b kokanee explorations ltd, report on four …

m: 49'23'N

FORT STEEL MINING DIVISION

CRANBROOK AREA

...

- FILE NO:

b

KOKANEE EXPLORATIONS LTD,

REPORT ON FOUR DIAMOND DRILL HOLES I

(KV90-36, 37, 38 and 39) , RE. LOG NO: P/- 50

ACTION: I VINE PROPERTY

, VINE 1 ,

N . T . S . 82G/5W

LONG: 115'49'W

,

OWNER

KOKANEE EXPLORATIONS LTD. I

Suite 104, 135 - 10th Avenue South Cranbrook, B.C.

V1C 2N1

Work Performed From April 12, 1989 to May 29, 1990 9

Report by: L. STEPHENSON . Submitted: November, ,1990

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,

TABLE OF CONTENTS

PAGE

1.00 Int r oduc t i on . . . . . . . . . . . . . . . . . . . . . 1

2.00 Location and Access . . . . . . . . . . . . . . . . . . 1 3.00 Regional Geology . . . . . . . . . . . . . . . . . . . 1 4.00 Property Geology . . . . . . . . . . . . . . . . . . 1 5.00 Diamond Dri 1 1 ing . . . . . . . . . . . . . . . . . . 2

6.00 Conclusion . . . . . . . . . . . . . . . . . . . . . . 2

Exhibit "A" . Statement of Expenditures . . . . . . . . . . . 3

Affidavit . . . . . . . . . . . . . . . . . . . . . . . . . . 4

Author's Qualifications . . . . . . . . . . . . . . . . . . . . 5 -e Location. Map . Drillholes KV90.36.37. 38 '+ 39 . . . . . . . . . 6

Section 10. 050E . KV90.36. t37 . . . . . . . . . . . . . . . . . 7

Section 9. 500E . KV90-38 . . . . . . . . . . . . . . . . . . ' . 8

Section 9. 775E . KV90-39 . . . . . . . . . . . . . . . . . . . . . 9

APPENDIX I . Drill Logs KV90.36.37. 38 t 39 . . . . . . . .Attached .

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KOKANEE EXPLORATIONS LTD.

REPORT ON FOUR DIAMOND*DRILL HOLES

VINE.1 CLAIM

FORT STEELE MINING DIVISION'

L. Stephenson November, 1990

1.00 Introduction

In our continuing exploration drilling on the Vine claim group, where Kokanee owns a 90% interest (Cominco Ltd. lo%), four diamond drill holes were completed as part of the program. These intersected the vein and are detailed below.

2.00 Location and Access

Vine claims (all of them) are located at the end of Hidden Valley (south) Road, north of Moyie Lake. Access by government maintained highway to the centre of the claim group is present.

0

3.00 Reqional Geoloay

The claims lie within the central portion of the Purcell Anticlinorium, which consists of sedimentary argillites, quartzites and related intruded gabbro sills and dykes of the Aldridge formation. These formations host both the Sullivan deposit and the St. Eugene deposit, approximately 30 kilometres north and 14 kilometres south, respectively.

The structural features of the area appear to have had a significant influence on the location and control of the ore zones in the Aldridge formation.

The St. Eugene mine reported over 1.0 million tons were mined and indicated recovered grades of 10.86% lead, 2.73% zinc, 5.53 ounces of silver and 0.0049 ounces per ton of gold.

4.00 Propertly Geology \

The property is underlain by the regional Middle Aldridge rock. A vein was discovered in 1976 by Cominco and the fault structure, associated with the mineralization, has been traced for 4 kilometres.

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Stratigraphic drilling on the property intersected a large section of massive quartzite. This rock type was also found at the St. Eugene where it hosted the largest tonnage zone.

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There appears to be strong evidence that the structure, hosting the St. Eugene deposit, and the Vine zone are related, offset by the Moyie Fault located just to the south of the Vine property.

The mineralized structure has been traced for over 1,000 \

metres with a down dip extension of at l e a s t 700 metres.

I

5.00 Diamond Drillinq

Four drill holes were completed as part of the ongoing exploration program on the property (Appendix I Drill Logs). These holes, KV90-36, 37, 38 and 39, were drilled in the central'portion of the currently known Vine Vein structure.

All holes were collared in the quartzite and argillites of the Middle Aldridge and terminated in the argillites and quartzites of the Lower Aldridge. As well, all holes intersected the mineralized vein structure. In holes KV90-36, 37, 38 and 39, the Sullivan stratigraphic horizon was intersected with holes KV90- 36 and 37 also intersecting the Sullivan Footwall Quartzite stratigraphic horizon.

6 .OO Conclusion

\ ' $he cores of the four diamond drill holes represent excellent examples of drilling in and about the Sullivan stratigraphic horizon and good examples of mineralization of the Vine Vein.

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The resu ants cont

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Report

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- 3 -

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EXHIBIT "A"

STATEMENT OF EXPENDITURES

DIAMOND DRILL PROGRAM

ON VINE 1 CLAIM Fort Steele M.D.

INDIRECT

Salaries : D . L . Pighin - Geologist - Supervision +

core logging

writing 2 days @ $400/day 800.00

25 days @ $250/day $ 6,250.00 L. Stephenson - Geologist/P.Eng. - Report a

As.says Acme Analytical Laboratories Ltd. 852 E. Hastings St., Vancouver, B.C.

94 samples - 30 element I.C.P. $1153.21 - Fire assays 980.00

2,133.21 . Indirect Total = $ 9,183.21 .

I

DIRECT

Connor's Drilling Ltd. 2007 West Trans Canada Highway Kamloops, B.C.

Four Diamond Drill Holes $168,276.19

TOTAL DIR NDIRECT COSTS

.- 'Stephenson- ;-<. qfl ,M. B .A. , P. Eng. jj,cy,, - -\ 'r.

