many other holes in Pick Lake sill. (May be fault zone (?) Note: Flattening wedge at 297 m.

Fault

Fault

Mottledlight Sdark grey

fgtomg

312.6 - 315.7 - Very brokenand blocky altered zone.Possibly a faulted GFPxenolith?

25X biotite Fault25?. cordierite

HOLE NO: UL-27 LOGGED BY: R.C. SIM PAGE: 12

DRILL HOLE LOG

BROH 10

SOCKTYPE COLOUR



318.0 Flattening wedge287.9to331.0

Very blocky with numerous slickenside? at 55-60" - Non magnetic

319.3 - 319.7 - Fg massive int/mafic dyke with sharp contacts at 50 C

320.6 - 320.8 - Massive siliceous granitic dyke at 85"

320.8 - 321.4 - Massive fgdyke sinilar to 319.3 at 60'

tx grades into a weak to noderate foliated, none nagnetic gabbroic chill at 326.9 tt.

327.0 - 327.1 and 330.8 -330.9 - massive graniticto granodiorite dykes at 50-60"

331.0to402.1

OFF Greywithlightgreyspots,oftenpink.stained

mg Massive to weak foliated defined by slightly flattend Q1Z eyes (15Z- 20X) at 60"

332.2 - 332.8 - Weak foli ated mg granitic dyke at 60"

332.8 - 333.5 - Massive fg intermediate dyke at *60"

Ueak altered, very rarevisible feldspar, * 10XcordieriteIX -3X biotite, highlygranitic (pink) stainedto " 355 ai

Very rare trace pyrite.

HOLE NO: U l-27 LOGGED BY: R. C. SIM PAGE: 13

DRILL HOLE LOG

FROM ROCK 10 TYPE

331.0 to 402.1 cont'd

GRAIN ANGLE 10 COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION

334.1 - 334.4 - Broken zone with fractures related to QlZ/carb/hem veins and vugs containing euhedral xlls of (Hz, calcite and pyrite (3X)

SULPHIDES REMARKS

335.2 - 335.4 - Massivemg syenitic dykes at 45"

337.7 - 337.8 - Massivefg int. dyke at 60"

Pink and white e.g. granitic pegmatites at337.8 - 338.2 at 45" 338.4 - 338.5 at * 80"

342.3 - 343.5 - Massivefeld. phyric (52) inter-uediate dyke.Sharp contacts at 50"

354.3 - 355.5 - Fg massive weak feld. phyric (2X) int. dyke, similar to 342.3 at 55"

339.5 - 340.3 - 10Z QTZ /carb veins over section -highly pink stained QFP

Magnetite begins occur ring in OFF at 347 m increasing to locally 2 X in rounded blebs K l um)

O -2X (locally) muscovite beqins at 356 a .

362.5 - 362.6 - Graniticdyke at 50"

365.4 - 365.8 - Highlycarbonate veined andclotted granitic dyke,Sharp contacts at 70"

HOLE NO: WL-27 LOGGED EY: R. C. SIM PAGE: 14

DRILL HOLE LOG

FROM ROCK 10 TYPE

331.0 to 402.1 eont'd

GRAIN COLOUR SIZE TEXTURE AND

371.2 - 371.9 f 9 int. dyke

372.4 - 372.5 dyke at

STRUCTURE

- Massive at

- Granitic


50"

65 0

SULPHIDES REMARKS

402.1 SILICEOUS Dark to GARNET- blue/ 574.3 IFESOUS grey

ALTERED with SEDIMENTS pink

spots

119to

378.6 - 378.8 - Pinkstained QIZ vein at 70"

378.9 - 379.1 - Graniticdyke at *70"

380.8 - 381.5 - Fg massiveint. dyke, sharp contacts at 65"

387.8 - 388.0 - Graniticdyke at *45 0

391.5 - 392.4 - Massive feld. phyric int. dyke, sharp contacts at 65"

397.7 - 399.0 - Blocky corewith fractures along QIZ/carb veins.3 cm grungy at 398.0 H at 30"

Typically massive tonoderately foliated 8 60-65"defined by siliceous bands(rims about garnets) orlocallised chloritic/amphibole clots(locallised up to 7X)

Alteration in QFP hasgradually increased,at 378 nt 355! cordierite2X - 55! biotiteIX - 4X MuscoviteNo visible feldspars

Patchy pink stained

Typically 3-10X garnets -Ocm +X- silica rims in fg-mg mass of biotite (20X), cord ierite aOX i qts Numerous qts veinlets i clots Ocii throughout Top In pervasive bio/cord.

Possible fault ?

Generally 1-2X pyrite, 1 7. p o with rare tr cp disseminated or note commonly in chloritic clots or qts veins (locally up to 4X py, 2X po over 10cm sections). Patchy 1-2X mag netite in rounded blebs t2am

ft

ft

ft

ft

Q

HOLE NO: WL-27 LOGGED 6Y: R.C.SIM PAGE:

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



404.0-404.5:Qtz S chlorite healedbreccia zone,

405.7-405.8:Epidote bleached int/ afic dyke 6

408.5-409.0: Irregular qtz dyke with 207. injested sediment fragments.

410.8-410.9:Pink t white graniticpegmatite dyke S

411.5-412.1:Altered intermediate dyke Hassive, fg with sharp contacts 6

413.4: 7cm garnetiferousOX) granodiorite dyke 8

60"

'80"

75'

65"

416.4-416.5: Granitic dyke U

1.5 x 3csi pyrite clot at lower contact containing 2 angular purple sphalerite fragments 4?)

Pink stained for 10cm Q upper contact.

15X cordierite 3Z biotite U anthophyllite

6 * 413m: Light green feathery wisps of antho phyllite begin occurring in seds. Avg: 3X over section

75"417.1: 2cw x Sem banded fragment with 30X pyrite interbanded with anthophyllite rich siliceous bands on 3mm scale.

HOLE WL-27 LOGGED BY: R.C.SIM PAGE: is

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



426.4-426.5: Composite garnetiferous granodiorite dyke cut by 4cm qts vein l?

432.1-432.5 t434.8-435.3:Massive to weak foliatedfg int/nafic dykes.Sharp contacts 8

436.4: 7cm garnetiferous granodiorite dyke U

441.7-442.1:Massive fg feld. phyric(4X) int. dyke 6

70"

55"

446.9-447.0:60X irregular qtzclotting over section.

448.4-448.8:Eeld. phyric (7X) int.dyke, sharp contacts 8

452.1: lOcta garnetiferous granodiorite dyke S

452.7-453.0:hassive fg int/mafic dyke fi

444.0-444.8:Intense biotite developed over section (40X) with 15X garnet.

444.8-445.9:Gradational sone over 10cm of less altered, sassive, fg, 'intermediate 1 sedinents.

70"

60"

75"

HOLE NO: WL-27 LOGGED BY: R.C.SIM PAGE: 17

DRILL HOLE LOG

FROM10

ROCK TYPE


White qts veins B 453.0-453.2 8 456.2-456.3 6


60" 40"

SULPHIDES REMARKS

Dark 199 459.2-464.4:green to Major gabbroic dyke.with fg Upper contact not verywhite distinct due to bleaching.spots Typically noderately

foliated equigranular gabbro t? 65"

460.2-460.8: Biotite/cordierite rich xenolith of sediments in GB.

461.8: 3cn qts vein withbiotite rich halo for Seeabove and below.Lower contact sharp at464.4 8 65 0

469.4: lOcni Qb dyke 8 65 0

477.4: 5cm granitic dyke 8 50"

483.4-483.7:Granitic pegmatite dyke l?

458.2-459.21Gradational pervasive cord/ bio/anth altered zone of sediments, bottom 0.2m contains 20X light brown blades of anthophyllite up to 2ca.

Ir garnet over top 0.3m (due to contamination)

479.0! lOcoi sone with 15X pyrite clots

25" 52 carbonate veining


DRILL HOLE LOG

J

J

J

J

J

FROM 10

ROCK TYPE COLOUR



484.4-484.9 i485.4-486.0:Massive fg int/aiafic dykesSharp contacts 8Sedimentary xenolithat 484.5-484.6

485.1-485.4: Well banded section of sediments on am scale, locally folded i crenulated from

55 s

60-10 0

Unaltered

Host altered to cordierite in l-2mn) halo about vein

493.5-493.6: Mafic dyke Q

8 " 495m: well developed silica rims enveloping garnets 8

75"

70-75"

None

487.5: ICB zone with 25X vein type sulphides in discontinuous band at 65" to CAIX cp3X po2X py

19X sphalerite

Possibly a poorly developed tuff ?

488.9-489.0:5X po veins over(IX py, tr cp)

section

12X gnt 10X biotite

+40X cordierite IX anthophyllite

497.4-498.3!Biotite rich zone envelopingeuhedral garnets Klcra)over section:30X biotite42 anthophyllite

20X garnet +40X cordierite

Localized clots of sulphides often associated with garnets (IX py, 2X po)

Ir diss py.

t

J

J


r

DRILL HOLE LOG

FROM 10

ROCK TYPE



500.6-502.1 S503.2-503.6:Hoderate to well foliated 8 75 0Intermediate to gabbroicdykes.Sharp contacts S 70"

506.4: 7cm msucovite rich(10X) qts vein S 5 5 6

Eg massive to weak foliated S 75" 507.7-519.9:Gradstional zone of garnet poor sediments more 'intermediate sedimentary* in appearance. 15* biotite 40X cordierite 3X anthophyllite in wispy

clotsAvg. 3X garnet in localized zones.

506.7-506.85:5X sulphide clots S veinsover section3X po, IX py, IX cp.

1.5cH vein 6 506.85 contains wispy banded sulphides on nn scale but is enveloped in qtz - probable vein.

IX po, IX py in localized patches associated with garnets

517.8: 15cm garnet rich sone with 5X po streaks S clots (IX py, tr cp)


DRILL HOLE LOG

FROM ROCK 10 TYF'E

GRAIN COLOUR SIZE

Dark qrey fg with whiteSpots

ANGLE 10 TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES

519.9-523.2: 1 7. m agnetite Massive to locally foliated defined by amphibole* - feld. phyric (5X) intermediate dyke. Sharp contacts (? 60 C

REMARKS

C

t

t

w

w

t

t

523.2: BacK into typicalsiliceous garnet alteredsediments7-10X garnet (+X- silica

rims)+40X cordierite 10X biotite 1-2X anthophyllite Localized sillimanite wisps (up to 2X)

IX po, IX py in clots

525.4-525.9:Bleached intermediate dyke. Fg, moderately foliated with sharp contacts 8

530.6-532.2: Massive fg weakly feld. phyric (3X) intermediate dyke. Sharp contacts e

c

t

c

c

c

c

t

e

t

t

t

75"

60"

538.5-539.5: Patchy pink granitic staining of silica rims. Rare garnets retrograded to qts 8 chlorite.

541.3-542.l: 50X irregular qta clots over section commonly containing 10X garnet.


w

t

DRILL HOLE LOG

PROM 10

ROCK TYPE COLOUR



543.5: 10cm garnet richqts patch, sililar to above.

542.2-542.4:1-2X granular honey colouredstaurolite over section.

543.0-545.0: 157. wispy banded antho phyllite over section

Hatrix very cordierite rich 544.4-544.7: 5X po, IX py, tr cp. in dendritic veins S clots " parallel to foliation S 75" to CA

Darkgreenwhite

545.7-547.6:Massive gabbroic dyke,sharp contacts S

Below 548m, sediments become generally nore massive uith garnets commonly not enveloped with silica.

550.5-553.0:20X section composed ofbiotite/anth. rich sonesenveloping qts clots or"wormy 1 folded qts veinsaero.

Garnetiferous granitic dykes 0 554.7-554.8

557.7 - 4cm 558.4 - Sen 559.5-559.6 5&0.1-560.2

75"localised pyrite veinlets

HOLE NO: UL-27 LOGGED EY: R.C.SIM PAGE:

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



D .3 r kgreen/greywithwhitespots

C

c

c

c

c

c

c

t

l

t

560.9-561.5:Weak foliated fg weaklyfeld. phyric (2X) int.dyke, contacts 8 60"

fg 565.2-567.3:Highly feld. phyric (15X)weak foliated intermediatedyke 6 75'

Green, fg weak foliatedchloritic nafic dykesat: 567.7-567.8 8 75"

569.3-570.3 8 70" 570.5-570.6 8 65"

572.6-572.7:Garnetiferous graniticdyke 8 50"

2X magnetite in sediments begins 8 558m.

574.3 ALTERED Mottled fg to 'INTER- blue/ to 638.2 MEDIATE 1 grey mg

SEDIMENTS

Generally massive equigran ular altered greywacke (?) to locally weakly siliceous banded often with ninor associated garnets. Upper contact gradational over meters.

579.3-579.5! Garnetiferous granitic dyke 8

Similar dykes/veins at: 582.9 - 10cm 584.5 - 6cm 586.2-586.3

70-75 0

85"

Variable, but generally highly altered to bio/cord/ anth */- gnt assemblage. 10-15X biotite 3-7X anthophyllite +40X cordierite Up to 32 garnet

Rare localized veinlets of pyrite

2X pyrite clots

HOLE NO: UL-27 LOGGED BY: R.C.SIM PAGE: 23

i C

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



593.5-601.5:20X section composed ofsilica rimmed 3arnet richaat'l similar to siliceousgarnet altered sedimentsabove.Contacts gradational.

598.5-598.8:Locally crenulsted antho phyllite wisps i bands.

600.0-600.05: 3'/, pyrite veinlets i disseminated parallel to foliation direction.

602.5-604.0: Very blocky ground. Locally chloritic with rare slickensides

605.3-606.1:Blocky ground with 2cnchloritic grunge at 605.5 8

Fink S white granitic dykes/veins at:

610.0 - 4cm611.5 - 5cm612.2-612.9 8

Fault zone

8 604: rare silica r ins are pink stained S envelope retrograded garnets (qtz t chlorite)

Fault45"

75 s

625.0-631.0:7X garnets over section inbands, often no silica rims.

HOLE NO: UL-27 LOGGED BY: R.C,SIM PAGE:

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



632.6-633.2:Feld. phyric int. dyke 0 70 C

633.5-633.6: Weakly garnetiferous granodiorite dyke. Irregular contacts.

635.0-635.3:Int. dyke, sane as above 8 75"

l

l

t

639.2to667.1

INIER- COLATED SEDIMENTS, TUFFS i RHYOLITE FLOWS (?)

Variable Var- Biotite altered banded iable (tuffaceous) zones comiionly

mineralised gradins over 1-lOcB to nore Massive weak altered sediments. Localized zones of moderately foliated, 1119. black l white weak altered OFF (?) flows are also present (details below).

639.2-639.5!Biotite rich banded zone bordered by 5cm intermediate dyke aat'l at top 8 bottom 8 70*

639.5-639.9: Hell banded mineralized tuffaceous zone on l-5ma scale S 80"

Intense biotite/ cordierite alteration of selective (more mafic) bands

4X po, IX py, tr cp i sphalerite in disseminated i discontinuous bands.

639.9-641.0: Weak altered nassive intermediate sedimentary niat'l - Sen granodiorite dyke at 640.1


i* DRILL HOLE LOG

FROM10

ROCK TYPE COLOUR



641.0-641.4:Well banded tuffaceous zonesimilar to 639.5Banding locally 'bends'around re-crystallisedqtz fragments.

641.4-642.0:Locally banded mainlysedimentary mat'l.

642.0-642.4: Composite granodiorite- qts dyke with irregular biotite rich contacts.

642.4-642.8: Massive weak altered sediments

642.8-643.8:Banded zone, highly altered. Cut by irregular grano diorite dyke at 643.1-643.3

643.8-644.4:Moderately foliated weakly feld. phyric intermediate dyke. Sharp contacts 8

644.4-647.0:Massive to locally banded/foliated intercolated tuffS sediments SBlocky biotite rich faultat 645.1-645.3 B

75"

75"

70"

20X banded biotite oversection

+30X cordierite 2X anhedral garnets in

localized bands

2Z localised garnets

4X garnet in qtz rich zone or dyke

Cut by 5* qtz veins Ocm

40X biotite bands 5X garnet

32 po, IX py in disseminated bands

2X po in chloritic veinlets

3X diss po.

153! biotite over section 3X anthophyllite Locally 2X garnet

Fault

HOLE NO: UL-27 LOGGED BY: R.C.SIM PAGE:

DRILL HOLE LOG

FROM 10

ROCKTYPE COLOUR



C

C

t

Salt l pepper

Salt S pepper

113

Big to eg

"647.0-'648.9:Gradational more siliceousnone possibly representinga rhyolitic (OFF) flow.US, moderately foliated (J 70"

648.9-650.1:Intercepted sedimentsi tuffaceous mat'l cutby feld. phyric int.dyke at 649.5-649.7 e 65"

650.1-653.6:Well foliated equigranularrhyolitic (QFP) flow.15X flattened qtz eyes.Upper contact gradational,lower sharp 8 80 e

653.6-660.1:Intercolated banded tuff S massive sediments, also locally snail ^Octo 1113 QFP (?) flows (6.9. 657.5- 657.6 l 657.7-657.9)

Eeld. phyric int/mafic dykes at: 654.6-654.9

655.7-655.8657.5-657.6

660.1-662.4:Weak to moderately foliatedQEP flow. Gradational uppercontact, sharp lower 8 75 0Massive int/niafic dykeat 661.8-661.9 8 55"

WeaK altered, 5X biotite over section

7X biotite over section 15X cordierite

Ir diss py S po

IX diss po, tr diss py.

Possible QFP

Patchy altered, locally Ir diss py S po. 5X cloudy visible feldspars 5X biotite over section Locally up to lOX

Patchy, banded mat'l 2X po, IX py disseminated connonly contains 7X biotite

QFP i.

5X biotite10X cordieriteIX anthophyllite

Ir diss py \ po. QFP ?

C

c

c

t

HOLE NO: UL-27 LOGGED BY: fi.C.SIM PAGE: 27

DRILL HOLE LOG

FROM 10

ROCKms COLOUR


ANGLE TO CORE AXIS ALTERATION SULPHIDES

ID! diss py S po.

REMARKS

662.4-664.3:Intercalated biotite altered banded tuff i massive sediments cut by granitic dyke at 664.0-664.2

664.3-664.5:Int/mafic dyke 8 75"

664.5-664.8:Well foliated weak alteredGFP dyke/flow l? 75"

664.8-667.0:Generally massive fg sed iments with minor banded tuffaceous component

665.5-665.8:Feld. phyric int. dyke 8 80"

667.0-667.1:Granodiorite dyke 8 "80"

2X py, IX po diss S in clots

QFP

po, IX py disseminated

667.1 ALTERED Mottled to BANDED grey S 667.85 TUFFACEOUS white

VOLCANIC(CLR)

Mottled to well banded on .5-lcm scale 8

Intense biotite/cord 80" alteration of selective

bands separated by milky siliceous bands

27. py, IX po disseminated to 667.85

667.2: 5cm zone with 32 euhedral magnetite Klmm)

Locally looks like altered CLR

667.85 MASSIVE to SULPHIDES 663.45

Brassybrownwithwhitespots

fg Massive sulphides to supporting 12X rounded

668.2 re-crystallised chert niq-cg fragments (avg. 2-3niin,up to

2cm). Sharp upper contact 8

One 2cm biotite/cord rich fagment 6 lower contact

to 668.

65"

3X wispy to clotted cp.27. pyrite cubes U2mm)

40X sphalerite mixed with 43X pyrrhotite

Est. IX Cu__20X,Zn 0.60 m CL

45668.0-668.08:Weak banded altered CLR frag ment/bed. Sharp upper contact B 50" Irregular lower. Gradation at 668.2 to mq sulphides into cq at 668.35


DRILL HOLE LOG

FROM ROCK10 TYPE

668.45 GRANO-to IHORIIE668.65 DYKE

COLOUR

Salt Spepper

GRAINSIZE

mgtoeg

ANGLE 10TEXTURE AND STRUCTURE CORE AXIS ALTERATION

Massive irregular siliceousdyke, contacts veryirregular.