$177,459.40

- 4 -

IN THE MATTER OF THE

B.C. MINERAL ACT

AND

IN THE MATTER OF DIAMOND DRILLING PROGRAM

CARRIED OUT ON THE VINE 1

\ I

CRANBROOK AREA

in the Fort Steele Mining Division of the Province of British Columbia

More Particularly N.T.S. 82G/5W

A F F I D A V I T

I, L. Stephenson, of the City of Cranbrook, in the Province of British Columbia, make Oath and say:

1. That I am employed as a geologist by Kokanee Explorations Ltd. and, as such, have a personal knowledge of the facts to which I hereinafter depose:

2. That annexed hereto and marked as Exhibit "A" to this, my Affidavit is a,true copy of expenditures incurred on a Diamond Drill program, on the Vine 1 Mineral Claim.

3 . That the of April of miner

said expend , 1990 and the 29th day o 990 for the pu .a1 exploration.

- 7 - - ' ..'?

\ - .

.h day

.rpose

- 5 - '

AUTHOR'S QUALIFICATIONS

I , Laurence Stephenson, of Cranbrook, B.C. , in the Province of British Columbia, do hereby certify that:

1. I graduated from Carleton University in 1975 with a Bachelor of Science* degree in Gedlogy then, in 1985, graduated from York University with a Masters,of Business Administration;

2. I am registered 'as a Professional Engineer for the Province of Ontario (1981) and currently a member in good standing;

3 . ' I have had over 2 3 y e a r s expe i n the f i e l d of mining exploration. . .

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1 i 0 2000 3000

KOKANEE EXPLORATIO! VINE PROPERTY . -

D r i l l h o l e s KV90-36,37,38,39

Location Map

KV90-3(

KV90-37 -

-

900 m

700 m

500m

KOKANEE EXPLORATIONS LTD VINE VEIN

SECTION 10,050 E

- 8 -

I lOOm

?

900m

700 m

KOKANEE EXPLORATIONS LTC VINE VEIN

SECTION 9,500 E

Scale: I : 2500 I Date ' NOV. 1990

K V W - 3 9

800 m

600m

I KOKANEE EXPLORATIONS LTC I VINE VEIN

SECTION 9,775 E

IDclte: NOV. 1990

APPENDIX I

D R I L L LOGS

VINE DRILL HOLES

HOLE # ELEVATION LENGTH

KV90-36 956m 309.5m

KV90-37 955m 457.3m

KV90-38 1105m ~ 572.6m

KV90-39 1024m 570.4m

,

-68' '

-75'

- 60'

-75O

KOKANEE EXPLORATIONS LTD. KILL HOLW RECORD Page No. 1

Name of Property: Vine Corr. Dip: see attached Remarks :

Hole No: KV-90-36 Length: 327.4m

Location: Sect.Ot5OE

Elevation: 955m (approx) Azimuth: 030° Collar Dip: -75deg.

Core Size: HQ Tests at: see attached Logged by: ASH/DLP Date: April/90

M E T E R A G E D E S C R I P T I O N S a m p l e

0.0 - 12.8 Overburden

12.8 - 33.8 Quartzite and Siltstone: medium and thick bedded sediments. Some intervals, less than 1. Om, of thinner, more argi 1 laceous beds. Typical Middle Aldridge type lithologies. Bedding 66 deg. to core axis.

Start date: 12/4/90 Finish date: 19/4/90

ppb Dum % % DDm /

33.8 - 64.2 Quartzite and Siltstone: similar to above.

64.2 - 70.1 Fault, brecciated sediments in gouge and calcite matrix, "Haaen Fa ult." Some intense chloritization near base.

70.1 - 77.7 Sullivan Horizon: predominantly thinly laminated, silty argillite. Abundant pyrite in laminae in part. Well fractured rock with calcite healed fractures up to 5.0cm.

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K O K A N E E EXPLORATIONS LTD. DRILL HOLE RECORD

Prope r ty : Vine Hole No.: KV-90-36

M E T E R A G E D E S C R I P T I O N From To

7 7 . 7 - 1 6 0 . 1 S i l t s t o n e and A r g i l l i t e : t h i n l y laminated tc medium bedded, b i o t i t i z e d sed iments , Lowei A l d r i d g e f o r m a t i o n . Rock is well f r a c t u r e d and badly broken i r p a r t .

B r e c c i a t e d sed imen t s i n gouge and c a l c i t t f r o m 8 5 . 1 - 85.7m. S l i c k e n s i d e s a l o n g f r a c t u r e p l anes i n p a r t More than usua l amount of p y r i t e i n s c a t t e r e d , b e d d i n g p a r a l l e l banding and lamina t ions tc 86.9~1.

B r e c c i a and gouge i n broken s e c t i o n a t 89.6m, a p p r o x i m a t e l y 2 0 . O c m i n d i c a t e d . Some we1 1 f r a c t u r e d rock i n d i c a t e s movemenl a l o n g bedding i n p a r t . C a l c i t e hea led f r a c t u r i n g up t o 4 . 0 c m w i t 1 some sediment f ragment i n c l u s i o n s , sub - p a r a l l e l t o c o r e from 94 .2 - 96.6m. C a l c i t e v e i n i n g 1 1 9 . 8 - 120.3m w i t 1 p y r r h o t i t e / p y r i t e up t o 3.0cm, ve in ing 35 des t o c o r e a x i s .

Page: 2

Loca t ion : Sect.O+50E

S a m p l e - No. From To Au Ag Pb Zn cu

ppb D p m % % DDm

KOKANEE EXPLORATIONS LTD. DRILL HOLE RECORD

From To

Most pronounced fracturing from para1 le1 to 20 deg. to core. Fractures commonly calcite healed with pyrrhotite/pyrite mineralization in part. At 155.2m, a few cm of gouge along slickenside fracture plane 35 des. to core. Broken section for 40.0cm (fault plane). Bedding 66 deg. to core.

Page: 3

No. From To Au Ag Pb Zn cu pDb m m % % DDm

Property: Vine Hole No.: KV-90-36 Location: Sect .0+50E

160.1 - 182.6

182.6 - 189.0

189.0 - 222.0

222.0 - 226.5

Si 1 tstones and Argil 1 ites : similar lithologies to above with much less fracturing and far more competent rock. Bedding 65-70 deg. to core.

Siltstone and Argillite: as above with fracturing becoming more pronounced. Core from 182.6 - 183.2m is intensely fractured and broken. No indication of major breaks. Bedding 70 deg. to core.

Siltstone and Argillite: similar to above with much less fracturing. Fault zone 216.5 - 216.9m with slickenside fracture planes 30deg. to core. Bedding 65 - 70 deg. to core. Sediment: as above. Intensely disturbed zone, well fractured rock, brecciated and with gouge in part.

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KOKANEE EXPLORATIONS L T D , DRILL HOLE RECORD

From To

Fault breaks indicated at : 222.0 - 222.6m, remainder of zone appears to be disturbed zone adjacent to main break.

226.5 - 235.4 Sediment: as above. Moderately fractured for most part, minor amount of badly broken core.

Page: 4

No. From To Au A 9 Pb Zn cu PDb DDm % % PDm

235.4 - 282.2 'Footwall Quartzites': top of zonemarked by usual, very thin, laminations of biotite in mudstone (matches with holes KV-90-32 at 255.1m and KV-90-34 at 234.4m.) Quartzites and siltstones, medium and thick bedded sediments with intervals, usually less than 1. Om, of thinner, more argillaceous beds fracturing parallel to low angle to core causes broken segments. Beginning at 253. Om fracturing becomes more intense causing severely broken core in some intervals. Slickenside fault plane at 259.1m, 40 deg. to core has gouge and brecciated sediments immediately above. Core remains intensely fractured and badly broken to fault zone at 267.6 - 270.4m. Fracturing at low angle and parallel to core below the fault causes continuation of broken core. Fault contains breccia with gouge and well fractured rock throughout.

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Property: Vine Hole No.: KV-90-36

Page: 5

Location: Sect.O+50E


Fracturing intensifies again beginning at 274.4m and continues to top of vein structure at 282.2m. Occasional thin (a few cm) segments of breccia and gouge i.e 272.9m, 276.8q, 279.9m and 281.lm. Top of vein zone at 282.2m. (Base vein zone 318.6m) Hangingwall vein structure at 282.2111 cuts core at 52 des. 281.0 - 282.0 -Brecciated chloritic hangingwall waste sediments (siltstone), widely scattered quartz-cal ci te vein1 ets, minor disseminated sulphides, mainly pyrite.

282.0 - 284.0 Quartz Massive Sulphide Vein: 282.0 - 283.0m - 60 to 80% sulphides, mainly galena and pyrrhotite, lessor arsenopyrite, minor chalcopyrite and pyrite. Sphalerite rare. Core loss 2%. 283.0 - 284.0m - quartz - massive sulphides. 80% sulphides, mainly pyrrhotite with lessor arsenopyrite widely scattered blebs of chalcopyrite, very rare galena and sphalerite.

284.0 - 288.3 Siltstone: bedding is not evident. Medium grained, abundant fine reddish biotite, wispy patches of chlorite, patchy silicification and a1 bi ti zation .

S a m p l e - No. From To A u Ag Pb Zn cu --

ppb ppm % % DDm

84386 281.0 282.0

84387 282.0 283.0

84388 283.0 284.0

0.02 0.004 29 230 0

5790 398 22.2 14.5 2902

4840 44 2.63 0.13 4527

K O K A N E E EXPLORATIONS LTD- D R I L L HOLE RECORD Page: 6

Hole No.: KV-90-36 Prope r ty : Vine

M E T E R A G E D E S C R I P T I O N S a m p l e From To - - - - - - ~ From To Au Ag Pb Zn c u

Locat ion: Sect.O+50E

Some d i s s e m i n a t e d p y r r h o t i t e i n t h i n i r r e g u l a r f r a c t u r e s . 284.0 - 284.7 - b r e c c i a t e d c h l o r i t i c s i 1 ts t o n e . Brecc ia zones have s c a t t e r e d m i n e r a l i z e d c l a s t s i n c a l c i t e m a t r i x , c h l o r i t e is abundan t i n b r e c c i a , p y r i t e is s c a t t e r e d t h r o u g h o u t . 284.7 - 285.7 - a s above b u t less p y r i t e . Some s c a t t e r e d v e i n l e t s of g a l e n a .

Gabbro: f i n e g r a i n e d , h i g h l y f r a c t u r e d , r a r e c a l c i t e v e i n l e t s . Con tac t c u t s core a t 63 deg . Q u a r t z : massive s u l p h i d e v e i n a s f ol 1 ows : 289.6 - 290.6; t o p 50.0cm of i n t e r v a l c o n s i s t s of s m o k y q u a r t z , s t r o n g l y m i n e r a l i z e d by a r s e n o p y r i t e . Badly broken zone . Lower 50 . O c m c o n s i s t s main ly of mass ive p y r r h o t i t e , w i t h s c a t t e r e d q u a r t z e y e s . (80% Sulph ides ) a r s e n o p y r i t e r e l a t i v e l y abundan t , o c c u r s d i s s e m i n a t e d i n p y r r h o t i t e and i n q u a r t z e y e s . 290.6 - 291.6; mainly mass ive p y r r h o t i t e w i t h q u a r t z eyes . I n t e r v a l is 80% s u l p h i d e s . A r s e n o p y r i t e d i s s e m i n a t e d i n p y r r h o t i t e and i n q u a r t z eyes . Some wide ly s c a t t e r e d mass ive a r s e n o p y r i t e p a t c h e s . Widely s c a t t e r e d b l e b s of c h a l c o p y r i t e . Thin i r r e g u l a r v e i n l e t s of m a s s i v e b lack-green c h l o r i t e t h roughou t . S p h a l e r i t e and g a l e n a ve ry r a r e . 291.6 - 292.6: mainly mass ive p y r r h o t i t e