SULPHIDES

5X po, tr-lX cp in irregularveinlets (dendritic) throughout

REMARKS

to MINERAL- to banded 692.2 IZED grey i

TUFFACEOUS whiteVOLCANICfCLR)

668.65 ALTERED, Mottled fg Mottled to locally wellbanded matrix altered volcaniclastic 8

671.5: 2cm biotite rich grungy fault 9

671,8-672.0:Feld. phyric int/iuaficdyke

l? " 673.Sn: banding becomes less evident, tuff has settled/ banded texture S

Banded intense biotite to 673.5 (avg. 10X over

75-80" section) * 30X cord.

80"

80"

80"

5X fg biotite +20X cordierite

2'/. po, 21. p y in disseminated bands to " 673.5

eq of altered CLR l?'669.5m

Fault

Mainly po (avg. 3-43O in discontinuous bands Hum i disseminated (locally up to 6X over 20cm sections) (tr-lX pyrite)

676.8-678.3: Feld. phyric int/mafic dyke. Sharp contacts 8 10cm granodiorite dyke at 677.7

677.9-678.0:Chlorite healed brecciazone,

75"

J

A

J

678.3 - 3cm l678.5-679.2:Granitic pegmatite dykes e "80"

Similar dyke at 681.6-681.8 5X muscovite flakes

683.3-683.4: Mafic dyke 8 70"

5 x 3mm moly clot @ 678.6m

UL-27 LOGGED BY: R.C.SIM PAGE:

DRILL HOLE LOG

FROM TO

SOCK TYPE COLOUR



683.4-683.9:Massive, mg granodioritedyke, irregular contacts

685.7-685.8: Granitic dyke 8

686.3-686.6:Granodiorite dyke, similarto above, but mineralized.

689.7-690.2: Feld. phyric int. dyke, fg, massive, with sharp contacts 0

691.5-691.6 l 692.0-692.2: Granodiorite dykes, irre3ular contacts.

2Z garnet

65 s

3X clots Klrnm) po, several aoly clots ^mro associated with sulphide veinlet at 686.55

80"Garnets begin occurring at 691m.

692.2 GARNET- Grey to IFEROUS with 697.3 SEDIMENTS pink

spots

fg Generally massive with weak foliation defined by biotite wisps S 80"

694.8-694.9:Int. dyke 8 80"

102 biotite in wispy bands(avg. ^nii)+40X cordierite5X garnet K5nm) with raresilica r ins

2X py, 2 7. p o in disseminated bands

697.3 ALTERED ..Blue/grey fg to INTER- with 702.1 MEDIATE black

SEDIMENTS streaksWITHTUFFACEOUSCOMHPONENT

Generally massive with biotite wisps locally moderately banded, upper contact marked by loss of garnets.

698.6-698.7: Irregular Syenodiorite dyke.

10X biotite +40X cordierite

2X py, IX po in disseminated clots i bands

Same as garnet unit above, but with no garnets.


DRILL HOLE LOG

FROM 10

702.1 to 708.0

ROCK TYPE

MULTIPLE PHASE RAINBOU' GRANITE

GRAIN t COLOUR SIZE TEXTURE AND STRUCTURE C

699.1-700.0: Pink l white massive 193 granitic dyke B

Variable Gen- Sharp upper contact 0 erally with 20cm fg grey granite

mg grading to mg mat'l, well foliated grey granite.

INGLE TO ;ORE AXIS ALTERATION SULPHIDES REMARKS

55'

75"

E.O.H.

706.0-706.6 i 707.0-707.4: Pegmatite dykes 8

10cm epidote at 706.5-706.6

End of Hole.

HOLE NO: WL-27 LOGGED BY! R.C.SIM PAGE: 31

GEOCHEM AND ASSAY SHEET

SampleNumber

US07110712071307140715

07160717071807190720

07210722072307240725

07260727072307290730

07310732

SampleNumber

Cm)From

6.045.075.0

105.0135.0

168.0336.0366.0393.0405.0

435.0465.0495.0510.0540.0

571.0579.0609.0639.0650.6

672.0693.0

(u)From

(m)lo

9."0

48.078.0

108.0138.0

171.0339.0369.0396.0408.0

438.0468.0498.0513.0543.0

574.0582.0612.0642.0653.6

675.0696.0

(nilTo

EstinateCu Zn Py

2211

tr

tr,---

trtr -- 2

tr -- 221

1

1-.

12

12

EstimateCu Zn Py

Po

-- --

---- 1

112

--1

1 --1

32

Po

(DI)Length

3.03.03.03.03.0

3.03.03.03.03.0

3.03.03.03.03.0

3.03.03.03.03.0

3.03.0

(DI)length

ppnCu

78104

276

2473

28

5026573

25

843

744

13123

XCu

ppmZn

157B3

280293180

50303543

225

13413029510465

883032

23630

30100

ZZn

ppbAu

76897

76866

87657

66586

510

gin/tAg

H

03033

04433

31302

24224

22

9

Za20

.43

.38. 22.81.21

.93

.21

.23

.59

.10

.47

.96

.11

.77

.36

.24

.28

.80

.96

.47

.34

.95

m/tAu

Comments

QFPQFPQFPQFPQFP

QEPQFPQFPQFPSil, gnt, alt. seds.

SGSSGSSGSInt. seds.SGS

SGSInt. seds.Int. seds.Alt. tuff * seds.QFP ?

Alt. CLRGnt, alt. seds.

Comments

9

e

0733 667.85 668.45 1.0 20.0 2 43 0.6 1.71 20.96 52.0 0.13 MS

HOLE NO: UL-27 PAGE:

GEOCHEM AND ASSAY SHEET

Sample (m) Number From

US

771

772

773

774

775

667.1

668.45

668.65

670. 6

671.3

(m) lo

667.

668.

670.

671.

673.

Estimate _ ( m)Cu Zn

85

65

6

8

3

Py Po Length

0

0

1

1

1

.75

.20

.95

.20

.50

P?" Cu

138

619

234

20

184

PP* Zn

173

93

83

37

258

ppm Ag

0.9

0.9

0.7

0.4

0.8

ppb Au

5

6

5

7

5

Z Na20

2.68

5.68

2.81

3.52

2.64

Comments

Alt CLR

GR Dyke

Alt CLR

Alt CLR

Po Mineralised CLR

HOLE NO: UL-27 PftGE: 33

HOLE NUMBER: UL-28CORPORATION FALCONBRIDGE COPPER

DRILL HOLE RECORD IMPERIAL UNITS: METRIC UNITS: X

PROJECT:

QRID:CLAIM NUMBER:

LOCATION:DATE STARTED:

HATE COMPLETED:

PN370 WINSTON LAKE

SELCO

WINSTONOCTOBEROCTOBER

LAKE2, 1985

23, 1985

FIELD COORDS: LAI:DEP:

ELEV:SURVEY COORDS: LAU

DEP:ELEV:

4+95S3+25E422m1+592N3+856. 5E10423M

COLLAR BRNG:COLLAR DIP:HOLE SIZE:

FINAL DEPTH:

ROD LOG:PULSE EM SURVEY:

300"-83"60586ft

CONTRACTOR:CORE

MULIISHOICOLLAR

STORAGE:CASING:PLUGGED:

SURVEY:SURVEY:

SI .LAMBERT DRILLINGCLEAVER0.

X

8m BULAKE

4

*

t

PURPOSE:

9

a

t

*

t

Jt

41

?

J,

f

ACID TESTS IROPARI TESTS MULIISHOI DATACorrected Corrected

Depth (n)

3 50 100 150 200 250 300 350 400 450 500550

HOLE NO:

Angle

-83"-ei"-79" -73' -77" -75" -72" -69" -67" -62 0 -55"-52"

Depth (m) Angle Depth (n) Azimuth Dip Depth (n) Azimuth

t -73" (2 ETCHES)

100 304 160 308 220 308 280 302 (309) 340 309 400 311 460 309 520 310 580 314 (311)

316 (312)

Dip

-82" -82" -80" -77" -73" -70" -66" -61" -56" -520

WL-28 LOGGED BY: R.C.SIM

J

J

DRILL HOLE LOG

*)

f,

*(

*)

9

9,

9

FROM ROCK10 TYPE

0 to CASING0.8

0.8 ALTEREDto QEP135.4

COLOUR

Grey withpatchywhitestreaksJ pinkspots

Pink,white lgrey

GRAINSIZE

*9tomg

mg

ANGLE TOTEXTURE AND STRUCTURE CORE AXIS

Generally moderately towell foliated defined bymicas S sillimanite S 65"Locally chloritic maficclots (.1 x 3mm also definefoliation.Cut by numerous minor (3cvqt2 l granitic veins iclots.

1.3-1.5 S2.9-5.8:Massive equigranular

ALTERATION SULPHIDES REMARKS

Intense alteration Rare tr diss pyrite3-7X Muscovite Rare localised magnetite10-15X biotite (up to IX)0-3X garnet+35X cordieritePatchy wispy sillimanite,locally up to 3X overIjcrn sections.

0

t

granitic dykes.Sharp contacts 6 65"

11.8: 10cm qtz veinedbiotite rich shear sone B 75"

13.4-13.8:Epidote bleached S partiallycarbonate healed brecciazone 8 "60*

14.4-14.5:Muscovite rich (7X)granitic dyke 8 70"

IS.5-19.6:Granitic dyke, same as 2,9,cut by feld. phyric int.dykes at 18.8-19.0 and19.3-19.6

20.8-21.0:Massive fg int/mafic dyke 6 70 0

Fault

Fault ?

t HOLE NO: UL-28 LOGGED BY: R.C.SIM PAGE:

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



Grey fs 26.4-32.4: with Massive, locally feld. white phyric intermediate dyke, spots Sharp contacts 8

QFP xenolith at 31.8-32.0

35.1-35.7:Massive, mg granitic dykeContacts 8

36.2-36.4: Muscovite rich (7X) granitic dyke 0

36.5-36.9 S37.4-37.6!Feld. phyric int. dykes S

37. 6-37. B:Granitic dyke, sane as 35.1

46.6-47.0 S 48.2-48.4: Muscovite rich (5X) granitic dykes 8

48.6-49.2:FS nassive syn-volcanic intrusive dyke.

contacts S

Cut by 5X qtz t hematite veinlets

60"

60"

55"

65"

S 6 5"

65"

"60 0

7X biotite 15X cordierite

&0. 7-61,0:Biotite envelopins 10X qtsclots S.larqe rounded QFPfrasments, possible healedfault?

Possible fault ?

63.4-63.8:20X qts/epidoteover section


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



66.3-66.4 t6G.7-66.9:Irregular granitic dykes

67.4: 2cm calcite/qta vug with euhedral crystals Similar vug at 68.0 - lcn

69.0-69.1: Granitic vein

70.4-70.8:Well foliated feld. phyricint. dyke 8 75 0

73.3-73.4:Blocky ground with fracturesalong chloritic veins

73.5-74.1 S74.2-74.4:Pink granitic dykes 6 65"

74.5-77.8:50X dendritic qts/carb/epidote/hewat He/graniticveining over section.Locally blocky veinsaverage 0 "35"

Massive mg granitic dykesat: 84.0-84.6 8 65"

85.6-85.8 e 50"85.9-86.0 8 60"

88.6-89.0:Blocky, highly veined zonesimilar to above

5X nusc. books <\cm

Fault

Fault?


[IS ILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



9

9

93.6-93.8 t94.2-94.6:Massive fg mafic dykes e *65 0cut by 10!( qtz/graniteveins

94.8-97.4:40X veining over sectionSane as above l? "45"

99.2-99.5:Pink, cassive fg graniticdyke 8 *65*

99.5-101.1:30X veining over section, 35-45*very blocky, very chloriticlocally

101.4-101.6: Granitic dyke with irregular contacts

101.6-101.9:Blocky chloritic ground,possible fault 0 45"

104.3-104.5: Granitic dyke 6 *60 0

108.5-109.2!90X banded graniticveining over section l?

109.5: 10cm qts veiningenveloped in biotiteHas blue tinge (cordierite?)

110.2-111.1 S 111.4-111.7: Granitic dykes (3

50-60"

Fault

Fault

Fault?

50-60 0 3-5X muscovite


O

e

e

c

Q

4t

4

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



Cut by 2X qtz, carbonate or sillimanite rich qtz veins, all Ocm

132.0-135.2:Blocky ground with numerousfractures along chlorite orcarbonate veins.No grunge, probably not afault.

8 "117*: HEP altered to!5X muscovite10-15* biotite+40X cordieriteRare trace garnetPatchy sillimanite 0-2X(locally)IX anthophyllite

Ir diss pyrite

135.4 GABBROto215.9

. Harkgreenwithwhitei p inkspots

MS Generally a Massive equi-to 3ranular intrusive withC3 localised weak foliation

defined by chloritic clots 8Sharp upper contact(no chill) 6

137.0-137.1:Grey granitic dyke B

137.2: 7cti qtz vein 8

75"

40"

70"

55 8

1-2X leucoxene(no magnetite)Feldspars commonly stainedpink due to IX hematite/carb veining.

Rare trace diss pyrite

137.6-137.8:Weak, foliated fgintermediate dyke B 60"

140.6-140.7:Granitic/pegmatite dyke 8 80"

141.1-141.3:Grey granitic dyke,same as 137.0 e 70"

HOLE NO: UL-28 LOGGED BY: R.C.SIM PAGE: G

DRILL HOLE LOG

FROM ROCKID TYPE COLOUR



-*

t

Q

0 HOLE NO:

141.4-142.0:Syn-intrusive fg gabbroicdyke, ng in centre,grading to fgSharp contacts 8 70"

154.5-155.0: Pink granitic dyke Sharp contacts, top S 20"

bottom 8 75"

156.0-157.0:Weakly feld. phyric (2X)massive fg intermediatedyke S 8 0"

158.5-158.8 l159.1-160.0:Massive fg intermediatedyke 8 70"

160.5-160.8:Hematite veined l stainedqtz dyke 8 "35"

164.6-166.0:Pink S white granitic dyke 8 40*

175.0-175.1: Granitic vein 8 60"

178.6-179.5: Syn-intrusive gabbroic dyke, same as 141.4 8 60"

181.2-181.4: Granitic dyke 8 70"

Intense epidote veining at contacts

Intense epidote veining at contacts

5X associated epidote veining

168.7: 5X pyrite clots in lOcn granitic/qtz vein

UL-2S LOGGED BY: R. C. SIM PAGE: 7

e

DRILL HOLE LOG

FROM TO

ROCKCOLOUR



184.2-184.4:Fg massive intermediate dyke S 70 s

184.&-184.8:Blocky, grungy, chloriticfault zone 9 45"

185.9-186.9:Massive fg intermediatedyke e 50"

Similar dykes at:188.6-188.7 6 O 0 188.9-189.2 8 75" 191.3-191.8 S 60"

15X granitic ve i rung over section

Cut by 52 granitic veins

10X granitic veining

8 193.5m: Phlogopite wisps begin occurring in GB (NOTE: leucoxene disappeared at * 185m)

Fault

194.3-194.9!Massive fg intermediatedyke 8 60"

195.0-195.5:Highly feld. phyric (12X)intermediate dyke B 70"

Phlogopite definesfoliation @ 65-70"

200.9-201.0:Fg intermediate dyke S 70"

203.5-204.5:Massive fg feld. phyric(5X) intermediate dykeSharp contacts S 75"

Phlogopite has increased to 4X at 197m.

198.3: 5cm qts vein with 4X yellow/orange garnets (?)


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR


ANGLE CORE

TO AXIS ALTERATION SULPHIDES REMARKS

4

4

t

9

m

*

204.5-204.7:Massive mg granodiorite 22 garnetdyke 0 75"

205.3-206.2:Banded granitic dyke 8

206.6-206.7:Massive granitic dyke P

206.7-207.3:Moderately foliated feld. phyric intermediate dyke. Sharp chilled contacts 0

209.2-209.3:Grungy chlorite/carfaonaterich shear plane (zone) 8

Phlogopite defines foliation 6

210.5: 7cm int. dyke S

55" 52 muscovite

60"

2X garnet (anhedral, Ocm)

55"

Fault30-45"

fi 210m: gabbro contains 60-70" average 102 phlogopite in

wispy clots

60"

212.5-212.6:Granodioritic dyke 0 '45"

212.6-212.8:Fg massive intermediate 22 garnetdyke 8 50"(same as 206.7)

212.8-213.5:Granodiorite dyke l? 50"

214.4-214.6:Light grey feld. phyricintermediate dyke 0 60"

IX py clots associated with chloritic veinlets

O

O

O


o

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR

GRAIN SIZE IEXIURE AND STRUCTURE


None

REMARKSt

t215.9 TRANSITION Army to ZONE green 217.2 GAP.BRO with

brown spots

eg Massive chloritic matrixwith well defined foliation by phlog-biotite 8 50" Upper contact gradational narked by loss of feldspars Lower gradational over 10cm narked by influx of Magnetite and colour change.

216.2: 5cm granitic vein 8 40"

15X brown phlogopite/biotite in coarse wispy clots

217.2to219.0

219.0to225.5

MEIA-PERIHO-IITE

VOLCANICRAFT (?)(XENOLITH)

Lightblue/greywithgreenspots

Lightgreywithblackspots

ng Massive ultra-mafic cut by102 chloritic veinletsK. 5cm) bleaching host tolight green (TZ) colour.Fractures common alongveinlets.

fg Equigranular massive toweak foliated fi 0-10'Top contact sharp with10cm green bleached PX e 85"

IX carbonate veining

10-15X, fg biotite to 223.1(gradational)Cut by nunerous qtz/carb-onate veins Klcm)

None

IX very fine disseminated Could possibly bepyrrhotite recrystallised QFP?

Light eg 221.6-221.8:green Chloritic altered nafie(mottled) dyke.

Sharp contacts, top irregularbottom 0 40"

221.8-222.3:Feld. phyric gabbroicdyke l? "40"

15X biotite in foggy clot in Matrix of sericite and chlorite

8 223.1: gradation over 15cm to 'fresh' raft mat'l Well foliated 6 30" 7X feldspars, no visible qts eyes.

None


DRILL HOLE LOG

^ FROM ROCKTO TYPE

J

jl

225.5 META-to FERIDO-

^ 248.7 HIE

a

*

^

^

^

^

4

4

4

4

0 HOLE NO:

'

GRAIN ANGLE TOCOLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

224.7-224.9:Composite Gb/Graniticvein, top S 5 "

bottom B 60"3cm pervasive biotite atbottom contact B 35" to CA

Steel eg Typical massive magnetite Noneblue/grey rich ultra mafic unit.

5X phlog B 225.5-225.9

225.9-226.5:Sharp contacts define 15X biotite in bands None Reaction sone due tomagnetic biotite rich zone Proximity of raft?

237.2-237.9:Chloritic nafic dyke withsharp biotite rich (2cn)contacts 8 85"

237.3: 5cm qts clottingenveloped in biotite

238.8: 3cm chloritic grungy Faultfault 9 *80 0 (?)

B "240n: PX begins to becomebleached light green

241.6-242.0:Very chloritic biotitebanded ultra-mafic dyke.Sharp upper i lower contacts 6 70"

Similar dyke B 242.4-242.6 8 70"

Dykes border well foliatedfeld. phyric int. dyke at242.0-242.4

UL-28 LOGGED BY: R.C.SIM PAGE: 11

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



244.5-245.2:Well foliated grantitic dyke 8 55"

245.3: 7cm massive granitic vein B SO 0

Cut by 5Z chloritic veinlets K2mm)

248.3: gradation influx of fg bio/phlog 15X

248.7 PERVASIVE to BIOIITE- 261.5 CHLORITE

ZONE

Gradational upper contactover 20cm to very wellfoliated ultra-mafic sone B 45-50"Numerous fractures alongbiotite cleavage planes

249.3-249.5:Granitic dyke; irregularcontacts.Other granitic veins B

251.2 - 2cm251.4 - 3cm254.3 - 7cii

255.1-255.5:Ultra-mafic peridotitedyke, massive, fg, highlymagnetic with 2mm chillsat contacts S 65"

255.5-255.8:103! qtz veining over section

Cg massive pegmatitic dykes,often containing xenolithsof biotitic host at:

256.9-257.9258.8-259.1 (3 45" 259.3-259.7 6 50"

248.7: increase to pervasive biotite ^OX) S chlorite

None Non-magnetic - may be extremely baked xenolith or non-magnetic ultra mafic cumulate phase?