288.3 - 289.6

289.6 - 292.6

84389 284.0

84390 284.7

84391 288.6

84392 289.6

84393 290.6

84394 291.6

284.7

285.7

289.6

290.6

291.6

292.6

DDb p p m % % DDm

380

14

680

7630

1840

2430

3

10

1

5

5

12

0.23

1.44

0.03

0.45

0.58

1.12

0.01

0.01

0.02

0.03

0.01

0.01

158

67

135

1911

1556

3540



Page: 7

Location: Sect.O+SOE

M E T E R A G E D E S C R I P T I O N From To _I_- - ~ . . _

as above, but more disseminated chalcopyrite. Lower 50.0cm of interval less pyrrhotite but more arsenopyrite. Galena and sphalerite are rare.

292.6 - 318.6 Gabbro: mainly coarse grain, becomes fine grained near basal contact. Footwall contact cuts core at 45 deg. 299.0 - 302.0; brecciated gabbro, shearing with gouge cuts core at 43 deg. and at 33 deg. abundant slickensides. Breccia consists of rock flour matrix with gabbro, quartz and calcite clasts. Some quartz clasts are mineralized. 298.0 - 299.0: gabbro waste. 299.0 - 300.0; sheared and brecciated gabbro. 300.0 - 301.0; brecciated gabbro, rare mineralized clast. 301.0 - 302.0; brecciated gabbro, rare mineralized clast. 302.0 - 303.0: gabbro waste. 310.2 - 311.2: gabbro waste. 3 u : quartz-sulphide vein. 208 sulphides. mainly pyrrhotite, minor arsenopyrite and chalcopyrite. Base of vein structure.

318.6 - 327.4 Qaurtzites and Siltstones: well fractured, broken core. Very rubbly core from 321.31~ downward, approximately 45% core loss. END OF HOLE KV-90-36 AT 3 2 7 . 4 ~ .

~ a m ~ I e - ~ - - . A u Ag Pb Zn cu From To No. w b w m % % I) Rm

84395 298.0 299.0 260 1 84396 299.0 300.0 29 3 84397 300.0 301.0 61 0

84398 301.0 302.0 260 1

84399 302.0 303.0 52 0 84400 310.2 311.2 19 1

136 2 84401 311.2 312.2 84402 312.2 313.2 10 1

0.07 0.17 0.01

0 . 0 2

0.01 0.02 0.10 0.02

0.06 225 0.09 245 0.02 56

0.02 103

0.02 20 0.02 252 0.002 1080 0.04 254

KOKANEE EXPLS2R.AT.X ONS----.- LTD - DRILL HOLE RECORD Page No. 1


Hole No: KV-90-37 Length: 457.3m (1500')

Location: Sect.Ot50E Start date: 19/4/90 Finish date:

From To

0 - 12.8 Overburden 12.8 - 155.2 Middle Aldridge Formation, Quartzite and

Siltstone: medium and thick bedded sediments. Intervals, usually less than 1.0m, of thinner more argillaceous type sediment (distal and inter turbiditetype deposition). Occasional quartz veining from 30 to 60 deg. to core, normal to bedding, with minor pyrrhotitefpyrite in some veins. Quartz veins range from less than l.Ocm up to 25.0cm.

Elevation: 954m (approx.) Azimuth: 030' Collar Dip: -75 deg.

Core Size: HQ Tests at: see attached Logged by: ASH/GMR rate: ?pril/%

.- NQ . F r o m T o - - Au Ag Pb Zn cu pwb Dmn % % m m

.: I: ..

. . . . - . . .

From To --.--_~.----- - - --- -_ -

Bedding 70 deg. to core throughout.

155.2 - 156.7 Similar lithologies to above. Variously disrupted sediments. 12.0cm breccia and gouge at 155.01-~, moderate to intense fracturing common,

156.7 - 162.8 Major fault zone ("Hagen Fault"), brecciated sediments in gouge and calcite matrix.

162.8 - 166.5 Lower Aldridge Formation, Siltstone and Argillite: this interval moderate to intensely fractured and broken core due t o proximity to major fault above.

166.5 - 240.1 Siltstone and Argillite: predominantly thin and medium bedded sediments with occasional, more argillaceous thinly laminated to thin bedded sediments. Rock is salmon pink, purplish and grey i n colour, mottled in-part. Noticeable increase in iron content (pyrite) compared to Middle Aldridge type sediments. Fracturing is variously moderate to intense throughout €or most part, some lesser intervals of weak fracturing. Fractures vary from parallel t o 25 deg. to core.

KOKANEE EXPLORATIONS L T D . DRILL H O L E RECORD

No. From To Au Ag Pb Zn cu poh wwm % % DDm

Paae: 2

Property: Vine Hole No. : KV-90-37 Location: Sect.O+SOE

KOKANEE EXPLORATIONS LTD, DRILL HOLE RECORD

Property : Vine Hole N o . : KV-90-37 -.

M E T E R A G E D E&C-RA-.PTIoJ- From To -_----I_ _- No. Ft

240.1 - 364.4 Footwall Quartzites: medium and thick bedded quartzites and siltstones with intervals, usuallv less than 1 . 0 m of thinner more argi 1 laceous beds. This lithology is similar t o typical Middl e A1 dridge type deposition. Top of zone marked by 15.0cm (approx.) irlterval of even, parallel laminated, fine grained pyrite in a homogenous, medium/l ight grey si 1 tstone.

Fracturing varies from weak to intense throughout, with occasional segments of brecciated rock and gouge as follows: 261.0 - 262.0m, 292.8 - 293.4m. ?84.5rg, 313.7 - 314.9111, 319.8 - 320.3m, 323.2 - 323 5m, 330.2 - 330.3m, x 0 . 5 - 340.7m,

343.3 - 346.6m, 355.2m. poor recovery, 5.0cm only, in badly broken ground. 358. I - - - U . B * Ground from 340.5m down to _?_5!%8m_ is , for the most wart very badly broken with much core loss (estimated 50%). Ground condition improves to moderately broken below 35x8~ in quartzites an? siltstones of the "Footwall Quartzites."

-._ -

Paqe: 3

Cocatior!: Sect.O+SOE

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364.4 - 379.4 3.&!4,4--95.4m: waste sediments, albitized and chloritized sulphide, quartz and calcite vein zone, cuts core at 41 deg. Vein is general I y competent rock, detached descriptions. Sample intervals as follows: 365.4 - 366.4 : quartz-sulphide-minor calcite and chlorite vein. 50 to 80% sulphides. Mainly pyrrhotite, arsenopyrite and lessor chalcopyrite, galena and sphalerite are rare. Coarse1 y crystalline arsenopyrite (commonly euhedral 1 is disseminated throughout smoky quartz and pyrrhotite. Calcite is rare in this interval. Core loss 2%. 366.4 - 367.4: quartz-sulphides. 50 to 80% sulphide. Same as above but with a 10.0cm zone of good coarse aalena. Chalcopyrite is still relativelv abundant. Core loss 2%. 357.4 - 368.4: quartz-sulphides 50 to 80% as above with some Datches of verv coarse crystal 1 ine arsenopvrite. Core loss 1%.

I 84421 364.4

84422 365.4

84423 366.4

84424 367 4

. .

!

,. ,

. . , :

. . .

. .

365.4 39

. . . . .

366.4 1590

367.4 2120

368.4 ' 17?n

0.01 0.01 59 0

19 1.91 0.01 2013

7 n 713 n.nn4 7 5 0 8

1 .

3: .. . . . . . . . _ . .

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. , ".; , - ::,. : r. ' I KOK'ANEE EXPLORATIONS LTD. . , . _I . -, * . $1 . DRILL 'HOLE RECORD Paye: 5

: ' . . , ,< ... Property: Vine Hole No. : KV-90-37 Location: Scct.O+SOE >.'' .;.. . '.'. r . -

t . 1 . . .

- .

- -- M E T E R A G E L F - 2 C R T E-T-3-93. -.______.__ S a m o 1 ' e -- !%Am& ._ ... . .. - -. .- ~ . _. , . -. . .. . . , . . . . . .. .. - p:~-.-::-Fr.om. . -__...To_ . . .. - .. .. A u A a Pb Zn cu

% owb wwn! % ----Ee!L- 0 . 8 8 0.0s 920 2 3 8 0 1 0 I ----.. 3 6 9 . 4 - 3 6 9 . 4 : u i i a r t z - s ~ . r l n h i ? ~ s . S O % / 8 4 4 2 5 3 6 8 . 4 3 6 9 . 4

sulphides, mainly pyrrhotite with1 disseminated euhedra! arsenopyrite (very' I

I coarsely crystalline in part). Scattered chalcopvrite, some scattered patches of coarsely crystalline qalena. Sphalerite is rare. Core loss 1% 1 6 9 . 4 - 370.4. : a)tart,z - gulphides. 20 to 80% sulphidss. mainly Dyrrhotite and arsenopyrite. - Arsenopyrite re1 ativsl v abundant (coarse euhedral crystals). Chalcopyrite is not uncommon throughout. Galena occurs sparinqly. Sphalerite is rare. Interval includes scattered patches of. finely crystalline calcite which is generally very weakly mineral i zed, 3 7 0 . 4 - 3 7 1 . 4 : calcite, minor smoky quartz, sulphides lo%, main1 y arsenopyrite. Arsenopyrite occurs as scattered euhedral crystals throughout

. cut smoky, quartz intervals and in siliceous wisps o r ' bands in white calcite. Some fine galena. 3 7 1 . 4 - 372.4: .sul?hi.de and srnokv quartz. 60 to 80% sulphide, mainly wyrrhotite with abundant disseminated coarse1 y . crystal 1 ine arsenopyrite. Relatively abundant chalcopyrite, aalena and sphalerite are rare.

I 8 4 4 2 6 369.4 3 7 0 . 4 2110 4 0 . 2 7 0 . 0 1 836

1 . 2 2 0.01 214 2 7 5 0 1 0 8 4 4 2 7 3 7 0 . 4 3 7 1 . 4

8 4 4 2 8 3 7 1 . 4 3 7 2 . 4 2 5 5 0 R 0 . 8 3 0.16 2 7 0 1

I

KOKANEE EXPLORATIONS LTD. DRILL HOLE RECORD Page: 6

Property: Vine Hole No.: KV-90-37 Location: Sect .0+50E

372.4 - 373.4: sulphide and smokv quartz. 30 to 40% sulphides, mainly finely disseminated arsenopyrite. Interval is badly broken. Some core (waste sediment from hangingwall ) some core ground up. Core loss approximately 50%. 3Z3.4 - 314.4: calcite: fine crystalline, crackle brecciated. Hosts scattered wisps and patches of finely crystalline arsenopyrite. Other sulphides are very rare. 374.4 - 375.4: calcite: fine to coarsely crystalline. Scattered wisps and band of smoky quartz and finely crystalline arsenopyrite. Some patches ofpyrrhotite and rare chalcopyrite. 375.4 - 376.4: sulphide, quartz, minor calcite. 80% sulphides, mainly pyrrhotite, with abundant arsenopyrite disseminated in pyrrhotite and smoky quartz. Chalcopyrite is relatively abundant. Core loss 1%. 376.4 - 377.4: mainly calcite, with scattered patches of finely crystalline arsenopyrite and scattered patches of pyrrhotite with minor chalcopyrite. Core loss 1%. 377.4 - 378.4: quartz-massivesulphides. 85% sulphides, mainly pyrrhotite

84430 373.4

a4431 374.4

a4432 375.4

a4433 376.4

a4434 377.4

373.4

374.4

375.4

376.4

377.4

3?8.4

nDb Dam % % m m 0.03 1250 1630

820

1430

362@

8530

3630

0.26

0.03

0.05

0.25

0.01

0.75

0.004 74

0.01 294

0.30 2222

0.003 467

0.22 929


Prom To --.--- -- --. with disseminated arsenopyrite, minor chalcopyrite, rare galena and sphalerite. Core loss 1%. 378.4 - 379.4: quartz - massive sulphides as above. Core loss 1%.