2x.5cn moly clot at 259.5 Several other smaller clots over dyke


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR


ANGLE CORE

TO AXIS ALTERATION SULPHIDES REMARKS

Dykes continued: 260.0-260.4 S 260.6 - 5cm

Foliation angle has gradually changed from 50" to CA to 65" at 261w.

2X pyrite clots

259.9-261.3: Gradational decrease in biotite to a fg well foliated gabbroic looking naterial

261.3 GABBROto264.4

Darkgreenwithwhitestreaks

fg Sharp upper contact 8Mod. well foliated equi granular gabbroinon-wagnetic) U

65'

65"

261.8-262.1:fg Massive feld. phyricintermediate dyke 8 65"

Sera biotite i 2cn granitic vein at bottom contact at 70' to CA

264.4to265.0

265.0to278.4

ALTEREDGFP

GABBROICDYKESUARM(IN QFP)

Mottled/bandedblue/greyJ white

Darkgreenwithmottledcloudywhitesones

'9towg

f9

Very well foliated 6 60' +35X cordierite Noneequigranular 15X biotite20X stretched qtzeyes K4mm)

Well foliated equigranulargabbro commonly showing abanded textureghostly light colouredsplotches K3cm) seem torepresent fragments ofaltered QFP


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



Gabbroic dykes l?:265.0-269.0 0 70"

272.0-274.5 8 "75"

276.3-278.2:All dykes have sharp 75"contacts with altered QEP

l Oca granite vein @ 267.8

Granitic dykes S 271.8-272.0 272.5-272.8 273.1-273.2

Granitic dyke 8 278.2-278.4

Note: visible feldspars in alt. QEP 8 274.5-276.3 (4Z)

278.4 ALTERED to GFP 334.0

Mottled 119 blue/grey S black

White, pink i grey

Equigranular qts/cord groundmass with biotite defining well developed foliation l? 70" Locally cloudy white feldspars faintly visible (e.g. 286.5m)

Granitic veins at:278.7 - 5cm 0 75' 280.3 - 6cm 6 70"

281.8-282.8:Eg massive highly feld.phyric 10X intermediatedyke (composite dyke withinternal contacts e 282.1)Contacts at 70"

Massive eg granitic veins 8: 295.9-296.0

297.2 - Sen297.6-297.7297.8-299.4300.6-300.9301.1-301.7 (70X of section)

+40X cordierite 15!! biotite 1-2X Muscovite

Very rare trace diss pyrite Locally feldspars are visible, but still seems to be a very altered OFF

Magnetic

HOLE NO: WL-23 LOGGED BY: R.C.SIM PAGE:

J

J

J

DRILL HOLE LOG

FROM TO

SOCK TYPE COLOUR



Granitic veins (eont'd) 304.5-305.1 305.9 - 5cm 311.0-312.0 (302 of section)

313.1-313.5:Fg massive feld. phyricint. dyke 6

314.4-314.9: composite granitic/qtz dyke S

316.8-317.1:Very coarse graniticpegnatite l?

319.7-319.85: Granitic dyke S

322.6: 5ci granite vein

323.4: l.Scw granitic vein highly folded (wormy)

325.4-325.9;Feld. phyric intermediate dyke with well defined foliation by chloritic mafic clots (152) Klcti) Sharp contacts 8

75"

45"

"80"

60"

75"

Gradational decrease from 313.0-315.0 in biotite content to 72 feldspars begin to become quite common.

32 Muscovite books

32 py cubes

Vein originally perpend- icular to foliation Veins pre-deformation ?

52 grit over bottom 20cm in QFP.


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



334.0 SILICEOUS Greyto BARNET with469.4 ALTERED pink

SEDIMENTS spots

Generally a massive fs matrix supporting up to 10X garnets (rare silica rims)Locally a weak foliation is defined by ghostly siliceous patches or patchy chloritic clots

B

+35X cordierite 5-10X biotite 4-10Z garnet

Ir-lX disseminated pyrite (locally increasing withgarnets)

Patchy 1-32 magnetite

75"

337.5-337.9:Massive, ng granitic dyke 8 4 0"

340.7-341.0: Chloritic mafic dyke ?

341.2-341.7: Feld. phyric int. dyke. Sharp contacts, top 8

bottom S

341.7-342.2:50X irregular graniticclots over section

346.5-346.9!Blocky, grungy fault zone 8

75"

75' 30"

'70' Fault

347.1-347.3: Granitic dyke 8 75"

357.2-357.5: Massive, fg chloritic iiafic dyke S

358.7-359.0:Massive, fg granodioritedyke - irregular contacts.

359.9-360.1:Garnetiferous granitic dykeIrreqular contacts.

75 0

HOLE NO: WL-28 LOGGED Elf: R.C.SIM PAGE: 16

DRILL HOLE LOG

FROM10

ROCK TYPE COLOUR

Greenwith white spots

GRAIN SIZE

fs

TEXTURE AND

362.6-362.9: Feld. phyric

363.0-367.5: Patchy well equigranular

STRUCTURE

int. dyke 8

foliated 9abbro 8


75"

75"

SULPHIDES REMARKS

Locally 2 X dies pyrite

363.9-364.4: Granitic dyke 8 75'

364.5-364.7:Numerous chloritic shearsover section 8 70-75"

368.9-369.0:Granitic dyke, irregularcontacts.

375.7-377.0:Light green/grey intermediatedyke/int. sediment (?)Zone with rather sharpcontact 0 75"

378.0-378.1 l378.8-378.9:Granitic dykes andirregular contacts.Similar dyke at 381.4-382.1 8 '55"

386.0-386.3:Feld. phyric int. dyke S also at 390.0-390.1 8 and 392.7-392.9 8

Salt S pepper granodioritedykes/clots B 399.4-399.5

and 399.75-399.8

75" 75" 75'

Unaltered

Fault

ICB vein 6 376.0 with 502 pyrite, 50X yellow sphalerite

8 *390m: silica rims aboutgarnets become commonRock weak banded 6 75" to CA

1-2X pyrite clots associated with garnets (locally up to 4X over sections OOcm)

HOLE NO: UL-28 LOGGED BY: S.C.SIM PAGE: 17

DRILL HOLE LOG

FROMTO

ROCK TYPE

GKAHi COLOUR SIZE TEXTURE AND STRUCTURE


413.2-413.6:Well foliated fs int/gabbroic dyke S 7 5"

419.0-419.2:White qts dyke, top l? 55"

bottom (? 85"

420.6-420.B:Fg massive int/maficdyke B 65"

Grey with fs 421.3-424.B:patchy Massive intermediate dyke,white locally feld. phyric.spots Sharp contacts 8 70"

Sediment xenolith at422.6-422.7

424.8-425.0:Granitic dyke 8 80"Similar veins/dykes at

432.3-432.6 - over 50X section

432.9-433.2 8 60"

433.2-434.0!Feld. phyric int. dyke.Similar to 421.3 8 75"

Massive to weak foliated 8 75"

3X garnet

pyrite veinlets

2X py streaky veinlets increasiri3 B contacts

Localized pyrite veinlets(as above)3Z py e 422.8-422.9

6 *435n: Garnets no longershow silica rimsAlt. has decreased insediments to:+30Z cordierite2-5X garnet5Z biotiteTr-2X anthophyllite

1-2X py, tr-lX po in localized veinlets is commonly parallel to foliation

Patchy Magnetite due to pyrrhotite


DRILL HOLE LOG

FROM10

ROCKTYPE COLOUR



Bark green

440.7-443.3:Massive chloritic nafic dykeSharp contacts 8

Garnetiferous granitic dykes at: 447.2-447.3

451.6 - 5cm451.9-452.0454.1-454.4454.8-454.9455.9 - 5cm456.8-456.9458.1-458.4463.0 - Sen463.1-463.3

463.5-464.3: Blocky core, mainly dry fractures, few chloritic Probably not a fault.

405.2-405.3:Garnetiferous granitic flow

75"

4X sillimanite, no garnet

465.5: Silica rimmed garnets begin retrograding to chlorite S qtz

Very common above 'intermediate 1 sediment unit.

469.4 WEAK Greenish fg Typically nassive equi- to ALTERED grey granular sediments 541.5 INTER- Locally weak foliated 75"

MEDIATE defined by mottled SEDIMENTS siliceous patches (Omni)

Upper contact gradations! narked by decrease in garnets.

472.7-473.2:Chloritic mafic dyke,massive, fgSharp contacts @ 8 0"

Variable S gradational from unaltered to minor cord (20X) g biotite K5X) to garnetiferous patches similar to above.

Very rare tr py, slightly nore comaon in garnetiferous zones.Localized bands (Ocm) containing up to 5X sub hedral magnetite K2nn)

HOLE NO: WL-2S LOGGED BY: R.C.SIM PAGE: 19

DRILL HOLE LOG

FROM TO

ROCK GRAIN TYPE COLOUR SIZE TEXTURE AND STRUCTURE

473.8-475.3: Massive, mg, granitic dyke, contacts fi Similar dykes at 476.2-476.35 9 480.3-480.4 fi 480.6-480.8 6


IX diss/clots pyrite 40"

45" 75" 750

491.7-491.9: Granodiorite dyke 8 700

ijranitic/granodiorite dykes at:

492.3-492.6492.9-493.0494.4-494.5 - qts vein497.3-497.5 8497.7-499.2 - over 70X

section

65"

482.0-482.3 i 483.0-483.5:Gradational garnetiferous altered sediments

Irregular 3 x lcn pyrite clot B 483.4m.

484.3: Several garnetiferous veins K2nim) cutting sediments

491.1-491.6:Pervasive biotite zone cutby 5X qtz clots S veins

i " 492m: sediments begin to beeoae nore altered. Generally 10-152 biotite +35X cordierite Still with patchy zones of siliceous gnt. alt. sediment

HOLE NO! WL-28 LOGGED BY: R.C.SIM PAGE: 20

DRILL HOLE LOG

FROM ROCK TO TYPE COLOUR

GRAIN SIZE

ANCLE TO CORE AXISTEXTURE AND STRUCTURE

501.8-501.9: Qtz vein

501.9-502.1: Granitic dyke

Salt S ng Massive granodiorite(?)/pepper QFP(?) dykes at:patchy (contacts grade over 5mni) *75-80 cstained 509.6-510.5pink 511.6-511.8

512.3-512.5513.2-513.6514.4-514.5514.7-515.3516.0-516.3516.5-516.7

Dark fg Massive, locally feld. green phyric int/iiafic dykes at:

512.5-513.2513.6-514.4514.5-514.7516.3-516.5

519.0-519.4:Granitic/qtE conposite dyke 8 *60*

521.6-521.9:Qts/carb vug with euhedralcrystals - blocky ground

523.8-524.1:Granodiorite dyke l? 80"


502.1-502.3:Intense/pervasive biotite zone with 10X qtz clots

2-4Z fg biotite 10X cordierite f?)

3X py clots over section

IX pyrite clots (On*) May be equivalent to 'QFP 1 seen just above intersection in WL-27

Alteration gradationally decreased at "527m to fresh' int. sediments with small gradational patches of altered niat'l.


DRILL HOLE LOG

FROM ROCK GRAIN 10 HPE COLOUR SI2E

541.5 INTER- Grey with fg to COLATED nettled 550.6 TUFFACEOUS white S

( TEXTURE AND STRUCTURE 1

528.8-528.9: Granitic dyke Other granitic dykes at:

532.1-532.2 535.0-535.3 8 535.5-535.6 6 536.0-537.2, top 8

bottom @ 539.5-539.6 8 541.0-541.2 8

Generally a massive weak altered unit (sediments) with localised banded

INGLE TO:ORE AXIS

*75" "80" 45" 5"

80" 75"

75"

i ALTERATION SULPHIDES REMARKS

Sediments - +25X cord, Very localized pyrite, 52 bio, tuffs - *30X cord iiainly in biotite rich up to 30X biotite over zones in diss bands (up

l SEDI- black MENTARY zones MATERIAL

9

*

zones which are generally nore altered (tuff)


542.6-542.8 i545.2-545.3:Fg moderately foliatedfeld. phyric intermediatedykes 8

sections *C0.3ra

IX garnet often enveloped in biotite

to 5X over sections Rare tr po.1-2X nagnetite in seds S tuff KlM)

75 8

547.9-548.0 l548.4 - 4cm: Granitic veins

549.3-549.5:Banded tuffaceous Bonewith sharp contacts

549.9-550.05:Qtz vein, irregular contacts

550.05-550.3:Garnetiferous granodiorite dyke

40X cord10X bio5Z anthophyllite

4X garnet

32 py, tr-lX po in disseminated bands

D

J

J

IX py t po 27, magnetite


TI

DRILL HOLE LOG

FROM TO

550.6to555.2

ROCK IlfPE

INTER-COLAIEDQFPELOUSf?)i TUFF ACEOUSMAT'L

COLOUR

Mottledtobandedgrey/blackt white

GRAIN SIZE

Vari able

ANGLE TO TEXTURE AND STRUCTURE CORE AXIS ALTERATION

Well foliated mg QFPflows with gradationalcontacts (over l-2cm)to moderate to wellbanded tuffsBoth units are non magnetic.

SULPHIDES REMARKS

'QFP 1 sections don'tseem to be graniticbecause they are weaklyaltered and do not con tain magnetite (truegranites below contain"2X magnetite)

J

J

550.6-551.S:GFP flow well foliated 0 Patchy visible feldspars (cloudy) arid barely visible qtz rich rounded domains (qtz eyes?)

Similar QFP zones at: 551.8-552.0 552.2-552.4 552.7-552.9 554.5-554.6

75-80 Very weak altered OCX patch cord. 2X biotite

10X biotite

Ir- IX diss pyrite

Flows separated by biotitealtered banded zones (tuffs) 75-80"

553.5: Sen granitic vein

Qtz veins 8 554.1 - Sea 554.65 - 2o 554.7 - 7cw 555.0-555.1

Avg. 20X cord, 10X biotite Tr-lX diss pyrite

555.2 MASSIVE to TO SEMI- 555.5 MASSIVE

SULPHIDES

Orange S fg Wispy dendritic web of fggold sulphides enveloping 35Xsulphides fragments (5X white roundedwith grey qts up to lcm, 20X hostS white frags, angular up to 3cm,fragments 10X perv. bio/cord frags

Wispy gradational contacts with only 10/i sulphides over bottom 5cm.

Smaller pervasive biotite/ cord fragments are very rotted i invaded with sulphides

Tr-lX pyrite6X chalcopyrite (wispy

veinlets) 25X pyrrhotite 33X sphalerite (orange/

brown)

Est: 2'/. Cu 16X Zn 0.3m~


DRILL HOLE LOG

FROMTO

555.5to558.8

558.8to558.9

558.9to569.6

ROCKTYPE

ALTEREDVOLCANICTUFF(CLR)

FELSIC(QFP?)FLOW?

GARNET IFEROUSTUFFAC EOUSSEDIMENT/FRAGMENTAL(MINERAL IZED)

GRAINCOLOUR SIZE

Mottled Aphan-to iticbanded fgblack tlightgrey

Mottled mgblack lwhite

Mottled fglight ldark greywith pinkspots

ANGLE TOTEXTURE AND STRUCTURE CORE AXIS

Locally well banded alteredtuffaceous unit on 0.5-lcmscale S 75-80"

Several chloritic/carbonaterich fractures from 555.5to 555.6

Massive zone similar toQFP 's above sulphidesSharp contacts, top S 60*

bottom 8 75"

Fluctuating unit frommassive to banded(altered) on lcm-5cmscale 6 80"

ALTERATION SULPHIDES

+40X cordierite 2X po, IX py in streaks,15X biotite locally with clots and disseminatedcommon pervasive bands Klcm)Patchy localized antho phyllite m overall)

Minor cordierite "10X None21. b iotite

Avg. 8X garnet to 567.0 2X py, IX po to 562.3(gradational) in discontinuous bandsLocally up to 15X over Tr-lX sphaleritesection ^Ocm (associated with gahnite)+35X cordieriteftvg. 15X biotite (brownand black)2-5X anthophyllite2X gahnite over section(locally up to 5X overlcm sections)

REMARKS

Seems to separate foot wall units. May be smalldyke coming in alongcontact.

560.8-561.2:Feld. phyric int. dyke.Sharp contacts over 5mm 2 80"

562.0-562.1:Garnetiferous granodioritedyke.Sharp contacts with 5cmbiotite in host S 75"

562.3-563.2:- Several sulphide rich bands, sulphides in biotite rich host. 3X py, 2X po, tr sphal over section

Hay be equivalent to 'pyrrhotite zone' in WL-11 S UL-12


DRILL HOLE LOG

FROM ROCK 10 TYPE COLOUR



563.2-563.7:Blocky zone with numerouschloritic fractures2ca chloritic grungeat 563.2 B

564.1-564.3: Blocky z one cut by numerous chloritic fractures 8

"45"

"45"

Fault

Possible fault

567.3-567.4: FS massive int. dyke 9 80"

Gradation decrease over 15cm to tr-lX 9nt at 567.05

Below 567.4: qts fragments are stained light brown/ yellow

Below 564.3: Mainly posulphidesAvg. 2X po, tr-lX pytr-lX sphal associatedwith gahnite

567.4-569.6: 1-2X sphalerite over section, associated with gahnite, also 3X py -f po

@ +S68.5: unit begins to look very fragmental with bedding constantly changing enveloping banded fragments up to 4cmVery sharp lower contact at 569.6 e 80"


l

l

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



569.6 CRYSTAL Mottled us Moderate to well foliatedto RICH INI/ to defined by mafic streaks585.O FELSIC spotted and bands 8 75-80"

FLOWS grey S Several crystal rich flows E.O.H. WITH white with more altered and

MINOR generally More banded TUFFACEOUS tuffaceous tops COMPONENT (CLR ?) 569.6-570.5:

Weak banded altered tuffaceous zone becomins slightly crystal rich over lower 20cm.

Salt S 570.5-571.1:pepper Massive 013 granitic dyke

Sharp chilled contacts 8 80 0

571.1-573.9:Patchy crystal (feldspar)rich throughoutSharp lower contact withl.Sciu chill e 65"cut by granitic dykeat 571.2-571.3

573.9-575.0:Patchy feldspars (3X total)in fg massive alteredmatrix.Cut by granitic veins at:574.2 - 7cm and574.6 - 5cm

575.0-575.3:Cg granitic dyke @ "80"

Flows look a lot like granite but seem to be slightly altered. Very poorly defined faint tiafic clots suggest this may be very weak altered CLR?

+25X cord 10X biotite

IX diss py * poIX vfg diss magnetite

20X cord 5X biotite

20X cord, 7X biotite

HOLE NO: WL-2E LOGGED BY: R.C.SIM PAGE: 26

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



J

J

J

575.3-579.0:Well foliated crystal 10X cord, 3X bio grading Tr diss pyrite,rich I8X) flow. to 20X cord, 5X bio 6 577.5 IX diss nagnetiteGradationally decreasing cut by 5X chloritic veinletsin crystals S increasing over bottom 0.5min alt 6 577.5

579.0-579.7:Pink, white S greygranitic dykesSharp contacts @ 70"

579.7-585.0:Weak altered feld. phyric 5-10X cord, 2-3X biotite Ir diss py(patchy) unit, similar to IX diss Magnetite575.3Cut by fg Massive feld.phyric int. dykes at:

581.4-581.8 8 80"582.1 - Sem 8 70 0

S 583.1-583.5 @ 75"

End of Hole.

HOLE NO: WL-28 LOGGED BY: R.C.SIM PAGE: 2 7

tt

tt

ft

tt

tt

tt

tt

tt

tt

tt

tt

tt

tt

tt

tt

tt

tt

'

W W

ROUTINE GEOCHEH RESULTS

Sample (m) (m) Estimate di) ppm ppn ppb 'iNumber From lo Cu I n P y Po Leristh Cu Z n Au

US 0734 6.0 9.0 -- — — — 3.0 46 590 70725 39.0 42.0 — — — ~ 3.0 21 108 50736 69.0 72.0 -- -- — — 3.0 7 60 50737 102.0 105.0 — — ~ — 3.0 6 60 50738 129.0 132.0 — — ~ ~ 3.0 3 41 6

0739 219.0 222.0 ~ — ~ ~ 3.0 35 45 50741 279.0 232.0 — ~ — — 3.0 20 40 60742 309.0 312.0 — — — — 3.0 7 63 50743 336,0 339.0 — -- 1 — 3.0 8 118 50744 369.0 372.0 -- — 1 ~ 3.0 9 132 6

0745 399.0 402.0 -- — 2 — 3.0 130 130 50746 429.0 432.0 — — 1 — 3.0 16 100 50747 459.0 462.0 ~ — 1 — 3.0 35 34 60748 477.0 480.0 — ~ — — 3.0 8 39 60749 504.0 507.0 ~ ~ ~ — 3.0 8 28 50750 531.0 534.0 — — — ~ 3.0 24 51 5

HOLE NO: UL-28

Na20 Comments

1.81 Alt QFP1.77 Alt QFP2.22 Alt QFP2.02 Alt QFP1.34 Alt QFP

4.58 QFP raft (?)4.15 AU QFP2.85 Alt QFP3.02 Sil. gnt. alt. seds.3.01 SGS

2.37 SGS1.57 SGS2.52 SGS1.77 Int. Seds.2.19 Alt. Int. Seds.2.67 Wk alt. Int. Seds.

PAGE: 28

tt

tt

tt

tt

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tt

tt

ft

ft

ft

NON-ROUTINE GEOCHEH RESULTS

Sample (m) Number Fron

US 0851 553.60852 555.20853 555.50854 557.20855 558.9

0856 560.80857 561.20858 562.30859 563.20860 564.7

0861 567.050862 568.30863 569.6

(m) To

555.2555.5557.2558.9560.8

561.2562.3563.2564.7567.05

568.3569.6570.5

EstimateCu Zn

2.0 16.0--—— 0.1

,.— 0.1

0.2—— 0.2

— 0.2— 0.5--

Py

11212

--2311

121

Po

25121

—1212

211

(m)

1.60.31.71.71.9

0.41.10.91.52.35

1.251.30.9

ppm Cu

173—1119690

1430

10425

130

184101

7

ppm Zn

525—13281120

491972301466935

30901764119

PP* A9

0.6--1.10.40.4

0.20.51.10.70.8

0.80.94.0

ppb Au

10--667

66656

1855

XNa20

2.82~2.723.292.97

2.972.482.861.74

1.142.223.38

K X g/t g/t Cu Zn Ag Au

2.90 9.44 58.0 0.05———

————..

———

Comments

Alt. seds t CLRMS/SMSAlt. CLRAlt. CLRGnt. alt. tuff/sed.

Int. dykeGnt alt. tuff/sedsAlt. tuff/sed.Gnt. alt sed/tuff - fault zoneGnt. alt. sed/tuff

Alt. sed/tuff fragmentalAlt. sed/tuff fragmentalAlt. tuff (CLR)

J! X XXX XX X X X X X Si02 A1203 Fed HqO CaO Na20 K20 Ti02 P205 hnO C02 S

2 K ppa ppn ppn ppm ppi* ppm ppb H20 LOI Cu Pb Zn Ni Co AS Au

0739 219.0 222.0 QEP raft (?)

3.0u

0740 252.0 255.0 3.0m Pervasive bio/chlorite

54.9 1.02

48.9 8.85 10.57 17.12 6.69 1.20 2.88 0.74 0.26 0.21 0.83 0.96 0.01 1.72 88 10 70 453 48 0.7

HOLE NO: UL-28 PAGE: 29

HOLE NUMBER: UL-29CORPORATION FALCONBRIDGE COPPER

DRILL HOLE RECORD IMPERIAL UNITS: METRIC UNITS: x

PROJECT: PN 370 WINSTON LAKEGRID: SELCO

CLAIM NUMBER:LOCATION: PICK LAKE

DATE STARTED: OCTOBER 14, 1985DATE COMPLETED: NOVEMBER 6, 1985

PURPOSE:

ACID TESTS Corrected

Depth (n) Angle Depth (m)

FIELD CHORDS: LAI: 4+30SDEP: 6+60E

ELEV:SURVEY COORDS: LAT:

DE P:ELEV:

CorrectedAngle Depth (ID)


FINAL DEPTH:ROD LOG:

PULSE EM SURVEY:

TROPARI TESTS

Azimuth Dip

300"-B3 8BQ854a

X

CONTRACTOR:CORE STORAGE:

CASING:PLUGGED:

MULIISHOT SURVEY:COLLAR SURVEY:

MULIISHOT DATA

Depth (B) Azimuth

ST. LAMBERT DRILLINGCLEAVER LAKE1.5m BU

X

Dip

30 bO90

120 150180 210 240 270 300 330 360 390 4204504805105405706006306606?07107507&0810840

82.5" 81"80" 79078"77" 76" 76" 74073" 71" 70.5" 70"

69"69"68.5"68"67.5"67"66"65"65"S3 062 0bi"61"30"

65125 185 245305 365 425 485 545 605 665 725 785845

.................

298295 296 299300 303 325 1 306 301 ? 299 ? 308 306 309 ?306

-80"-78" -76" -75 0-73" -72 C -70.5" -70" -69" -68" -66" -64 0 -62.5"-61"

Q

a

e

t

c-

HOLE NO: WL-29 LOGGED BY: R.C.SIM

DRILL HOLE LOG

FROM 10

POCK TYPE COLOUR



O to 1.50

CASING

1.50 ALTERED Light mg Generally well foliated to QFP grey with defined by micas 0 342.7 pink spots Patchy sugary texture

l white due to recrystallization flakes of qts in matrix.

Rarely cut by cloudy siliceous veins (Ocn) often py mineralized with bio rich halo in host.

7.8: 5cn nusc. richqts vein e 55"

13.7: 4cm band rich inbiotite (50X) e 55'

Light grey, massiveintermediate dykes S 27.6-27.9 (? 55" 29.0 - 5cm 6 55" 32.2-32.3 6 55"

Creamy mg 38.2-38.6:Musc/sericite rich siliceous dyke.

46.7-47.1:weak foliated fg feld.phyric int. dyke l? 55"

47.1-47.6: Irregular mottled siliceous granitic dyke

+40X cordierite 55" 10-152 biotite

3-5X muscovite 2-4X garnet tr-lX anthophyllite

Localised clots pyrite (\'2mm) or in veins associated with qts (IX total)

+20X cord.

3X muse books IX gnt


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR


ANGLE TO COKE AXIS ALTERATION SULPHIDES REMARKS

55.0-56.8:Blocky, vuggy hydratedfault zone, localisedchloritic grunge sonesthroughout 3 55-60"

61.2:4cm qts vein with 9reen bleached halo in host 10cm above i below,

74.3-74.7:Hell foliated biotiterich (50X) zone w ithsharp contacts 6 60"f may be dyke?)

76.8:5cm recrystallized qts "55"vein (?) partiallyaltered to cordierite

Creamy white muse, rich siliceous dykes B82.5-82.6 and83.0-83.3 B 40"

83.4-83.9:Well foliated bleachedint. dyke cut by 25Xqts/ep veinsSharp contacts S 5 0"

48.5-49.0:Intense biotite developed in host due to 15X qtz clots over section.

OFF the same below fault but contains tr-lX gahnite

Fault

Intense gahnite with powdery light brown hogbomite selvedge

Patchy 1-3Z wispy white sillimanite begins S 7 7m

Intense vein-line dendritic po (tr cp) at contacts

C


C*

e

e

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



94.3-95.2:Gradational bleached zonein QFP (epidote ?)

Black aphanitic diabasedyke with sharp chilledcontacts at

105.9-106.0 B 65" 106.9 - 3cm 6 50"

110.9-111.O:Blcoky, grungy chloritic Faultfault zone e "60"

Irregular muse, rich qts veins l c lots at

111.7-111.9112.3-112.5112.7-112.9

Light green intermediate 2X garnet dykes (?) at

117.5-117.6 B 50'118.1-118.2 8 50"

130.7-131.4:Well foliated fg-nggabbroic dyke cut by10X qts veinsSharp contacts S 5 5 0Similar dyke at133.2-133.5 e 50"

MS.4-147.0:Fg well foliatedgabbroic dyke @ 70"


0

* DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR

GRAIN SIZE IEXIURE AND STRUCTURE


Generally tr diss py.

REMARKS

Very altered QFPMassive to noderately foliated defined by lucas and sillimanite S 60"

151.8-152.1:Fg massive int. dyke.Sharp contacts 8

152.1-152.3: Granitic dyke B

"60"

•40"

155.4-155.7: Massive fg-mg int. Sharp contacts 8

dyke.

Sillimanite rich siliceous dykes at

157.2 - 5cm 9158.8-158.9 8160.-7-161.7Very wormy, irregularover 70X section

65"

60" 65"

Gradational increase in alteration from 147w-153* to: +40X cordierite

15-20X biotite 3-4X garnet 2-5X sillimanite 1-3X nuscovite Patchy localized up to 22 staurolite (granular, light brown, ^H) 1-3X gahnite (with hogbomite halo)

Cut by 43! carbonate veins

154.8-155.4! Intense biotite sone gradational over Sen 50X biotite over section

11. s illimanite 1-3X garnet

164.5-164.7: Biotite rich sone, similar to 154.8

e

m

4X pyrite clots (tr cp)

4X py clots

HOLE NO: LOGGED BY: R.C.SIM PAGE: O

O

5

DRILL HOLE LOG

-) FROM ROCK 10 TYPE COLOUR



grey

166.9-167.0:Blocky zone, 'dry' fracturesmay be drill related.

Sillimanite rich siliceous clots, sane as above, over 40Z section from 172.6-172.9

f9 173.3-175.1:to Patchy weak foliated int.mg dyke.

Grading 'to feld. phyricat 174.3-175.050X granitic veining from173.5-173.7Sharp contacts S

178.7-178.9: Tg int dyke Similar to 173.3

Possible fault?

60"

Intense gahnite associated with vein contacts

65'

Creamy mq Muscovite rich siliceouswhite dyk.es at:

181.1-181.3 @ 181.9-182.5 8 186.0-186.6 l! 187.1-187.4 e

+7X muscovite

60" 60" 50"

177.2: lcn qta/carb vein (recrystsllised) with sulphides at contacts 15X py, tr sphal over lcm

179.6-179.7:Several recrystallized qts hosted sulphide veins (\lcm) 15X pyrite3X sphalerite4Z gahnite over 10cm


DRILL HOLE LOG

fROH 10

ROCK TYPE COLOUR


ANGLE CORE

10 AXIS ALTERATION SULPHIDES REMARKS

Salt Spepperwithpinkspots

Massive fq gabbroic dykeat 183.7-184.1 S 50-60"

192.8-193.3:Siliceous dyke, saneas above at - 75"

f9 195.1-195.5!Massive altered syn-volcanic dyke.Sharp contacts S 6 0"

200.5-200.7: Pervasive biotite Bone bordered by 5cm qts veins (top and bottom)

203.9-204.5: 75X creamy white nusc. rich siliceous clots over section

205.2-205.3:Biotite zone bordered byquartz, sane as 200.5

Ueak foliated S 70"

211.7: 10cmfogsy siliceous patchin QFP

222.1-222.3:Granitic dyke (2 55"

5X nusc.

12X biotite +35X cordierite A'/, garnet (with siliceous

riss ?)

10X garnet (banded) BOX biotite 10X qts

SKm pyrite vein/band at 195.7 S 60"

Garnets disappear over 1m at 210mQFP altered to:

+50X cordierite 20X biotite 3X anthophyllite

Very altered QFP


DRILL HOLE LOG

FROM"OROCKHPE



223.4-223.6:Chlor-bio rich mafic dykewith qts veins at contacts l? 70"

Siliceous granitic dykes at 223.9-224.0 8 224.2-224.6 8 225.0-226.1: veins/dykes over 60X section 8

227.0-227.4 8

228.1-228.3 8

60"

"65"

75"

75"

244.4-244.6: Composite epidote rich mafic S qts veined dyke


251.7-251.8: White qtz vein S

258.2:5cm granitic vein 8

70"

700

60-70"

3X biotite veins 42 muse, flakes

229.4-229.5: Dendritic sillimanite (15X over section) enveloping altered QFP fragments

247.0: lOcn biotite band enveloping rounded QFP frag.

5X Muscovite

257.8-258.1: Light green (epidote ?) bleached sone with sharp contacts at 75 0

75"


0

* DRILL HOLE LOG

F SO (i 10

ROCK HPE COLOUR



265.1-265.5:Mg well foliated feld.phyric gabbroic dyke.Sharp contacts 0 70"

268.4-268.5:Granitic vein l? 65"

269.6-269.8:Massive fg int/maficdyke B 75"

269.8-271.5:Massive mg granitic dyke 8 65-75"

271.5-273.2:Gabbroic dyke.Sharp chilled contacts 8 50 0grading to mg well foliatedin centre.

273.2-276.6:Very weak to unaltered QFP

276.6-278.7:Massive fg-mg gabbroic dyke.Sharp chilled contacts 8 75"

278.7-280.0:Very blocky fault sone.Numerous dendritic fracturesfault grunges at 278.8-6cm 8 30-45 0

Begin to see a decrease in alteration in QFP S 266m, incipient altered 8 268m, unaltered fi 269n.

Highly epidote veined at upper contact (Sen)

Highly epidote veined over 20cai at bottom contact

Very ninor cord? biotite (2X) feldspars patchy stained pink

faulte

c

eHOLE NO: UL-29 LOGGED BY: R.C.SIM PAGE: 9

t

DRILL HOLE LOG

FROM 10

ROCK WE COLOUR



Numerous fractures (commonly chloritic) to 283.6Epidote healed breccia zones at:

280.2-280.4281.0-281.2

Minor chloritic grunge at 281.5 - lcm 0

Py nineralised carbonate vug at 283.3-283.5 0

283.6-288.2:Weak altered OFF - mg;generally massive tolocally very weakfoliated at 'swirling 1angles

Specked fg 288.2-293.9: greenish/ Massive intermediate dyke grey Sharp contacts 8

cut by irregular granitic/qtz clots S dykes at:

288.5-288.7 (over 50Xof section)

291.6-292.3 292.5-292.8 293.0-293.4 293.5-293.8

294.2-294.5:Irregular qts clotting over70X section in QFP

8 " 295m: QFP similar to 283.6 - weak foliated locally at various angles

40"

10"

Fault

20-60'

SO 0

Fg bluish cord, altered (?) matrix supporting 30X cloudy white spots K3mw) (feld t qts)

Dyke probably fg equivalent of gabbro

152 cord77. b iotiteIX anthophyllite

Ir diss py.


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



s*

9

9Mottled light S dark bluish/ grey

9

9

9

296.8-298.7:Irregular granitic iqts clots over 30X section

298.7-300.6!Massive, fg intermediatedyke with sharp contacts S 45 0

Similar to 288.2 cut by 10X irregular granitic/ qts clots KScrn)

300.65-300.75: Very well banded cherty fragments (?) on mn scale 8 5-15" Sharp contacts 0 40"

Numerous microfractures locally offset banding

Epidote stained

Gradational 3X magnetite (rounded \'2mni) disseminated from 299.3-299.6

2X py in veinlets S fine disseminated in one cherty band near lower contact

Possibly a mineralised 'cherty' exhalitive fragment.

pYLiti-iQ-feiQd.iQgks

301.1-301.2: Qt2-granitic vein 8

e " 301m: QFP weak to moderately foliated S Locally varying to as low as

Commonly irregular siliceous granitic clots/dykes 8304.5-304.6306.8-306.9308.1-308.2312.1-312.3312.5-313.0

50"

75'

10"

Moderately altered 20Z cordierite 5-7X biotite Ir-lZ anthophyllite

Ir garnet 8 301.5 (otherwise no garnet)

2X sillinanite wisps

None

HOLE NO: UL-29 LOGGED Et: R.C.SIM PAGE: 11

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



311.4-311.7:Gradational 32 sillimaniteover section

Dark

314.8-315.2:Fg gabbro dyke, wellfoliated with sharpcontacts 6 75"

318.0-318.2:Granitic dyke - bandedon .Sen scale over top7cm, sharp contacts 8 75'

319.1-319.2:25X white cloudy spots(qtz eyes) over section(gradational)

319.3-321.9:Massive gabbroic dykeSharp contacts ? 70 8Similar dyke at 322.8-323.1 S 8 0 0

Massive QFP to 327mgrading to very wellfoliated defined bynicas S sillimanite 8 75-80"

334.8-335.0:Massive qts vein, top 8 40"

bottom 8 65"

10X ghostly epidote patches 2X epidote veining

Very altered QFP+40X cordierite+ 10X biotite

52 muscovite 2'/. s illimanite IX anthophyllite

331.5-332.5:Gradational weak altered patch QEP 10X visible feldspars

None

HOLE NO: UL-29 LOGGED BY: S.C.SIM PAGE:

* ^4

4

f FROM ROCKTO TYPE

^

*

^

S

*

9

342.7 GAKBRO* to

431.5

9

9

9

9

9

w w

DRILL HOLE LOG

GRAIN ANGLE 10COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

335.0-335.5:Well foliated unaltered 2X euscovite NoneQFP sill25X flattened qts eyes10X white feldspars

335.6-335.7:Granitic dyke e "70"

Gradational weak/unalteredpatches QFP at:337.3-337.8339.1-339.4339.6-339.8340.0-340.4

340.6: 5cm granitic vein

341.2-341.8:Fg massive gabbro dyke 23! diss pyriteSharp contacts e 60"

Dark eg Massive gabbro locally 2 X leucoxene Rare tr diss pyritegreen to grading from eg to vcg. lop 7m cut by 3X qtswith 369n 1.5n fg 'chill* zone at and carbonate veinletswhite mg top contact 8 75" at 30-50' to CAspots below

White siliceous graniticdykes at:

350.8-351.0 S 45'353.4-354.5 B 55'

358.5-359.6:l?3 weak foliated feld.phyric int. dykeSharp contacts 8 75'

Similar int. dyke at362.4 to 363.0 e 75'

C*

9

Gabbro grades to 1113 at 369m with very weak foliation 6 70-75


A

Jt

J

DRILL HOLE LOG

FROM ROCK TO TYPE COLOUR



White siliceous graniticdykes at:

371.9 - 5cm B 50" 372.4-372.6 0 60"

Eg massive locally feld. phyric int. dykes. Commonly with irregular contacts at:

380.8-381.0 8 75"381.3 - 6cm381.6-381,9383.1-383.3 d '70"383.6-384.0

382.0-382.9:Pink granitic dyke Q 60"

382.9-383.1: Qtz vein B "75"

White aphan- 384.4-388.4:with itic White massive qts veingreen with sharp fracturedveinlets contacts 8

Locally 'vuggy 1 along qts/carb veins Klcin) S

389.5-389.8: Moderately foliated, fg intermediate dyke. Sharp contacts S

Cut by 2X black chloritic veinlets (often py mineral-

30-35' ized)

0-15"

75"

2X pyrite over section in clots up to lcm associated with dendritic veining

7Z black stretched chloritic clots (Onn)

389.9-390.7:Sum to 2noi carb veinat O" to CA


J

f

3

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



Pink with nig 390.6-394.7:black Massive to well foliatedstreaks granitic dyke.

Sharp contacts 8 75"

Major qts veins at:394.4-394.55 B 70-75" 394.6-394.65 8 70"

394.7-395.2:Well foliated fg feld.phyrie int. dyke B 75"

396.5-397.1:Massive fg chloriticnafic dyke B *45"

396.8-397.3:Blocky ground withnumerous fractures alongqts S chloritic veins B 10-20 0Minor slickensides.

400.0-400.3:Chloritic mafic dyke.Sharp contacts B 70"2cni chloritic grunge at400.1 B 45"

401.0-401.4 S402.6-403.1:Fg well foliated feld.phyrie int dykes 8 75"

404.5-405.0:Blocky ground with "dry"fractures along qts/epidoteveinlets

407,7: 5cai qta/ep healed breccia sone

Cut by 3X qtz/qtz-carb veinlets at shallow angles (0-10 0 to CA)

IX py clots -Claim

10X chloritic streaks/clots U5ma)

Possible fault?