Page: 7

No. F r q n _ _ T ~ - - . Au Ag Pb zn cu mib DDm % - % D Dm

1010 7 0.74 0.07 766 84435 378.4 379.4

Ch-l-oFitic with patches of brownish red, biotite, generally broken ground. Very rare sulphides. 379.4 - 380.8: waste.

379.4 - 380.8

Sulphide - Quartz Vein cuts core at 32 deg. 80% sulphides, mainly pyrrhotite, with minor disseminated arsenopyrite and relatively abundant chalcopyrite.

384.5 - 385.7 84441 384.5 385.7 2180 12 1.53 0.16 1356

380.8 - 381.5 Quartz - Sulphide Vein: 50% sulphides, mainly pyrrhotite, with minor disseminated arsenopyrite. Scattered chalcopyrite.

381.5 - 384.5 Gabbro: fine grained lamprophyric, badly broken ground. Slickensided cleavage cuts core at 25 to 30 deg. 381.5 - 382.5: waste 382.5 - 383.5: waste 383.5 - 384.5: gabbro waste

0.005 0.02 55 84436 379.4 380.8 20 0

84437 380.8 381.5 380 11 1.25 0.05 896

0.004 0.03 47 54438 381.5 382.5 7 6 0 0.002 0.01 92 84439 382.5 383.5 5 0

84440 383.5 384.5 27 0 0.002 0.01 45

385.7 - 388.0 Gabbro: fine grained, general 1 y sheared


and broken core, some gauge mixed with crushed calcite. Near bottom of interval shearing at 32 and 4 5 deg. to core. 385.7 - 386.7: sheared gabbro waste. 386.7 - 387.7: sheared gabbro waste. 387.7 - 388.0: sheared gabbro and calcite. Some pyrite, minor arsenopyrite iwca4cite.

388.0 - 390.0 Massive sulphide and quartz vein, abundant calcite in lower part of interval - see below. 388.0 - 389.0: massive sulphide and quartz. 80% sulphides, mainly pyrrhotite with disseminated arsenopyrite, locally abundant. Chalcopyrite is relatively abundant, rare sphalerite and galena. 389.0 - 390.0: mainly calcite uouae, with 10% disseminated Dyrite and minor scattered sphalerite. Abundant black chlorite.

390.0 - 419.2 Gabbro: gabbro interval is fine grained and lamprophyric next to sulphide veins but coarsegrainedin centre of interval. Some thin calcite veinlets scattered throughout, these are commonly barren interval and relatively competent. 418.3 - 4195: strongly sheared, abundant gouge.

84442 385.7 386.7 84443 386.7 387.7 84444 387.7 388 .O

84446 389.0 390.0

Pag,e: 8


-- Au At7 Pb Zn cu nvb pvm % % w m

0.002 0.02 35 33 0 27 0 0.005 0.01 29 12 1 0.001 0.01 138

0.89 0.23 2635 690 7

29 2 0.04 0.83 417

_ _ r . - 1.- .'

KOKANEE EXPLORATIONS L T D . DRILL HOLE RECORD Page: 9

M E T E R A G E D E S C R I P T I O N From To -. - -. - - ---__._____

390.0 - 391.0: gabbro waste. 417.2 - 418.2: gabbro waste. 418.3 - 419.?: sheared gabbro and calcite. Some pyrite and arsenopyrite, minor gal ena .

419.2 - 427.8 Massive Sulphides, minor Quartz, lessor Calc i t e : quartz occurs in massive sulphides as rounded clasts quartz "eyes." Vein cuts core at 45 deg. See sample descriptions below. 419.2 - 419.9: smoky quartz with some fine grained gabbro inclusions. Some finely disseminated arsenopyrite and minor disseminated sphalerite. 419.8 - 420.8: sulphides and uuartz. 80% sulphides, mainly pyrrhotite. Some good bands of arsenopyrite in quartz. Arsenopyrite is disseminated in pyrrhotite. Some disseminated galena in scattered patches of chalcopyrite. Chalcopyrite is widely scattered. 420.8 - 421.8: massive sulphide, minor quartz. 80% sulphides as above. 421.8 - 422.8: massive sulphides, minor quartz "eyes. I' 80% sulphide, main1 y pyrrhotite, with disseminated arsenopyrite. Some patches of heavily disseminated arsenopyrite.