Fault


e4*

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



Phlog defines foliation 8 75-80"

Eg massive to weak foliatedintermediate dyke at:

410.3-411.0 B 50" 411.9-412.0 8 70" 412.1-413.3, top S 1 0"

bottom 8 50" 414.3-414.8 8 70" 415.1-415.4 8 65" 416.6-416.9 5 50" 417.4-418.2 6 70'

418.2-418.9:Well foliated highly feld.phyric int. dyke B 80"Similar dyke at 420.8to 421.4 8 75"

Ir phlog begins at 408.7m (no leucoxene) increasing to av 9 . 5X at 412m.

FS aphyric int. dyke at 424.7-424,9 8 75"

430.3-430.8:Weak feld. phyric massiveint. dyke 0 70"Similar dyke at 431.0to 431.1 B 65"

431.5 TRANSITION Green to ZONE with 434.3 GAB&RO brown

wisps

eg Typical ultra-mafic unit with gradational upper contact defined by loss of feldspars. Well foliated defined by phlogopite l?

431.9-432.1: Granitic veins over 60X section

BX phlogopite over section None

80"

HOLE NO: UL-29 LOGGED BY! R.C.SIM PAGE: 16

1t

* FROM ROCKTO TYPE

Tt

J

J 434.3 MEIA-to PER1DO-

j 472.5 THE

j

J

^

.

J

jl

J

^

^

j HOLE NO:

J

1 ^

DRILL HOLE LOG

GRAIN ANGLE TOCOLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

433.0-434.1:Fg weak feld. phyricint. dyke.Sharp contacts B 75"Qtz vein at 433.05to 433.15 B 75 s

Steel ng Typical Magnetite richblue/grey to (25X) Massive ultra-uith eg nafic unit.black Top contact faulted S 60" Faultspots (marked by occurrence

of magnetite)5cm chloritic breccia

439.5: 153! chilleddendritic diabaseveinlets ^lcm over 10cmsection

440.0-441.0:Numerous fractures oversection along chilledU/M veinlets K2nni)

447.0-447.8:Fg Massive non-magneticmafic dyke.Sharp contacts S 45"Numerous fractures alongchloritic veinlets

447.9-450.0:Well foliated siliceous 10X biotite clotsgranitic dyke @ 80"

450.1-450.7:Siliceous granitic dyke.Sharp contacts, top S 4 0"

bottom 8 SO 0

UL-29 LOGGED Bif: R.C.SIM PAGE: 17

DRILL HOLE LOG

EROH 10

ROCK TYPE COLOUR



452.9-453.0: Chloritic blocky/ grungy sone 8

453.0-453.4: Siliceous granitic dyke cut by 15X black chlor itic veinlets 8 Sharp contacts 8

454.1-454.4:Massive 113 aafic dykewith numerous fracturesalong pervasive biotitebands

460.5-460.7: Chloritic, blocky fault zone with 2cm grur^e at 460.5 e

460.8-461.4:Fg massive feld. phyricint. dyke 8


Feld, phyric int. dykes at: 462.9 - Sem 8

463.2-464.0 8

•75"

30" *70"

FaultC

C

Fault

"70"

65 0

80"

SO 0 50"

Px gradational becomes greenish with black spots at 464m.

Feld. phyric int. dykes at: 465.4 - 7cm 8 70"

465.8-466.4 0 75"

HOLE NO: UL-29 LOGGED BY: R.C.SIM PAGE: IB

DRILL HOLE LOG

FRQH TO

ROCKnpE COLOUR



2cm chloritic grungeat 466.1m 8 "75"

Blocky chloritic corefrom 466.4-467.3,minor grunge at 466.6m S 7 5"

469.0: 5cm feld. phyricint. dyke with sharpbiotitic contacts 8 70"

"471.5-472.5: Gabbroic chilled base to sill.

Fault

Fault

472.5 QFPto548.0

Grey with tig Generally a massive weak/white spots

unaltered matrix supporting 25X qtz eyes K4wn) and avg. 10X visible cloudy white feldspars. Sharp qtz veined upper contact 8

476.7-476.B: Granitic dyke 8

Massive, vfg, light grey intermediate dykes at: 477.2-477.4, top B

bottom l? 478.3-479.6, top l?

bottom 8

482.4-483.4: Fg well foliated intermediate/gabbroic dyke Sharp contacts S

65"

55"

70" 45" 25" 70"

70"

Very weak incipient cordierite alteration to unaltered

Cut by 3X qtz, carb 1 hen veinlets KSsin) over top 5m.

2 X magnetite blebs U'lmai)over top 5w.y. rare tr diss pyriteoverall

Incipient/unaltered QFP


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR

GRAIN SI2E TEXTURE AND STRUCTURE

ANGLE TOCORE AXIS ALTERATION SULPHIDES

2X pyrite clots

REMARKS

483.5-483.9 and484.5-484.B:Cg massive graniticdykes, sharp contacts 8 70"

485.7-486.4:Fg well foliated int/gabbroic dyke, same as482.4 B 75"

488.9-489.6:Massive to wk foliatedfg gabbro dykeSharp contacts B 75"

492.3-493.0:Chloritic mafic dykeSharp contacts 6 65"

496.9-497.0: qtE vein 8 -70"

497.0-497.5:Fg locally wk foliatedfeld. phyric int dykeSharp contacts 8 70"

498.5: 5cm chloriticiiafic dyke 8 75"

501.0-501.3: Carbonate vein section (10X carb veins)

502.8-503.2:Well foliated weakly feld.phyric int. dykeSimilar to 497.0Sharp contacts 8 70"

504.8: 6cm granitic dyke S 55"

Cut by 10X qtE veins

Sem granitic vein at top contact

Patchy pink hematite stained due to 3X veinlets (hen/carb/qtz)

37. muscovite

HOLE NO: UL-29 LOGGED R.C.SIM PAGE: 20

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



9

i

i

3

J

t

J

J

Pink and white eg granitic dykes at:512.1-512.8 6 10"515.5-515.95 very blockyover bottom 0.3ni516.2-516.7 8 60"

519.5: Sen chloriticmafic dyke 8 70"also S 5 19.9-520.0 Q 60"


Hoderate to well foliated S 70-75"

521.95-522.0 and 527.5-527.8: Fg weak foliated inter mediate dykes 8 "70" also at 527.5-527.8 8 70"

and 529.0-529.5 S 75"

533.6: 5cm chloriticmafic dyke i? 80"

533.65-533.75!60X granitic veiningover section 8 80"

505.5-506.5:Pink, hematite stainedQFP cut by 7Z chloriticveinlets

8 " 520o: OEP gradationally becomes noderately altered over lw to: +35X cordierite 10X biotite 3-5X Muscovite

Ir diss pyrite 'Patchy 1 altered QFP


DRILL HOLE LOG

10ROCKTYPE COLOUR



534.9-535.2: Ueakly chloritic well foliated fs intermediate dyke, sharp contacts 8 75"

537.8-537.9 and538.9-539.0:Mg nassive granitic dykes S * 70"

539.4: 10cm fractured zone along carbonate veinlets

Granitic dykes at: 540.3 - 6cm S 540.5-540.7 B 542.1 - 5cm l?

546.2-546.7: Mafic clotted altered int/felsic dyke. Probable syn-volcanic QFP dyke with 10X chloritic amphibole clots Onn

70" 70" 70"

20X cord 3X biotite

548.0 SILICEOUS Mottled fg to GARNET- grey/ 705.9 IFEROUS green

ALTERED .with pink SEDIMENTS spots

A Massive to weak foliated fg matrix of qtz/cordierite/ biotite S amphibole support ing anhedral pink garnets (,1cm)

Moderate alteration: +30X cordierite 3Z anthophyllite 2 X biotite avg. 5X garnet

Ir py in clots often associated with garnets 2 X fg disseminated pyrite throughout

Localized siliceous bands (gradational) rarely enveloping garnets. Patchy chloritic mafic clots often define foliation 8 Sharp biotitic upper contact with QEP S

548.2-548.4: Granitic dyke @

"55"

45"

548.0-548.2:35X biotite over section


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR


ANGLE tO CORE AXIS ALTERATION SULPHIDES REMARKS

548.4-548.6:Clotted qta 3 graniteover section 8 "50"

Granitic dykes S veinsat: 556.4 - 3cm S 85"

556,8 - 3cm 0 75" 559.1-559.2 8 75"

559.9-560.2:Black chlorite healedbreccia zone with lcmchlorite/carbonate grungeat 560.0 8 40"

553.5-554.5:4X carbonate vein letsover section avg. 40" to CA

Fault

y

j

j

t

j

j

J

j

ronurc icra qia vein v *w

566.9-567.1:Siliceous granodioriteclot - very irregularcontacts e 0-70"

Grey fg 568.0-570.2:with Massive to weak foliatedwhite feld. phyric int. dyke.spots Sharp upper contact 6 65"

Cut by granitic/grano-dioritie dvkes 8 56S.2 - 5cm,569.1-569.2569.3-570.0

560.7: 3cn intense qtz/epidote veinlets (70X oversection) e 55" to CA

8 " 565.5m: siliceous rinsabout garnets gradationallybecomes nore common.Biotite increases to avg. 52

HOLE NO: LOGGED BY: R.C.SIM PAGE: 23

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR

BRAIN SIZE TEXTURE AND STRUCTURE


570.2-570.4:Composite qts/granodioritedyke. Irregular contacts.

570.8-572.5:FS massive feld. phyricint. dyke B 70"

573.5-573.8:Massive 1119 granitic dyke 0 45"

578.0-578.7:Massive fg chloritic maficdyke. Sharp contacts @ 70"

B 580.0 S 580.4: Two l x 3cm anthophyllite rich clots envelope up to l OX. euhedral magnetite up to 5mm.

580.9-581.2:Hassive granitic dyke 8 *70"

582.7-583.1:Well foliated feld. phyricgabbroic dyke 8 75"

584.9-585.4:Eg weak foliated dyke/weak altered sediments. Gradational contacts over 2em

8 "573m: sulphides increase to avg. 1-2X py in localised clots associated with garnets commonly magnetite becomes patchy 0-2X

2X garnet

585.8-589.0:Pervasive altered sons insediments5X anth. 302 bio, 652 cord.

Same as pervasive zone in top of seds in UL-2&

HOLE NO: iJL-29 LOGGED BY: R.C,SIM PAGE:

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR


ANGLE CORE

10 AXIS ALTERATION SULPHIDES REMARKS

J

J

J

Green with white spots

f3 to mg

Generally has good foliation defined by Mafic clots in matrix 8 75-80"

@ 590m: Seds altered to:+40X cordierite+ 10Z biotite3-5X anthophyllite7-10X garnet {± silica rims)

595.5-595.8:Moderately foliated weaklyfeld phyric int dyke UOXnafic clots)Sharp contacts S

596.4-596.9:FS int dyke, massive with sharp contacts S Similar dyke at 613.1- 613.5 e

615.4-615.5: Granodiorite dyke Irregular contacts

619.2-620.5: Eeld phyric int dyke Sharp upper contact B Grades over several em's to fg massive chloritic dyke with sharp lower contact S

627.5-634.5:Well foliated equigranular gabbro dyke with 20-30cm chill zones at contacts 8 Cut by pyritic qts vein at 634.2-634.3

1-2X po, tr-lX py in clots often associated with garnets

593.85: 3mm pyrrhotite vein/ band parallel to foliation

593.9: lew x 4cm po clot

75"

80"

80"6 614m: Biotite has increased to avg. 15X

80"

70"

70"

Pyrite rich qta veins at: 620.7 - Sum 621.6 - 6mm 622.4 - 2nn

HOLE NO: WL-29 LOGGED EY: R.C.SIM PAGE:

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



641.2-641.3:Siliceous garnetiferousdyke 0

Moderate to well foliated i

70'

70-75"

646.5-646.9:Irregular qts veins l clotsover 75X section

Massive to well foliatedto almost banded (locally) 8 75-80"

660.1-660.6:Well foliated fg gabbrodyke i? 75"

636.1-636.6:4X pyrite clots over section(associated with garnets)

3X sillimanite 3X garnet

0 "645m: sediments altered to: +50X cordierite

10-15* biotite 10X garnet 12 avg staurolite Uocally up to 4X eg: 645.7-646.0) 1-2X gahnite 1-2* anthophyllite Tr-2X sillimanite

1-2X py, 1-2X po in streaks and clost (tr cp)

Very altered garnetif erous sediments

105; pyrite, 5X pyrrhotite over top 10cm in qts vein

655.3: Several snail i'2mm streak clots chalcopyrite (similar to clots py S po) 15X cp over l en

S 655.5: gradational over0.5m decrease in alterationof sediments30X cordierite7X biotite1-3X anthophyllite1-3X garnetLocally small more intenselyaltered patches similar toabove do exist in this unit

HOLE MO: LOGGED BY: K.C.SIM PAGE: 26

DRILL HOLE LOG

FROM 10

ROCK TYFE COLOUR



668.9-669.2:Massive t 1) feld phyricint dyke e

670.0: 5cm grano diorite dyke 9

676.3-676.4:Highly feld phyric UOX) massive int dyke i? also at 681.8-682.1 6

686.1-686.3 l 686.7-687.2: Well foliated dykes 8

gabbroic

"80"

80" 75"

75"

"670.5-676.0:Tr-lX vfg diss sphaleriteover section

692.5-692.7 S692.95-693,05:Cttz veins containing 30Zangular host fragments

693.3-693.5:Blocky chloritic fault zonewith ainor grunge B

Fault30 0

699.5-700.7!Fg well foliated gabbro dyke S 75"

705.9 INTER- Grey with fg Generally a massive but to MEDIATE rare pink locally weak foliated 724.3 SEDIMENTS spots defined by crude siliceous

bands SLocally gradational sonesof garnetiferous sedimentsoccur .

"80"

Generally weak altered 10X cordierite 3X biotite 1-2X anthophyllite 0-5X garnet

IX py, IX po in localisedclots (often associatedwith garnets)Patchy tr-2X fine dissmagnetite


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



Massive to weak foliated feld phyric int dykes at: 708.7-709.2 6 SO 0 714.3-715.5 0 75' 716.7-717.3 6 75"

715.5-715.t: Qts vein B 70"

715.6-715.8:Blocky, chloritic,carbonate veined grungyfault Bone 8 70-80"

Granitic dykes at: 716.0-716.2 716.3-716.4 715.5-715.6

723.1-724.2:Massive weakly feld phyricint dyke 8 65"

Fault

724.3 WEAK to ALTERED 736.6 OFP

Salt g pepper

mg Massive to very weak foliated equigranular intrusive (?) with sharp contacts, top 2cv chill 8

bottom 20ca chill S65" 70"

Very weak/unaltered 5X cordierite (?) 2-3X biotite

Cut by 2X qtz, ep,

Rare tr diss pyrite

carbonate veins U'5mm)

724.7-724.9:Siliceous granitic dyke S * 70 0

727.0-727.5:Irregular garnetiferousgranodiorite dyke

727.5-728.5:raft/xenolith garnetiferousaltered sediments in QFPSharp contacts S 7 5"

HOLE NO: LOGGED Bt: R.C.SIM PAGE: 28

-)

•)

DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR


ANGLE TO COKE AXIS ALTERATION SULPHIDES REMARKS

735.6-735.8:Massive int dyke with 302 host (OFF) foments Sharp contacts B 70"

736.6 INTER-to 780.2

MEDIATE 10GARNET IFEROUS SEDIMENTS

J

J

J

Mottled fg Massive to aoderately grey with foliated defined by pink spots micas and siliceous rims

enveloping garnets (where present) 8 75-80 0

739.4: lcm chilled diabasevein 0 80"

747.3-747.6:Fg weak foliated gabbrodyke 8 80"

751.1-751.3:Garnetiferous granodioritedyke 6 70"

754.5-755.4:Fg int dyke, well foliated defined by chloritic mafic streaks 6 75"

755.4-757.0:Fg weak foliated gabbroicdyke 6 75"

Well foliated 8 70-75"

+30X cordierite7Z biotite

2-7X garnet (locally up to 15X over 30cn sections)

Cut by 2X garnetiferous siliceous veinlets K2cn)

IX py, IX po clots associatedwith garnets commonlyIX diss magnetite throughout

e "760m: Garnets become rare35X cordierite 12X biotite 2'/. anthophyllite

Avg 5X garnet (i silica rims)

IX po, IX py disseminated and in clots associated with garnetsUp to 2X magnetite locally, associated with garnets

Gradation to 'inter mediate" sediments below


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



774.0-774.1 3 775.4-776.0: Granitic dykes l? "75"

8 *772m: anthophyllite increases to avg 3X (locally up to 6X over 0.5m sections)

33! garnet in granite

780.2to829.3

PATCHY GreyALTEREDINTER MEDIATESEDIMENTS

f9to

vfq

Generally massive to verylocally weak foliateddefined by micas andanthophylliteVery rare 9rad3tional

Seems to be quite altere70-75" +50X cordierite

15X biotite5X anthophyllite

d Rare traces po l po Very non-descriptcommonly in streaks (boring) unit

aones of garnetiferous sediments (as above) Upper contact defined by decrease in garnets (gradational)

Fg massive mafic dykes at: 793.3-793.4 S 75"

794.2 - 5cm 6 60"

800.2-800,4:Massive fg feld phyricint dyke 8 SO"

Massive eg granitic dykes at: 802.2-802.6

803.0-803.3 8 60"803.7-803.9 8 *60"805.0-805.7 S "60"

804.3-804.8:Fg massive feld phyricintermediate dykeFoggy gradational contactsover lcm 8 " 75"

Feldspars stained pink

30X section pervasive biotite fragments

IX diss pyrite


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



811.6-812.1:Massive granitic dykingover 7 57. s ection 8

818.0-818.2:Fg Massive feld phyricint dyke, same as 800.2 8

818.2-818.5:Massive mg granitic dyke S

821.2-821.4:Blocky core with chloriticslickensides 8

Granitic dykes 8 1 822.4 - 5cm 8 825.0 - 5cm B 827.1-827.2 8

629.2-829.25: Granitic vein 8

"40"

70"

*60"

*45"

"80" "75"

*60"

Feldspars stained pink

Fault

Alteration in sedimentsgradationally decreases at" B25ia:+30X cordierite3-5X biotiteTr-2X anthophyllite

2X Magnetite, euhedral

829.3 ALTERED Streakyto SEDIMENT/ grey S830.05 TUFF brown

fg Well foliated to almostbanded unit on mw-cm scale S 70-75' Sharp upper contact 8 80"

Preferential alteration in gradational bands (Ocn) 40X cordierite 10X biotite 5X anthophyllite

27. py, IX po in disseminated streaks parallel to foliation IX sphalerite over bottom lOcw in disseminated bands parallel to foliation


DRILL HOLE LOG

FROM 10

ROCK TYPE COLOUR



803.05 MASSIVE Light fgto lyLPHIDii brown/ to830.15 beige vfg

Approximately 35X sectioncomposed of white qtswhich cuts sulphides B "65"Top 4cm sulphides arealmost aphanitic andseem to be banded on avery fine (sub-dim) scale B 75"Sulphides support 10!! qtzand bio/anth/cord fragmentsin which sulphide veins areinjected.

830.09-830.12:Qts vein - somewhat irregularwith 1 07. sulphide veins

830.12-830.14!Orange coloured band composed of "&OX rounded siliceous (qts) fragments Klmm) enveloped in sphalerite and minor py.

830.14-830.15:Qtz vein similar to above

Fragments over top 2cm are tiainly unaltered qts below frags or altered to bio/ cord/anth.