S a m ~ l e No. From To -_--.-- A u Ag Pb Zn cu

84447 390.0 391.0 1 0 0.002 0.03 18 84448 417.2 418.2 7 0 0.04 0.01 74 84449 418.2 419.2 1 2 0.09 0.02 71

VDh ppm % % Dmn

84450 419.2 419.8 185 1 0 . 0 5 0.08 147

84451 419.8 420.8 l@lO 19 4 . 0 3 0.04 821

84452 420.8 421.8 2390 23 3.17 0.074 1838

84453 421.8 422.8 A850 4 0.40 0.03 1421

fJaFEEE3$oEZ~kFei3i$i50*~ =TD- Property: Vine Hole Po.: KV-90-37

Page: 10

Location: Sect.O+50E


~ ..... . .. _. .- ..---._I._-_._ ---.- -.. .~ _____ Chalcopyrite relatively abundant, rare galena and sphalerite. 422.8 - 423.8: massive sulphides and quartz. 80% sulphides. mainly pyrrhotite, with abundant disseminated arsenopyrite. Some 10.0cm intervals contain as much as 30% crystalline atsenopyrite (usually euhedral). Chalcopyrite is relative1 y abundant. Core loss 2%. 423.8 - 424.8: massive sulphide and quartz. 80 to 90% sulphides. Same as above but less arsenopyrite and chalcopyrite. Core loss 2%. 424.8 - 425.8: massive sulphide, minor quartz. 80% sulphide, mainly pyrrhotite wi t h abundant disseminated arsenopyrite in patches and bands. 10.0cm sectior with relatively abundant sphalerite and galena. Chalcopyrite is rare. 425.8 - 426.8: mainly smokv quartz. E to 10% arsenopyrite aenerally fine11 crystalline. fineiv disseminated. rare pyrrhotite. 426.8 - 427.8: mainly white bull quartz. Minor arsenopyrite mineralization.

S a m D l e From To Au A g Pb Zn cu Po.. _I--- --

wub owm % % pvm

84454 422.8

84451 425.8

84458 426.8

423.8

424.8

425.8

426.8

427.8

4560

1680

3640

120

220

4

2

13

1

0

0 . 3 0

0.12

1.82

0 .(37

0.02

0.03 3644

0.004 993

0.32 1414

0.004 136

0.01 179

KOKANEE EXPLORATIONS C T D . DRILL HOLE RECORD

Property: Vine Hole N o . : uv-90-??

pa.ae: 11


M E T E R A G E D E S C R I P T T O N From To -__.._____._____I_____._. ___.

427.0 - 430.4 Gabbro: fine grained, sheared and rubbl y core. 427.8 - 428.8: qabbro waste. 428.8 - 430.4: gabbro waste.

430.4 - 430.8 Sulphide-Quartz Vein: 80% sulphide, mainly pyrrhotiteand arsenopyrite. Cuts care at 45 deg.

430.8 - 444.0 Gabbro: generally finely crystalline, strongly foliated, foliation commonly slickensided. Some thin lenticular calcite veinlets parallel to foliation. Foliation cuts core at 51 deg and at 40 deg . FOOTWALL VEIN STRUCTURE AT 44P,O-m 430.8 - 431.8: uabbro waste.

440.0 - 457.3 Chloritic and biotitic sediments. strongly foliated, commonlv slickensided parallel to foliations. Foliation cuts core at 4 5 des. Shearinq with qouqe c u t s core at 18 deg.

END OF HOLE KV-90-37 AT 457.3m.

84459 427.8 428 .8 40 1 0 . 0 0 4 0 . 0 3 171 84460 4 2 8 . 8 430 .4 65 1 0 . 0 7 0 . 0 5 187

84461 430.4 430 .8 1320 1 5 1 . 7 6 0 . 1 2 1235

84462 430.8 431 .8 4 40 5 0 . 4 3 0.06 1.86



Hole No: KV-90-38 Length: 572.6m

Location: Sect.5t17W Start date: April 28,1990

Elevation: Azimuth: 30' Collar Dip: -60 deg.

Core Size: HQ Tests at: see attached Loaged by: ASH/DLP Date:April/May/SO

Page No. 1

Finish date:

M E T E R A G E D E S C R I P T I O N From To - 0 - 6.4 Overburden

6.4 - 12.9 Quartzite: medium and thick bedded sediments (mostly thick). Some thick beds exceptionally calcareous e.g at 10.7~1. Minor amount of thinner, more argillaceous distal and interturbidite type deposition. Bedding 50 deg. to core at 10.2111.

12.9 - 27.4 Siltstone and Argillite: thinly laminated to medium bedded sediments. Rare quartzite beds inthin/mediumrange. This interval mainly distal and.interturbidite type deposit ion

S a m p l e ___ _______-- No. From To Au Ag Pb Zn cu

ppb m m % 8 vvm

KOKANEE EXPLORATIONS L T D . D R I L L HOLE RECORD


M E T E R A G E D E S C R I P T I O N From To ---- .-___

27.4 - 36.0

36.0 - 40.1

20.4 - 20.7m: good pattern, fair contrast. 21.3 - 21.9m: good patterns and contrast (broken core). 22.7m: good pattern, fair, contrast. - 2 m : 1.5cm 23.5 - 25.0m: segmented good patterns, fair to good contrast. Bedding 50 deg. to core.

Quartzites and Siltstones: medium and thick bedded sediments. Minor amount of thinner, more argillaceous distal and interturbidite type beds (similar to 6.4 -12.9m interval). Thin sill intrusion (lamprophyre) 35.2 - 35.6~. Bedding 55 deg. to core.

Similar to 12.9 - 27.4m

Page: 2

Location: Sect.5t17W

~ ~ B ~ ~ E E o o E ~ p P k E ~ ~ z 1 5 0 N S Page: 3

Proper ty : Vine H o l e No.: KV-90-38 Locat ion: Sect.5+17W

M E T E R A G E D E S C R I P T I O N S a m p l e From To ! No. __ From To - A u m Pb Zn c u

p D b PP m % % DD m

40.1 - 74.7 Q u a r t z i t e and S i l t s t o n e : medium and t h i c k bedded sed imen t s , occas iona l t h i n i n t e r v a l s of more a r g i l l a c e o u s and t h i n n e r bedded sed imen t s , usual l y l e s s t han a m e t e r of d i s t a l i n t e r - t u r b i d i t e t ype sed iments . H e w cm of b r e c c i a t e d sediment and gouge a t 61.9m, core f o r about 1.0m o n e i t h e r s i d e is broken and b r e c c i a t e d i n p a r t ( f o o t w a l l ) due t o f r a c t u r i n g a t l o w a n g l e (10 - 2 0 deg. ) t o c o r e . Does not appear t o be a major break. Bedding 55 - 60 deg. t o c o r e .