Top 4cm:2X cp enveloping fragments15X pyrite35X pyrrhotite38X sphalerite

6X pyrite4X sphalerite in qtz

10X pyrite 15X sphalerite Ir cp

20X sphalerite veinlets in qta vein

Est: 0.3X Cu in Zn 0.2m CL

Banding of sulphides may be a tectonic feature S not prisary

Orange colour to these qtz 'pebbles' may be due to translucency or they may be chert fragments containing very fine grained disseminated sphalerite

830.15 ALTERED Mottled fg to BANDED grey S to 831.3 TUFF(CLR) white mg

J CRYSTALTUFF(QFP)

Generally a gradationallybanded tuffaceous lookingunit on 0.5-lcm scale e 75-80"Grading into siliceousqts eyes (QFP) sones at:830.5-830.55 and831.1-831.2

830.8-830.95:Feld phyric int dyke e 75"

'QFP 1 sones are basically unaltered (1-2X biotite) Tuffaceous zones are preferentially banded altered to: 35X cordierite 10Z biotite 3X anthophyllite

2X disseminated to clots K2mm) pyrite in tuffaceous zones

QFP zones may be gradational qts eyed crystal sections of tuff

HOLE NO: UL-29 LOGGED 6Y: R.C.SIM PAGE: 32

DRILL HOLE LOG

FROM TO

831.3 to 832.3

832.3 to 851.8

ROCK TYPE

GIZ EYED CRYSTAL TUFF/FLOW (QFP?)

BANDED ALTERED VOLCANIC TUFF (CLR)

GRAIN COLOUR SIZE

Mottled mg grey S white with trans lucent grey spots

Mottled fg to banded grey, brown S white


Well foliated zone defined by qta eyes 8 252 qts eyes K4nnn) Gradational contacts over 5mm f?

Well banded/foliated on 0.5-lcm scale as above 6

ANGLE TO CORE AXIS

75-80"

80"

75-80"

ALTERATION

Very weak to unaltered 3X biotite

Hore mafic bands preferentially altered to biotite (i cordierite) with s i nor anthophyllite connon

SULPHIDES

Very rare trace disseminated pyrite

IX disseminated pyrite throughout (no po) Very localized magnetite up to 3X over Sen sections

REMARKS

This unit is generally loaded with pyrrhotite Here it is not.

832.5-832.6:Feld phyrie int dyke 8 70"

836.8-836.9: Qtz vein 8 75"

837.5-837.6: FS massive chloritic Mafic dyke B 70"

841.05-841.2:Fg aphanitic diabase dykeSharp chilled contacts 8 "45"

841.2-841.5: Gradation qts eyed QFP zone as above, also at 841.7-841.9

846.2-846.6: Massivefg-mg granodiorite dyke S * 75 0

Gradational qtE eyed QFPzones at:847.4-847.7849.0-849.1B49.7-849.9

832.6-832.9:252 biotite over section50X cordierite

3X sphalerite in dendritic ve inlets parallel to banding from 832.85-832.9


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR


AN8LE TO CORE AXIS ALTERATION SULPHIDES REMARKS

850.3-850.6:Siliceous granitic dykecut by numerous qts veinletsDyke contacts 6 65"

851.3-851.8: Gradational QFP zone as above.

851.8 INTER- to MEDIATE 853.5 TO FELSIC

DYKE

Grey to fg Massive feld phyric (2Z)green dyke cut by 4X white qts(where veinsbleached) Fo99y contacts 8

Epidote bleached gradationally frow 852.3-853.2

None

"75"

853.5to854.0

GRANITE

E.O.H.

853.5-853.9:Grey granite dyke, massive.

B53.9-584.0:Mg massive graniteContact e

End of Hole.

80"


ASSAY SHEET

Sample (M) Number From

(m)To Cu Zn Py to Length Cu Zn AS

PP b Au Na2Q Comments

US0901 828.3 829.3 -

0902 829.3 B30.05 - 0.1 2

0903 830.05 S30.15 0.3 11.0 10

0904 830.15 831.3 2

0905 831.3 832.3 -

0906 832.3 832.9 - 0.1 2

0907 832.9 634.4 - - 2

1.0 0.004 0.02 0.5 7 3.04

l 0.75 0.031 0.07 0.8 8 3.05

15 0.1 0.14 6.97 4.9 8 1.23

1.15 0.015 0.11 0.4 5 2.95

1.0 0.004 0.02 0.1 6 4.26

0.6 0.012 0.28 0.5 B 2.53

1.5 0.027 0.06 0.6 9 3.36

Int. seds

Alt sed/tuff

MS

Alt CLR * 15X QFP

QFP

Alt CLR

Alt CLR

HOLE NO: UL-29 PfiGE:

GEQCHEK SHEET

ft

t

ft

*

ft

*

^

*

•ft

*

-

*

*

*

SampleNumber

US08010802080308040805

08060807080808090810

08110812081308140815

08160817081808190820

08210822082308240825

082608270828

HOLE NO

(m)From

6366696126

156189219252285

309339474507522

549579609639672

702711729741771

786816843

(m)To

9396999129

159192222255288

312342477510525

552582612642675

705714732744774

789819846

.-29

__ Estimate..Cu Zn Py

11111

trtr

.--

-....

-112

0.1 1

11

-11

-.

"po

-----

-----

.----

.-111

1--

tr1

.-

(m)Length

33333

33333

33333

33333

33333

333

PPICu

434

136822

2362

124

24

1222

123

1113269

17411548

26

58

PP*Zn

2712651263216129

1162671107051

5734413731

25015420912101002

6416871

25427

386950

ppbAu

76657

575B6

96857

69776

96775

577

XX XNa2Q Si02 Ii02

0.420.641.360.900.58

0.140.141.442.340.08

0.632.361.324.402.82

2.762.592.021.823.31

2.713.384.11 69.60 0.590.952.76

2.731.772.81

Comments

Alt. QFPAlt. QFPAlt. QFPAlt. QFPAlt. QFP

Alt. QFPAlt. QFPAU. QFPAlt. QFPAlt. QFP

Alt. QFPAlt. QFPIncipient QFPIncipient QFPAlt. QFP

SGSSGSSGSSGSSGS

SGS•Inf SedsQFP (incipient)Int/SGS sedsSGS

Alt. Int. SedsAlt. Int. SedsAlt CLR

PAGE: 36

HOLE NUMBER: WL-30CORPORATION FALCONBRIDGE COPPER

DRILL HOLE RECORD Imperial Units Metric Units X

PROJECT:

GRID:CLAIM NUMBER:

LOCATION:DATE STARTED:

DATE COMPLETED:

PN370WINSTON LAKESELCO

FIELD

SURVEY

COORDS:

COORDS:Pick Lake Grid

OCTOBER 30, 1985

LAT:DEP:

ELEV:LAT:DEP:

ELEV:

4+20S1 + 75E430mU6+65N33+50E


FINAL DEPTH:

RQD LOG:PULSE EM SURVEY:

3000-82 0

BQ460m

X

CONTRACTOR:CORE STORAGE:

CASING:PLUGGED:

MULTISHOT SURVEY:COLLAR SURVEY:

MCKNIGHTCLEAVER2.7m BW

X

DRILLINGLAKE

PURPOSE:

Depth

6306090120150180210240270300330360390410450

ACID TESTS Corrected Corrected

Angle Depth Angle

-82-81-79-78-77-76-75-74-73-73-72-71-69-66-64-63

TROPARI TESTS

Depth Azimuth Dip Depth

3595155215275335395455

MULTISHOT DATA

Azimuth

300306299 ?309309308309315 ?

Dip

-81-77-76-74-73-71-66-62

HOLE NO: WL-30 LOGGED BY: R. C. SIM

DRILL HOLE LOG

FROMTO

0 to2.7

2.7to37.9

ROCKTYPE

CASING

ALTEREDQFP

GRAINCOLOUR SIZE

Mottled fgto streakyblue/greyi lightgrey

ANGLE TOTEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

Typically well foliated Moderately altered V. trace diss pyritedefined by qtz eyes (257.) 357. cordieriteand micas @ 60-65 0 77. biotite

2-47. anthophylliteTr-27. muscovite

2.9-3.0:Siliceous epidote stainedqtz/granitic vein @ 65

5.8-6.6:Massive mg granitic dyke @ 35

8.8-8.9:Massive fg int. dyke @ 600

8.9-8.95:Granitic vein with irregularbottom contact

10.9-11.05:Siliceous epidote stainedgranitic dyke, similar to2.9m @ 500

12.0-12.3:Massive fg magnetite rich(47.) chloritic mafic dyke @ 45 0

13.8-14.0:Granitic dyke @ 550

14.1-14.2 and15.4-15.5:Massive fg int dykes @ 50-600

57. muscovite flakes

12.3-12.7:37. gnt, 27. euhedral magnetite( 4mm) in QFP


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



15.5-15.9:Moderately foliated Int/mafic dyke, 207. chloriticmafic clots definingfoliationSharp contacts @

18.2-18.3:357. irregular qtz clotsover section

Granitic clots at: 19.4 - 4cm 19.9 - 10cm

20.5-3cm carbonate rich grunge zone supporting 507,, siliceous qtz fragments @

Mottled fg 20.9-24.4:dark grey A massive intermediate dyke4 black with 307. ghostly amphibole

rich mafic fragments ( 3cm)often weak stretched definingfoliation @Sharp contacts to dyke @

28.4-29.2:Granitic dyke, massive,mg-cg @

32.1-33.1:Massive fg int. dyke, similar to 20.9 with several mafic fragments visible at 32.3m Sharp contacts @

Blocky core ("dry" fractures) at: 33.3-33.5, 34.0-34.2,

34.8-35.0, 35.7-35.9 Fractures mainly along veinlets, not fault related.

55"

350 Fault

17. disseminated pyrite

65 U SO0

60C

500

57. muscovite

Cut by 37. hematite/ carbonate veinlets

27, diss pyrite


DRILL HOLE LOG

FROM ROCK TO TYPE

37.9 GABBRO to 96.1

GRAIN COLOUR SIZE TEXTURE AND

36.8-36.9:

37.9-39.0: 407. gabbroic supported by

ANGLE TO STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

Granitic dyke © 60O

fragments epidote, qtz

Green with white spots

i chilled int dyke mat'l. Chlorite/carbonate grunge zones at: 38.1 - 5cm

38.7-38.839.0 - 2cm

mg Below 39m, gabbro is wellfoliated, equigranular @ 60

42.3-42.5:Fg massive gabbroic dykeSharp contacts @ 60

43.6-44.6:Very blocky chilled int.dyke Abundant grunge throughout. Fault zone @ 10C

Fault zone @ 0-20 (?)

Feldspars pink hematite stained to 42m 2X powdery light brown leucoxene to 43.6m, numerous qtz A qtz/carbonate/hematite veinlets cut to 6m of section

43.4-43.6:Feldspar stained lightgreen (epidote)

Cut by IS'/i qtz/carb veins

Rare tr diss pyrite

Fault

44.6-44.8, 45.1-45.2 8.45.5-45.7: Granitic dykes @ 30-400

46.3-46.5:Massive qtz vein supporting15X host fragments. Contacts @ 60O

51.4-51.6:Fg massive feld. phyric int.dyke @ 60"

lcm pyrite clot @ 46.4m

HOLE NO: WL-30 LOGGED BY: R .C.SIM PAGE:

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



56.6-57.2: Granitic dyke @4CT also a t 60.9 - 7cm @ 55 0

62.8-63.3:Massive white qtz vein @ 450

64.8-65.2 8. 65.7 - 7cmGranite dyke @ 50O

66.0-66.2 i 66.4-66.5:Fg massive intermediate dyke @ 65

67.8 - 5cm composite qtz- qtz/epidote vein with frac tured contacts @ 30

70.6-71.0:Fg weak foliated intermediatedyke. Contacts © 550

Massive fg feld phyric int.dykes at:

72.3-72.9 @ 700 75.3-75.9 @ 650 76.6-77.2 @ 550 77.4-77.6 @ 550

Granitic dykes at:78.3-78.4 @ 55078.6-79.4 @ 65079.5-79.7 @ 60080.2-80.5 - 507. of section81.8-82.0 @ 60082.1-82.4® 600

82.9-83.1 b 85.8-86.2: Fg massive int dykes cut by ID-15% garnetiferous sili ceous granitic veins Sharp contacts @ 50-600

Granitic dykes at:90.1-90.2 @ 65091.1-92.6 @ 650

Trace phlogopite begins at 80m in gabbro

47, garnet over sections

Avg. 47. phlogopite at 90m


DRILL HOLE LOG

t

t

tFROM TO

ROCK TYPE



96.1 TRANSITION Green to ZONE with 96.6 GABBRO brown

streaks

95.5-96.1:Mass.fg feld phyric int dyke @ 600

eg Well foliated ultra mafic @ 500 77. wispy clots phlogopite typically chloritic

None

96.6 INTER- Dark grey fgto MEDIATE96.9 DYKE

Massive blocky dyke cut by 57,, chloritic veinlets Sharp contacts @

Possible fault @ 60 (?)

65U

96.9 META- Steel mg to PERIDO- blue/grey to 130.1 TITE with eg

black spots

Typical massive equigranular magnetite rich (257,,) ultra mafic

Chloritic fractured zone at:104.7 - 5cm and109.5 - 10cm

probably not faults.

120.2-120.3: Granitic dyke @ 600

126.8-127.0:Grungy chloritic fault zone @ 60

127.1-127.5:Similar grungy fault zone0.25m cave &L mud 600

127.5-130.1: Non-magnetic gabbroic chill zone

129.4-129.5: Granitic dyke @ 75 0

207. granitic clots ( 3cm) over bottom 20cm

Cut by 17, carbonate veinlets None

Gradational biotite rich (up to 707,) zones at:111.8-111.9112.8-113.1115.2-115.6

Biotite zones (as above) at 120.3-120.5 122.8-123.2

Fault

Fault zone

37, pyrite clots associated with granite


DRILL HOLE LOG

FROM TO

130.1 to 199.3

ROCK TYPE

INCIPIENT ALTERED QFP

GRAIN COLOUR SIZE

Mottled fg to streaky blue/grey 81 white


Well foliated defined by siliceous streaks A biotitic mafic streaks ® Sharp upper contact @

ANGLE TO CORE AXIS

60-650 650

ALTERATION SULPHIDES

Weak altered Tr diss pyrite 20-257. cordierite Avg. 7-107. biotite Tr-1% muscovite Patchy visible feldspars

REMARKS

Incipient altered QFP

133.4-134.5, 135.1-135.58. 138.2-138.6:Chloritic biotite rich fgwell foliated mafic dykes @ 50O

Granitic veins at:137.7 - 4cm @ 60O 139.6 - 6cm ® 60O

139.9-140.3: Mafic dykesimilar to above @ 500

Massive mg granitic clots at: 143.9-144.0 @ 450 145.1-145.3 @ O0 146.1-146.4 @ 550

Massive fg feld phyric int/mafic dykes at:

151.5-152.4 @ 650 154.5-154.9 @ 700 157.2-157.7 @ 600

157. biotite

Granitic dykes at:156.6-156.7 @ 650 158.7 - 5cm @ 45 0

Massive granitic dykes at:161.1-161.9 @ 45C 165.6-166.2 @ 600

Cloudy white feldspars ( 2mm) become common in weak altered QFP at about 155m.


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



Dark fg green/grey

Well foliated 65-70"

Massive granitic dykes at:171.4-171.5 @ 75 0 173.6-174.1 @ 600 174.3-175.3 @ 700

175.3-177.4:Massive aphyric intermediate dyke.Sharp contacts, top @ 700

bottom @ 450

Massive granitic dykes at:177.6-177.8 @ 450 178.3-178.45 @ 500 178.8-179.2 @ 75 0

179.8-180.5:Fg weakly feld phyric int.dyke. Massive, sharp contacts @75

Granitic dykes/veins at: 180.9 - 6cm181.2-181.3 @ 350 183.5-183.6 @ 450

Fg massive aphyric intdykes at;

185.4-185.5 @ 650 186.0-186.1 @ 600

At about 167m: alteration in QFP gradationally increase over 1m to:

Tr diss pyrite Tr-1% diss magnetite

"Patchy" alt. QFP

87. biotite1-27. anthophylliteAvg. 47. muscovite


DRILL HOLE LOG

FROM TO

ROCKTYPE COLOUR



188.9-189.7:Fg intermediate feldphyric dyke with 1 5'/,chloritic/amphibole clots(l x 5mm) definingfoliation ©Sharp contacts @

194.1: 5cm siliceous granitic vein

65" 700

27. anhedral garnets 5mm from 198.3-199.3

199.3 SILICEOUS to GARNET 367.8 ALTERED

SEDIMENTS

Medium/ dark grey

5-207, dark grey-black streaks and "clots" of mafic (amphiboleAbiotite)) material up to 3mm x 25mm in a fg medium grey homo geneous intermediate matrix.This resembles the upper volcaniclastic unit (ie CLR)

3-1 y/, anhedral to sub hedral garnet up to lcm with local concentrations (157.) of smaller l-5mm garnetsThe garnet is locally rimmed or sits within a siliceous patch.

0-27. diss py as diss. streaks and blebs

41

41

*

4*

41

217.2-221.2: Fg ash? of intermediate composition - massive, weak banding, little or no garnet

214.6-215.0: 3-57. blebby py

Volcaniclastic material

Granite dykelets: 204.5-204.7 @ 70-900 207.0-207.2 @ 700

Mafic dyke: 207.65-209.3

212.7-214.0:Fg medium greenish-greywith mottled appearancedue to qtz patches anddark grey amphibole?patches.

220.5: Epidote fracture at 45 0

220.3-220.5:Several narrow epidoticfrac. fillings

HOLE NO: HL-30 LOGGED BY: R .SIM/P.SEVERIN PAGE: 9

41

e

c

o

a

e

o

4

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



Black with pink S, white spots

fstomg

@ 232m: mafic clots have graded to typical silica rimmed gnt seds.

237.5-238.3: Pervasive well foliated biotite supporting T/, qtz frags ( 7mm) 81 cut by irregular granitic vein at 239.0 - 5cm Contacts to biotite gradational over 3cm

239.5-239.9:Foliated fg feld phyricint dykeSharp contacts @

241.5-246.8:Well foliated locallyfeld phyric intermediatedyke. Top 1.0m of dykebecomes very siliceous Aupper contact is hard todefine.

243.2-243.7: Fg massive int dyke, sharp contacts @

+407. cord 157. biotite Avg. 67. gnt

+S57. biotite

17. diss pyrite

Granite dykelets225.35-225.7230.7-231.0233.0-233.1233.6-233.7

226.4: 2cm qtz-epidote veinlet containing angular fragments of the metasediment^ .

233.3-234.4: fg with very little garnet Possible dyke but contacts diffuse

37. garnet from 241.5- 242.0 6. 245.8-246.3 (contamination)

1-27. disseminated Si veinlets py throughout Patchy magnetite, locally up to 37. over 20cm sections

65U

HOLE NO: WL-30 LOGGED BY: P.SEVERIN/R.C.SIM PAGE: 10

DRILL HOLE LOG

FROM TO

ROCK TYPE



Blue/grey with pink 4 white spots

fg

244.4-244.5:Granitic dyke © 700

249.3-250.3:Blocky ground with numerouschloritic fractures,5cm chloritic grungybreccia @ 250.2-250.3 @ 600

250.5-250.8:Massive mg granitic dyke @ 55

Generally well foliated by silica rims @ 700

@ approx. 260m: sedscomposed of:+507. cordierite77. biotite17. anthophyllite4-87. gnt {commonly withsilica rims)

244.2-244.3: 87. pyrite over section associated with 2cm qtz vein at approx. 550 to CA

Fault

27. py, tr po to 266m in clots

262.1-262.4:Garnetiferous granodioritedyke ® 750

266.5-266.8:Feld phyric int dyke,fg massive @ 70

57. gnt ( 3mm)

@ approx 277m: garnet content gradationally increases to avg. 67.

Below approx 266m to 277msulphide is predominantlypyrrhotite.Avg. 27. po, tr py in clotsup to 6mm

© approx 277m: sulphides change to 27. py, tr po in clots up to lcm often associated with gnt. eg 277.5 i 280.1 - lcm clot/bands py.

O

G

OHOLE NO: WL-30 LOGGED BY: R .C.SIM PAGE: 11

DRILL HOLE LOG

FROM ROCK GRAINTO TYPE COLOUR SIZE

Black fg with pink to 81 white mg spots


279.0-279.5 6.282.2-283.7: Fg well foliated aphyric intermediate dykes Sharp contacts @

285.7-289.8: Feld phyric intermediate dyke, massive to locally foliated. Contacts @

ANGLE TOCORE AXIS ALTERATION SULPHIDES REMARKS

27. gnt 279.0-279.5

282.2-283.7: 700 Epidote bleached (weak)

Feldspars patchy stained orange Dyke cut by 37,, epidote/qtz

65 veinlets up to 5mm

291.9-292.5:Chloritic/carbonate rich breccia zone cut by 1 57, granitic/qtz veins A clots Numberous fractures @ 50

294.0-295.7:Intermediate dyke, aphyricgrading to feld phyric at295.2m707,, qtz veining from 295.0to 295.2Other feld phyric dykes at296.4-296.6 A 296.7-296.8

304.1-306.2:Patchy foliated feld phyric int dyke, top @ 35 0

bottom @ 700 Cut by granitic dyke at 304.4-304.6

311.2-311.4:5070 qtz veining over sectionin biotitic matrix

315.6-315.8:Feld phyric int dyke @ 600

Fault

Granitic stained orange

@ 300m: sulphides decrease to m py, tr po (avg)


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



320.8-321.8:Fg massive int/mafic dyke @ 500

330.8-332.1:Well foliated mg gabbroic dyke. Siliceous sedimentary xenoliths at:

331.0-331.1 4 331.8-331.9 Similar GB dyke at 332.5-332.6 @ 700

Massive eg granitic dykes at 339.2-339.4 @ 342.4 - 5ctn 342.8-343.1 @

345.2-345.3 346.4-347.2

347.5-347.7 354.4-354.6 354.8-355.0

over 707. section @

50"

600

50"

60U 600 700 750

358.3-358.7:Blocky zone with minorgrunge zones at:

358.3 - lcm @ 500358.6 - lcm @ 50C358.7 - 1.5cm @ 65C

360.4-360.6:Blocky chloritic shear zone @ 45

365.9-366.3:Fg well foliated gabbroicdyke. Contacts @

343.6: 107. py clots in 5cm qtz vein

@ approx 356.5m: silica rims about garnets begin to become patchy orange stained

Fault

Fault

65"

HOLE NO: WL-30 LOGGED BY: R .C.SIM PAGE: 1 3

DRILL HOLE LOG

FROM TO

ROCK TYPE



367.8 WEAK/ Mottled to MODERATELY to banded 630.2 ALTERED light 8.

INTER- dark greyMEDIATESEDIMENTS

fg Massive to moderatelyfoliated, locally defined 75Oby ghostly siliceous bands( 3mm)Small localized gradationalgarnetiferous patches (asabove) do exist.

370.0-370.15:Fg gabbroic dyke @ 7 0O

374.0-374.3:Very blocky zone withnumerous chloritic fractures

386.2: 10cm granitic vein @ 75

387.5: irregular 2cm to 7cm qtz vein

388.1-388.3 8,388.4-388.6:Well foliated mg gabbroicdykes @

Massive mg granitic dykesat: 391.9-392.0 @

394.1 - 5cm @ 394.3-394.4 @ 394.9-395.05 @

396.2-396.4:Fg massive feld phyricint dyke @

55U

60" 800 700 700

55"

Avg 307. cord107, b iotite1-27. anthophyllite

I'/i diss pyrite, increasing to TL\ i n gnt patches Tr-27. patch magnetite

378.5-378.8: Gradational pervasive biotite zone 157, cord, 107. chlorite, 757. biotite

47. pyrite clots at vein contacts


DRILL HOLE LOG

FROM TO

ROCK TYPE



Granitic dykes at:403.5-403.7 @ 60O 406.7-406.9 - irregular 407.2-407.4 - irregular

408.0-408.1:Siliceous sillimanite richgranitic dyke @ 500

408.6-408.9:Blocky zone with 3cmmicaceous grunge at 408.6 © 55

412.1: 7cm granitic dyke @ 70O

413.0-413.3:Cloudy white siliceous zone/ dyke in seds. Contacts gradational over 2cm @ 75

Massive mg granitic dykes at: 418.0-418.15 @ 800 419.8-420.1 @ 500 420.2-420.3 @ 600 422.9 - 5cm irregular 424.7-424.8 @ 65O

427.6-428.7:Fg massive int/mafic dykeContacts @ 75Ccut by 7cm granitic dykeat 428.1Similar int/mafic dyke at429.6-430.2 @ 750

sillimanite

Fault

430.2 ALTERED to VOLCANI- 432.2 CLASTIC

(CLR)

Mottled fg Moderately to well banded to banded to on *mm scale @ grey, aphan- Locally patches exist with black 8c itic mafic clots in felsic white matrix (CLR)

Unaltered to 431.7 with 750 1-27. biotite

increase at 431.7-432.2 to 127. biotite, + 157. cord.

diss pyrite


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



430.9: 3cm granitic vein @ 75

431.2-431.7:More siliceous gradationalzone, may represent a felsicflow or crystal tuff.3cm qtz vein @ 431.25 @ 75C

432.1-432.2:307. clotted qtz veining oversection. Avg lcm veins

37. py, 27. sphal, tr cp over 10cm in clots at contacts with qtz veins

432.2to433.4

MASSIVE SULPHIDES

Milk mg chlcolate to brown 432.5

fg below

Generally a massive sulphideunit with possible very minorbanding (tectonic ?)Mg pyrite rich sulphides toapprox. 432.5m, grading overseveral em's to a homogeneousfg mixture.Top contact sharp but wavywith 2 x .75 cm fragment"plucked off" 8c approx. lcmabove true contact.

80U

432.2-432.25: Est: U Cu 41 cp wispy (banded ?) 60* py30X sphalerite tt't, fragments (qtz A biotite,

less than 3mm)

4cm rounded fragment (CLR) at 432.25 is injected with sulphides (frag covers ^ core)

432.25-432.5:201 frags (121 bio, 8X qtz)enveloped in25X po21 cp52 pyrite

48* sphalerite

432.5-432.95:Sulphides enveloping 20X frags commonly lnm-2mm up to 2cm (14X qtz, 6T. bio)3X cp3X pyrite

357, po mixed with 39X sphalerite

19. Zn1.2m CL

67, p y 27. p o

237. fragments

HOLE NO: WL-30 LOGGED BY: R .C.SIM PAGE: 16

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



Massive with irregular sharp contacts, top @

bottom @

80U 400

Very weak bio/cord

Knife sharp lower contact along 7mm qtz vein @ 70" 4cm bio/cord alt.

fragment (rounded) at 433.3m

432.95-433.15:Weak altered siliceous (CLR)fragments — cut by numeroussulphide veinlets, 7Z totaln. cpVI. po21 Sphalli py

433.15-433.4:Homogeneous sulphides similar to above fragment supporting approx. 15X fragments lmm-4mm up to 5cm3TI cp3% pyrite

35X pyrrhotite mixed with 441 sphalerite

433.4to457.5

ALTERED VOLCANI CLASTIC (CLR)

Mottled to banded grey, black 4 white

mg tofg to

aphan itic

Generally well banded on mm to -t-mrn scale @ 75-80"

Fluctuating alteration reflecting primary comp osition. More siliceous bands less altered. Generally: avg. 15-207. biotite, +307. cordierite

433.6-434.4:Massive mg granitic dykeSharp contacts @ 75 U

Seems to be more altered than footwall rocks generally are at Pick Lake.

433.4-433.6:127. disseminated bands ofsulphides over section onmm scale.37. cp, 27. po, 77. sphal.

To 442.7: CLR generally contains 1-27. py, 1-27. po, tr sphal in clots or disseminated bands

434.6: lcm band with207. sphal, 57. py, disseminatedto streaky.


DRILL HOLE LOG

FROM TO

ROCK TYPE



435.2: 7cm white barrenqtz vein @ 800

436.0-436.2:Fg massive feld phyricint dyke @ 75 0

436.7-437.7:707. highly irregular graniticdyking over section @ 25C

440.4-440.6:Mineralized black A whitebiotite rich siliceous dyke

Core angles locally swirling to O

443.2-443.35:Gradational siliceous zone,may be altered QFP flow?

Localized core angle fluctuations as above

445.5-445.8: 607. qtz clotting (veining) over sections

157. streaky clots but 17. garnet "blob" in bio.

442.3-442.7:47. subhedral garnets oversection ( lcm)

2-37. gahnite up to 2mm *

Avg 1-27. gahnite oversectionPatchy garnet, locallyup to 77. over 20cm sections

47. po, 17. cp, tr sphal, 27. py.

442.7-443.2:107. disseminated to banded sulphides over section 27. py, 17. sphal, 77. po

May be equivalent to po-zone in earlier holes?

443.35- 446.5:Highly mineralized zonesimilar to 442.7Avg. 57. po, 17. py, tr-17. cpi tr-17. sphal (from gahnite?)

446.5-452.6:Sulphides mainly in streaky banded clots, 37. po, 17. py, tr cp, tr sphal.


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



Granitic dykes/veins at:456.55 - 5cm @ 800 456.65 - 3cm @ 750 456.8-456.9 @ 750

451.3-452.2:ft'/, garnet over section

27. gahnite over section

Below 453.5: decrease in biotite to average 87. Avg. 47. garnets

452.6-453.5:Gradational zone withabundant diss bandssulphides.87. p o27o cp17. py17. sphal (from gahnite)

27. po, 17. py in streaky clots Si disseminated

This may be po-zone?

457.5 GRANITE to 460.0

Mottled fg to spotted to grey 81 white

A generally well foliated feldspar porphyritic grey granite. Sharp contacts @ 60

27. diss py 27. magnetite

457.0-457.3:Mg siliceous granodiorite dyke, top @

bottom @

40" 800

End of Hole.


ASSAY SHEET

Sample Number

WS 08760877087808790880

08810882088308840885

08860887088808890890

08910892089308940895

0896

(m) From

430.2432.2433.4433.6434.4

435.2436.7437.7439.0440.4

440.6441.6442.7443.2444.7

446.2447.7449.2450.7452.6

453.5

(m) To

432.2433.4433.6434.4435.2

436.7437.7439.0440.4440.6

441.6442.7443.2444.7446.2

447.7449.2450.7452.6453.5

454.5

EstimateCu

.1.01--

.---

0.2

--trtrtr

trtr--0.6

—

Zn

.19.43.5-0.5

tr---tr

—-0.50.50.5

trtr--0.5

^

Py

16--1

22122

32211

11111

1

Po

.292-2

2-124

11734

33328

1

(m) Length

2.01.20.20.80.8

1.51.01.31.40.2

1.01.10.51.51.5

1.51.51.51.90.9

1.0

ppm Cu

23592602094164205

588565

18263

160101312251439

118142114126492

84

ppm Zn

28616.027.3.437.26401725

274145362407882

813332

334517643015

815143222506263210

639

ppm Ag

0.915.95.70.41.0

0.50.40.60.50.5

0.80.81.60.80.9

0.91.21.71.01.1

0.5

ppb Au

611866

57555

75755

65668

7

-1,0

3.110.932.215.312.90

2.375.102,422.434.51

2.322.201.601.982.35

1.701.842.371.410.85

2.79

Comments

Alt. CLRMSAlt. CLRGR dykeAlt. CLR

Alt. CLRGR dykeAlt. CLRAlt. CLRSiliceous dyke

Alt. CLRAlt. CLRAlt. CLRAlt. CLRAlt. CLR

Alt. CLRAlt. CLRAlt. CLRAlt. CLRAlt. CLR

Alt. CLR


GEOCHEM SHEET

Sample (m) (m) Estimate (m) ppm ppm ppmNumber From To Cu Zn Py Po Length Cu Zn Ag

WS 0864 9 12 3.0 4 52

0865 130.1 133.1 3.0 2 84

0866 162 165 - 3.0 3 43

0867 192 195 - 3.0 22 79

0868 200 203 2 - 3.0 11 198

0869 227 230 2 3.0 31 107

0870 258 261 2 tr 3.0 209 351

0871 297 300 1 tr 3.0 21 87

0872 327 330 2 tr 3.0 8 46

0873 357 360 2 tr 3.0 17 58

0874 390 393 1 3.0 29 48

0875 423 426 1 3.0 15 69

ppb 7. Au Na-0 Comments

7 0.64 QFP

6 4.11 Alt. QFP

6 3.82 Incipient alt. QFP

7 2.71 Alt. QFP

5 2.73 SGS

7 3.34 SGS

6 2.57 SGS

5 1.00 SGS

8 3.71 SGS

5 2.70 SGS

6 3.20 Alt. int. seds.

5 2.53 Alt. int. seds.


1

1

1

'

1

t

J

9

J

J

'

1

J

,

1

4

J

?

t

1

CORPORATION FALCONBRIDGE COPPERHOLE NUMBER: WL-31 DRILL HOLE RECORD Imperial Units Metric Units X

PROJECT: PN370 FIELD COORDS: LAT: 2+90S COLLAR BRNG: 3000 CONTRACTOR: ST. LAMBERT DRILLINGWINSTON LAKE DEP: 2 + 20E COLLAR DIP: -88O CORE STORAGE: CLEAVER LAKE

GRID: SELCO ELEV: 418 HOLE SIZE: BQ CASING: 0.3m EHCLAIM NUMBER: SURVEY COORDS: LAT: 1800N FINAL DEPTH: 510m PLUGGED:

LOCATION: DEP: 3757.5DATE STARTED: OCTOBER 25, 1985 ELEV: RQD LOG: MULTISHOT SURVEY: X

DATE COMPLETED: NOVEMBER 9, 1985 PULSE EM SURVEY: X COLLAR SURVEY:

PURPOSE:

ACID TESTS TROPARI TESTS MULTISHOT DATACorrected Corrected

Depth Angle Depth Angle Depth Azimuth Dip Depth Azimuth Dip

6 -88 030 -87 060 -85090 -84 0120 -840150 -83 0180 -82. 50210 -81. 50240 -SO0270 -780300 -77 0330 -740360 -67 0390 -66 0420 -640450 -62 0480 -580

1

206 310 ? -80265 310 ? -77326 309 ? -71386 307 -66446 306 -62506 308 -58

HOLE NO: WL-31 LOGGED BY: R.C.SIM

DRILL HOLE LOG

FROM TO

0.0 to 0.3

0.3 to 43.0

ROCK TYPE

CASING

ALTERED QFP

GRAIN COLOUR SIZE

Blue/grey fg with white wisps

ANGLE TO TEXTURE AND STRUCTURE CORE AXIS

Typically a moderate to well foliated unit defined by micas 4 sillimanite @ 50O


Intense alteration: Rare tr diss pyrite 1 507. cordierite 107. biotite 3-77. muscovite Patchy 0-37. sillimanite

Muscovite rich granitic dykes at:0.3-0.8 @ 600 0.9-1.3 @ 700 1.7-2.0 @ 500 2.4-3.0 @ top 650 Bottom contact vuggy t* fractured, possible fault @ 100 3.7-3.8 @ ' 500 5.2-5.3 @ 600 '6.4-6.5 @ 600 6.9-7.5 @ 550 7.7-7.9 @ "600

10.4-11.2:Fg massive int, dykeFairly sharp contacts @ 500

11.7-11.9:White siliceous clottingover 707. section

13.0-13.2:Muscovite rich graniticdyke @ 700

Possible fault

37. sillimanite

7.9-8.0:Pervasive biotite zone with numerous fractures along cleavage planes


DRILL HOLE LOG

FROM ROCK GRAIN ANGLE TO TO TYPE COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

13i6-13i8 .Blocky zone with fracturesalong foliation planes(biotitic) - 7cm qtz vein Possible fault?at bottom contactSimilar fractured zoneat 14.6-14.7 @ ~600

21.9-22.1:307. granitic 4 qtz clottingover section

25.3-25.6:Muscovite rich graniticdyke @ 50O

26.8-27.1:Fg massive intermediate Cut by 5 '/, chlorite Adyke, sharp contacts @ 55 epidote veins

27.1-27.3:'Fg well foliated int. dyke @ 50O

36.2-36.4:Fg well foliated magnetiticmafic dyke @ 65O

@ 39m: gradationallyover 20cm QFP becomesless altered to unaltered.457. cordierite17. biotite

39.5-40.4:Massive fg weak feld. phyric int/mafic dyke Sharp contacts @ 60O

42.0-42.2:Well foliated fg int dyke @ 500

HOLE NO: HL-31 LOGGED BY: R.C.SIM PAGE: 3

lft

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



A3.O GABBRO Green mg Typically a mg moderateto with to to well foliated "splotchy"140.5 white eg gabbro with foliation

spots defined by chloritic clots @Locally grading to eg to vcgmaterialFg chill over top 1m withsharp upper contact ®

Fg weak foliated int. dykes at: 45.2-45.7 @

46.9-47.2 @

48.8-49.0:Blocky chloritic zone cut by 3cm granite Possible fault @

Fg moderately foliated int. dykes at:

' 52.8-53.1 @ 53.4-43.7 @

Light fg 58.3-60.3:green Massive to weak foliated

highly epidote veined (107.) intermediate dyke. Sharp contacts @

Well foliated fg-mg intermediate dykes at:65.2-66.7 @67.3-67.5 @70.1-70.5 @72.0-72.5 ©

55-600

60"

60" 550

50U

50" 500

55"

30" 350 400 400

1-27. leucoxene in vcgsectionsMagnetite clots stillexist with leucoxene rims

Very rare trace diss pyrite

Possible fault?

@ 57.0m: GB becomes light green epidote bleached

60.9-61.1:Gradational epidote bleachedpatch in GB

By 65m: no leucoxene in GB (non-magnetic)

1-27. disseminated pyrite


DRILL HOLE LOG

FROM TO

ROCK TYPE



67.7: 2cm qtz vein © 40

69.2-69.4:3 to 4cm hematite/carbonate/qtz vein ® 150

79.2-80.1:Well foliated, mg graniticdyke, sharp contacts @ 55 0Top contact slightlychloritic t* b locky

80.4-80.6:White qtz vein @ - 45OBottom contact alonggrungy hem/carb vein (lcm) @ 45

86.9: 3cm granitic vein @ 60O

86.95-87.0: Int. dyke @ ~600

89.0-89.1:Fg massive int. dyke @ 45O

89.1-90.1:Granitic dyke, sharp contacts @ 45

90.8-91.2 i 91.4-91.8: Massive mg granodiorite dykes

92.1: 4cm qtz vein © 700

Light grey fg massive intdykes at:

93.1-93.3 @ 700 95.6-95.9 @ 600

Possible shear plane

Tr phlogopite begins@ 90m increasing to avg.37. @ 102m.


DRILL HOLE LOG

FROM TO

ROCK TYPE



Fg int. dykes (as above) 100.1-100.4 @ 100.6-100.8 @

103.1-103.2: Qtz vein® Other qtz veins @

109.1-109.2 4109.4 - 5cra

gabbro grades to eg splotchy, well foliated by phlogopite @

112.0-113.2:Aphyric weak foliated int.dyke, sharp contacts @

113.2-113.8:Blocky ground with 10cm chlor/carb grunge at 113.7-113.8 @

114.2-115.0 4 115.4-116.0: Well foliated highly feld. phyric (lO'/i) int. dykes. Sharp contacts @

60550

-40

60

45

45

60

Fg. aphyric int dykes @: 124.8 - 5cm clot 125.0-126.1 - very irregular

contacts @ 0-20O 127.6-128.0 @ 600 128.2-128.4 @ v550

Weak foliated granitic dykes @ 130.0-130.2 @ 550 131.5-132.7 @ 550

Int. dykes @ 131.1-131.2 4131.4-131.5 @ 55 0

Avg. 5-77. phlogopite clots

Fault

Tr-1% magnetite


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



132.8-134.0:Fg weak foliated gabbroicdyke @ 60O

135.7: 2cm qtz/hem/carb vein/vug © 55

137.1-137.8:Composite dyke, fg inter mediate cut by granite at 137.2-137.6

139.0-140.5:Feld phyric int dyke.Well foliated, defined by157. chloritic mafic streaks/clots, sharp contacts @ 55

17. phlogopite

140.5 TRANSITION Light to ZONE green 142.4 GABBRO with

brown streaks

eg Well foliated defined byphlogopite @ 55 Contact defined by gradational decrease in feldspar content.

141.2-141.4:Massive aphyric int.dyke @ 45

141.6-141.7:Blocky grungy chloriticfault zone @ v 60c

77. phlogopite None

TZ very biotite rich over bottom 20cm

FaultC

o

c

c

c

142.4 META- Steelto PERIDOTITE blue/grey161.95

mg Massive ultramafic unit to with gradational upper eg contact marked by appearance

of magnetite.

143.4-145.6:Pervasive biotite/chlorite zone in Px. Gradational contacts over 1.3cm

None

+ 507. biotite Highly magnetic


DRILL HOLE LOG

O

oo

FROM TO

ROCK TYPE COLOUR



148.1-148.7:Similar bio/chlorite zonegradational over *5cm

154.0-154.2: Chloritic mafic dyke. Non-magnetic. Sharp contacts @

307. biotite

151.5-154.0:Gradational, avg. 107. biotiteover section

60

156. 6-156.9!Chloritic blocky fault zone @ 55O

158.0-158.2:Chloritic blocky fault zone

160.9-3cm and 161. 4- 5cm: Chloritic/carbonate rich grunge zone @

161.7-161.95:Very blocky chloriticfault zone @

@ 60O

Cut by 37. carbonate veins

107. biotite over section

Fault

Fault

Fault

Fault

161.95 ALTEREDto QFP235.6

Mottledgrey/whitewithblackspecks

fgto

166.7mmg

Massive equigranular overtop 5m grading to weakfoliated mg unit definedby micas @

Granitic/granodioriticdykes @

164.9-165.0 @165.05-165.15 @165.2 - 3cm @165.9-166.0 @

+407. cordieriteAvg. 7'4 biotitet-4% muscovite

60-650

60060055 0800

Rare trace dlss. pyrite Generally QFP Isunaltered below gabbroicsill. This is not.

37. euhedral garnets ( 4. l cm) from 166.0-166.15m


DRILL HOLE LOG

FROM TO


166.7-167.1: Composite fg massive feld. phyric int. dyke @


500

SULPHIDES REMARKS

cut by granitic dyke at 166.7-167.0

167.1-168.05:Chloritic altered mafic dyke, mg-cg, very well foliated @ 55-600 Sharp chilled contacts @ 50O

Mg massive granitic dykes at169.5-170.0 @ 700171.0-171.1 @ 400175.2: 5cm @ 70O176.1-176.3 @ *.600

107. biotite 47. anthophyllite

177.6-178.2:Fg massive aphyric maficdyke, sharp contacts © 60O

185.8-186.05:Weak foliated aphyric dykeSimilar to above @ 600

@ approx. 187m: QFP gradationally becomes massive

188.6-188.7: Granitic dyke @ 800

199.8-201.3:Massive fg gabbro dyke.Sharp contacts @

Muscovite has decreased gradationally to trace

60"

201.7-202.85: Granitic dyke @ 70Tr garnet in alt QFP at 206.0m, rare visible feldspars noted below 207m where alt. decreases locally to 157. cord, 37. biotite.

Patchy tr-17. magnetite in less altered zones

C


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



212.9-213.7:Fg wk foliated gabbroic dyke @ 60C

Massive mg-cg granitic dykesat: 213.9-214.0 @ 750

217.2-217.6 @ 500219.2-219.8 @ ^600

221.8-222.2:GR over 507. of section

223.8-224.1:Biotite rich synvolcanicdyke @ *350

17, magnetite

357. biotite 15* cord.

Black fg 224.8-228.6:with Weak foliated weak alteredwhite feld phyric intermediatespots dyke.

Sharp contacts @ 50O Lower contact has minor chloritic shear.

229.5-230.2:Fg weak foliated gabbroicdyke, similar to 212.9 @ 650

232.0-232.1:Blocky zone cut by numerouschloritic veinletsPossible fault @ 700

57. biotite 107. cordierite (T)

1-27. magnetite

Fault ?

27. anhedral garnets inQFP begins @ 233.5 - 37. qtzclots/veins


——

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



235.6to418.6

SILICEOUSGARNET IFEROUS ALTERED SEDIMENTS

Grey with pink spots

fg Sharp upper contact

Well foliated

70

70

Garnets in weak bands defining foliation @ 65-70

247.2-247.7:Massive granitic dyke @

White garnetiferous siliceous granodiorite/granitic dykes @

249.4-250.2250.5-251.8 - very irregular252.5-253.2 @

i*

d

235.6-235.9:do'/, biotite, 157. anthophyllite enveloping 2 57. qtz clots and veins

235.9-244.3:Mainly pervasive biotite ( 257.)anthophyllite (107.) t,cordierite (+607.)with gradtional garnetiferouspatches @ 238.5-239.5

Below 244.3: Typical garnet- l iferous sediments: 407. cordierite5* biotite

2-37. anthophyllite 7-107. garnets (rare silica

rims)

245.6-245.8:507. biotite over section related to 307. qtz clots and veins

T/, garnet 47. garnet 57. garnet

253.2-254.4: Garnetiferous sediments

17. po, 17. py in streaks and clots often associated with garnets

e

Q

C

HOLE NO: WL-31 LOGGED BY: R.C.SIM PACE: 11

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



Dark grey with light green wisps 8. pink spots

fg Below 254.4: SEDS:Patchy massive gradingto well foliated definedby anthophyllite @ 65-700

270.7-271.0:Blocky, chloritic shear zoneNote: 5mm grungy shear@ 270.7 @ 250

271.5-271.7: Siliceousgarnetiferous veining Aclotting over 757. section @ -/55O

275.7-276.1: Fg massive chloritic mafic dyke @ 65O

277.4-277.6:Fg massive feld. phyric int. dyke © 700

278.7-279.2:Fg intermediate dyke. Massive over top 0.2m grading to well foliated defined by chloritic mafic clots ( *e 4mm) stretched @ 700 Sharp contacts @ 70C

279.9-280.8:Fg well foliatedgabbroic dykeBiotite rich contacts @ —700

285.0-285.3:Several weakly slickensided often carbonate rich frac tures over section @ Probably not fault related.

Below 254.4: Intense to altered sediments similar to 235.9 15-207. biotite 57. anthophyllite patchy localized garnet D-5% over sections < 1m (no silica rims) +607. cordierite

Localized clots, streaks and splashes 27. py, 17. po often associated with garnets Localized zones of magnetite 0-27.

Intense to pervasive altered sediments 254.4-298.2

Fault

27. fine disseminated po

37. garnet { < lcm) {through contamination?)

280.8- 282.0: Example of gradational zone often pervasive alteration, 507. biotite, 157. anthophyllite, over section

283.8-284.5:37. fg staurolite over section

HOLE NO: WL-31 LOGGED BY: R.C.SIM PACK: 12

DRILL HOLE LOO

FROM TO

ROCK TYPE COLOUR



296.6-296,8:Blocky zone with severalchloritic slickensidedfractures @ 700

Blue/grey fg Generally massive with verywith pink weak foliation locallyspots defined by siliceous rims @ 70-75

302.7-303.3:Fg massive feld phyricint. dyke @ 75O

303.5-303.8:Irregular granitic dyke

304.1-305.3:Massive fg weakly feld.phyric int dyke cut by 77.qtz/carbonate velnletsSharp contacts @ 700

Dark fg 308.8-313.6:green/ Massive feld phyric intgrey with dyke, non-magnetic.white spots Sharp contacts @ 75

Siliceous rims about garnet become Very common @ 319m

324.45-324.6:Siliceous granitic dyke withirregular contacts

@ approx 291m! Garnetsbecome common in bio/anthrich sediments (avg. 67. garnets)

Possible fault ?

@ 298.2: Sediments gradeinto more typical siliceousgarnetiferous sediments77. biotite+407. cordieriteAvg, 57. garnet (*/- silica

rims) 1-27. anthophyllite

27. py, tr-1% po dissemin ated or in clots often associated with garnets. 1-27. fg magnetite throughout

Seems to be less altered more siliceous sediments than above.

57. muscovite books

HOLE NO: WL-31 LOGGED BY: R.C.SIM PAGE: l 3

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



325.4-325.6:Granitic dyke @ 500

326.3-326.7:Massive fg tnt/maflc dyke @ 75O

326.7-327.7:Granitic dykes 4 clotsover 607. section

350.0-350.2:Grungy fault zone @ 45-55

Dark grey fg 350.7-352.9:to orange Intermediate dyke, moderate

to well foliated with sharp contacts © 75O Cut by 47. qtz/carb/hematite veins f l cm @ 15-300 Similar fg grey Int dyke at 354.1-359.2 @ 700

366.9-367.0: Granitic clot/dyke

367.0-367.3:Blocky, grungy chlorite/carbonate rich fault zone @ *45C

367.4-367.6:Mg weak foliated gabbroicdyke .

372.9-373.5:Fg massive intermediate/gabbroic dyke @ 70O

fg @375m: Sediments commonly show chloritic amphibole/biotite mafic clots avg 4mm, up to 2cm These clots are commonly stretched parallel to fol'n l* contain sulphides

47. muscovite

37, muscovite

Pink stained

Gradatlonal staining to brick orange from 351.7- 352.5

Fault

Fault

Feldspars granitic stained

+ 507. cordierite127. biotite37. anthophylliteAvg. 107. anhedral garnet(* 1.5cm commonly withsilica rims)

27. po, 17. py in clots associated with garnet or disseminated in mafic clots


DRILL BOLE LOG

FROM TO

ROCK TYPE COLOUR



388.8-388.9:Garnetiferous granodioritedyke ® 600Several irregular clotsover 407. section, to 389.0

389.3-389.4:Numerous chlorite fractures @ 70

390.5-390.6: Granitic clot

Possible shear zone ?390.2-390.3; 57. po, 27. py in wispy streaks 4 clots parallel to foliation

Salt 8, pepper with pink spots with white halos

Grey

AGO.4-400.6:Numerous chloritic fractures(as above) @ 700Section cut by 5 07, q tz/granite veins

401.5-401.9:Fg well foliated gabbroicdyke @ 75O

fg @ 402.5: Sediment gradationally become sugary. Massive fg qtz/cord/biotite support silica rimmed garnets.

Silica rims definefoliation @ 750

405.4-406.6:Fg-mg weak foliated feld.phyric (107.) intermediatedyke. Contacts © 75C

@ approx 390m: gradational decrease in garnet content to avg. 67.

401.0-401.3: 107. garnet over section partially retrograding to chlorite i qtz

507. cordierite 157. biotite Avg 57. garnet ( 5mm)

Tr-27, anthophyllite localized wispy sillimanite up to 37, over 20cm sections

Very localized magnetite up to 27. over 20cm sections

Possibly shear zone ?

37. py clots over section

Tr diss pyritePatchy localized magnetite(up to 37, over 10cm sections)


DRILL HOLE LOG

FROM ROCK GRAIN ANGLE TO TO TYPE COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS

\Dark green

Massive fg feld. phyric (37,) intermediate dykes at: 410.3-410.4 @ 412.1-413.4 @ 416.2-416.4 ® 416.7 - 3cm @

750 700 750 85 0

Tr diss magnetite

418.6to474.5

"INTER MEDIATE" SEDIMENTS (ALTERED)

Dark grey with light blue/grey clots

Grey

to 430m:Well foliated defined by cordierite clots and anthophyllite @

Fg massive dykes at430.0-430.2, 430.3-4cm, 430.6-430.7, all @

75U

750

Generally massive, butlocally banded on *mm scale @ 75-80Rare localized minorgradational zones o f morealtered (as above) materialexist ( < 1m)

431.3-432.0:Blocky zone with numerouschloritic fracturesMinor slickensldes @ 75O

Intense alteration toapprox. 430m:+507. cordierite in cloudyclots *i 5mm20-257. biotite37. anthophyllite

Gradational patches garnet iferous seds @ 424.2-425.2 - 57. gnt 427.0-427.5 - Tl. gnt with well developed silica rims

428.0-432.0:Biotite increases to avg 357.over section, locally banded

@ approx 430m:Sediments gradationallydecrease in alteration to:207. cordierite57. biotite57. anthophyllite

Rare tr diss pyrite Intensely altered sediments !

Rare localized disseminatedpyriteAvg 37. subhedral magnetitebelow 434.6 (up to 3mm)

Moderately altered sediments

Possible fault


DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR



433.5-433.7:Gradational biotite rich zone enveloping 207. granitic stained fragments

807. biotite over section gradational over 5cm

J

J

J

i)

Approx. 436.0-437.0: Weak altered gradational banded zone on -t-mm scale Siliceous bands A chloritic anth/biotite bands

Gradational intense biotite zones (same as 433.5) @443.0-443.64 4A. 1-445. O

Grey fg @ approx 445.0:Seds have graded into consistent massive weak altered sediments cut by 17. orange stained qtz veinlets (^. 1mm) at various angles

451.4-451.6 4 453.2 - 3cm:Cg granitic dykes @ 55O

454.7-455.1:Felsic dyke or siliceous zonein sediments. Contactsgradational over 3-4mm @ 800Gradational pervasivebiotite bands supporting157. orange frags (similarto 433.5 @ 454.75-454.8d. 455.0-455.05

@ approx 459m: seds become locally wk foliated defined by siliceous streaks (avg 1mm x 1.5cm) @ 80O

47. biotite over section 157. cordierite (?)

SO'/l bio, 207. frags.507. bio, 407. cord, 1 07. frags.

+407, cordieritey/, b iotiteMinor localized patches(A3Ocm) increase to mgA composed of 507. cord,157. bio (57. unit)

Dyke composed ofVI. biotite37. anthophyllite107. cord (?)i crystallized qtz

Tr diss pyrite Banded seds.

Localized tr py37. fg diss magnetite

Wk/moderate altered seds (Typical "non-descript" intermediate sediments)

27. magnetite, euhedral up to 2mm

- HOLE NO: WL-31 LOGGED BY: R.C.SIM PAGE: 17

DRILL HOLE LOG

FROM TO


462.0-462.1: Fg massive feld phyric (27.) intermediate dyke @


850

SULPHIDES REMARKS

466.9-467.2:Pervasive biotite zone(altered dyke?) locallycrenulated with sharpcontacts with 7mm bandedchill (?) @ 800

468.6-468.7.-Fg massive int/mafic dyke @ 7 5

470.95-471.0:Fg massive intermediate dykeSharp chilled contacts @ 800with 4mm banded py/mt veincut in at 470.96 @ 70O

O

O

9

907. biotite57. chloritic wispy clot 57. siliceous fragments (grains?) * 2mm

307. pyrite in dendritic arm" coming from vein onto host dyke, 107. magnetite over 1.5cm

Seds begin to show several intense biotitic bands C5cm

Tuffaceous component in sediments


(CLR)

Black 4 fg Gradational upper contactgrey to biotite banded unit on(banded) *cm scale @ 75-80"

Avg 30X cordierite127. biotite with bio inbands going from 57. to +207.

Patchy 27. magnetite to 475.0 2'/. diss pyrite from 475,5- 476.0

476.0 MASSIVE Light vfg Massive homogeneous sulphides to SULPHIDES brown/ enveloping 107. rounded qtz476.1 orange with frags (avg 2mm) 81 approx 107.

translucent fg biotite altered fragments white spots Upper contact gradational

over 5mm @ Bottom knife sharp ©

65" 800

Tt. pyrite rounded 4. I ran Est: 21 magnetite (anhedral clots) •*-tt pyrrhotite IX chalcopyrite - associated

with fragments 657, sphalerite - fg orange/ yellow to orange brown

Q.3% Cu 32Z Zn O.lm CL

HOLE NO: WL-31 LOGGED BYs R.C.SIM PAGE: 18

DRILL HOLE LOG

FROM TO

ROCK TYPE COLOUR




(CLR)

Mottled fg Generally well bandedto banded to throughout on mm scale @ 80grey, aphan-black 4. Iticwhite

478.5-479.0:Looks like typical clottedrhyolite

479.3-480.0:Well foliated feld phyric(77.) int dykeSharp contacts @ 80O

Cut by granitic dyke at 479.7-479.8

486.3-486.7:Fg massive feld phyric (37.)int dyke, sharp contacts @ 70

Preferential mafic altera tion to biotite, cord. Avg. 127. biotite

307. cordierite

482.2: 107. garnet over 2cm in biotitic bands

Generally 2-37. po, 1-27, pyrite in disseminated bands. Patchy up to 17, magnetite sphal to 476.15 with tr diss sphal to 476.85

486.7-486.8:57. po, 37, py in streaky/disseminated bands

487.0: 2mm pyrite/sphalerite band @ 75O to CA

487,7: Irregular 2 to 4cra sphalerite vein with sharp contacts (27. cp). 107. qtz clots in sulphides. Several minor clots 4. l cm for 3cm above A below vein.

Possibly stringer

Qtz hosted sphalearite rich veins @: 487.9 - 207, sphal over 2cm488.0 - 207, sphal over 3cm488.1 - 107. sphal over 2cm 488.3 - 57. sphal over 3cm Tr sphal © 488.8 in py/qtz vein _______________\__________


DRILL HOLE LOG

FROM TO

ROCK TYPE



Dark fg green/grey to with mg white spots

489.4-489.6:Feld phyric Int dyke

499.2-499.8:Fg-mg well foliated feldphyric dyke.Sharp contacts ©

501.2-501.6:357. irregular graniticclotting over section

503.2-506.4:Massive to moderatelyfoliated feld phyric (157.)Int dyke.Sharp contacts @

506.4-506.6:Massive mg granitic dyke @

507.1-507.4:Possible QFP flow or GR dykeContacts gradational over3-5mm @

End of Hole.

80U

80U

85"

85"

Tr garnet @ 499.15

27. fg biotite

Below approx 492m: CLR Average 57. diss/bands po, 1'i py, locally po increased to 87. over 2-3cm sections

496.0-496.2: Example of matrix altered typical CLR

@ approx 501.6: sulphide content in CLR decreases to 27. py, 17. po, t r mt.

17. diss pyrite

Tr diss pyrite

E.O.H.

HOLE NO: WL-31 LOGGED BY: R.C.SIM PACE: 20

ASSAY SHEET

SampleNumber

WS07890790079107920793079407950796079707980799080009080909

(ra)From

474.5476.0476.1476.85478.2479.3480.0481.5483.0484.5486.3486.7487.7488.3

(m)To

476.0476.1476.85478.2479.3480.0481.5483.0484.5486.3486.7487.7488.3489.0

EstimateCu Zn Py

10.3 32.0 7

0.5 12111111

-0.1 2

tr 2.0 1tr 3

Po

-5221-2212-111

(m)Length

0.50.10.751.351.10.71.51.51.51.80.41.00.60.7

% V.Cu Zn

0.004 0.020.03 16.370.10 0.460.03 0.040.004 0.020.004 0.020.004 0.010.02 0.010.01 0.010.03 0.010.01 0.010.06 0.060.05 1.080.06 0.08

gm/TAg

0.412.31.50.70.20.20.40.60.50.60.731.02.2l.B

ppbAu

610755667766866

'1,Na

3.1.3.2.3.3.3.3.2.3.3.3.3.3.

20

4546828520672729840133280822

Comments

Alt. CLRUSAlt. CLRAlt. CLRAlt. CLRInt. dykeAlt. CLRAlt. CLRAlt. CLRAlt. CLRInt. dykeAlt. CLRSphal vein in alt CLRAit. CLR

GEOCHEM SHEET

SampleNumber

WSWS0776WS0777WS0778WS0779WS0780WS0781WS0782WS0783WS0784WS0785WS0786WS0787WS0788

(m)From

15171204231240267300330360390420450495

(ra)To

18174207234243270303333363393423453498

EstimateCu Zn Py

----

112211

--

-1

Po

----111

trtr2--5

(m)Length

3.03.03.03.03.03.03.03.03.03.03.03.03.0

ppm ppmCu Zn

6 563 53

20 4220 4712 967 132

53 18710 12628 1465 62

182 158721 260

167 126

ppmAg

------------

ppb '1,Au

7555455565545

Na

0.4.4.3.2.2.3.4.2.2.1.4.2.

20

80222459244037003553393556

Comments

Alt. QFPAlt. QFPAlt. QFPAlt. QFPPerv. bio/cord/anth sedsPerv.alt. SGSSGSSGSSGSSGSPerv.alt "int" sedsWk alt "int" sedsAlt. CLR

HOLE NO: WL-31 LOGGED BY: R .C.SIM PAGE: 2 1

diamond drilling report pick lake project schreiber …

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