74.7 - 80.2

80.2 - 1 1 2 . 7

S i l t s t o n e and A r g i l l i t e : t h i n l y l a m i n a t e d (predominant ) t o medium bedded s e d i m e n t s .

( I n t e r v a l a t 7 8 . 5 q = o u t c r o p samples H89- 1 and H89-16 on Vine v e i n t r e n d no r thwes t of main t r e n c h ) . Bedding 55 deg. t o co re .

Q u a r t z i t e and S i l t s t o n e : medium and t h i c k bedded sed imen t s , s i m i l a r t o 40 .I - 74.7m.


Property: Vine Hole No.:

D E S C R I P T I O N J---

M E T E R A G E From To _______ ____-

Occasional minor fracturing with moderately broken core. At 108.4111 a 15.0cm gouge healed breccia at 20 deg. to core.

112.7 - 168.9 Quartzite, Siltstone and Argillite: medium and thin bedded sediments with abundant intervals of thinner, more argillaceous sediment in thin laminated to thin bedded range. Typical Middle Aldridge type deposition. Intervals of thinner, more argillaceous beds up to 7.0m. Very minor fracturing throughout, gouge healed break, 5 2 deg. to core, at 147.3m with moderately fractured core 1.0m on footwall (minor). Occasional quartz veining up to 7.0cm, 15 to 35 deg. to core. Bedding 5 5 deg. to core.

Page: 4

KV- 90 - 38 Location: Sect.S+17W

S a m ~ 1 e No. From To Au A a Ph Zn cu - _- . - - _. -.

W-b- PDm - ._ -%-.-..- 3 -. . p pm

LTD.


M E T E R A G E D E S C R I P T I O N

168.9 - 193.6 Quartzite and Siltstone: medium and thick bedded sediments with intervals, usually less than l.Om, of thinner, more argillaceous beds in thinly laminated to medium bedded range. Well fractured, crackle brecciated in part, from 172.3 - 174.7m: badly broken in part, mot'-a major break (no gouge) Moderate to badly broken from 181.4 - 183.5m with thin zone of calcite healed breccia (3.0cm), 25 deg. to core at 182.6m, minor break indicated. From l87.5 - 189.3m core is also moderate to badly broken due to fracturing, quartz/calcite healed in part, along fractures from parallel to 10 deg. to core and brecciation along planes 55 to 60 deg. to core (along bedding planes).

193.6 - 201.2 Siltstone and Argillite: thin1 y laminated to medium bedded sediments. Mainly distal and inter turbidite type .deposition. 10.0cm of gouge and calcite healed breccia at 40 to 45 deg to core at J94.2m. Bedding 65-70 des. to core.

201.2 - 216.5 Quartzites and Siltstone: medium and thick beddedsediments similarto168.9 - 193.6m etc. Bedding 65-70 deg to core.

Page: 5

KV- 90 - 38 Location: Sect.5t17W

S a m p l e No. From To Au Ag Pb Zn cu

ppb ppm % % DPlll

KOKANEE EXPLORATIONS L T D . DRILL HOLE RECORD

Property: Vine Hole No. :


216.5 - 225.0 Quartzite and Siltstone: as above, becoming moderate to badly broken due to fracturing commonly from parallel to low angle to core, to 225.0q.

225.0 - 232.0 Quartzite and Siltstone: medium and thick bedded, as above. Fracturing less severe, occasional moderately broken core. Some quartz/calcite veining up to 12 .Ocm form 20 - 32 deg. to core, normal to bedding. Bedding 60 - 65 deg. to core.

232.0 - 232.5

232.5 - 298.2

Fault, brecciated sediments, with gouge in part, at 40 deg. to core sharp top contact with slickensides.

Quartzites and Siltstone: medium and thick bedded sediments. Usual intervals, less than 1.0m of thinner, more argillaceous distal and inter turbidite type sediments.

e

Page: 6

KV-90-38 Location: Sect.5t17W

S a m p l e - No. F r o m T o - - . - A u A a Pb Zn cu

vvb pPm % % PDm

~ ; a F e € ? E ~ o E E p P k e E B z ~ o N S - Property: Vine Hole No.: KV-90-38

Page: 7

Location: Sect.5+17W

M E T E R A G E D E S C R I P T I O N .-_-.__I - - - - ~ From To

281.0 --: calcareous siltstone interbedded argil lite. Medium to thin bedded, sharp f 1 at bedding. Abundant reddish brown biotite (similar to Lower Aldridge type)

At 285.0m: bedding to core 72 deg. At 292.0m: 10.0cm crush zone.

-

298.2 - 311.0 Siltstone interbedded Argillite: mediurr to thin bedded. Generally flat, sharE bedding. Argi 11 i te beds very thinly parallel laminated, siltstone beds general 1 y argi 1 laceous and fine grained. Scattered calcareous beds, widely scattered thin pyrrhotite laminae abundant, fine reddish biotite (similar t o Lower A1 dridge 1, abundant chlori tization along hair1 ine fractures.

311.0 - 337.2 Siltstone interbedded Araillite: mediun to thin bedded, some scattered thick beds. Bedding i s distinct and wavy, some sharp, flat beddina at top of argillite beds. Rare limy siltstone, sericite common in si 1 t s t one. Shear zone 312.5 - 315.2m, contacts not clear. Very minor gouge.

Abundant chl ori t e,

KOKANEE EXPLORATIONS L T D . DRILL HOLE R E C O R D

Proper ty : Vine Hole No.: KV-90-38

Page: 0



337.2 - 390.2 Q u a r t z i t e s and S i l t s t o n e : medium and t h i c k bedded. Bedding wavy and i n d i s t i n c t , some load c a s t s . Bed tops g e n e r a l l y marked by 2 . 0 - 15.0cm th i ck a r g i l l i t e . La the - l i k e carbonate c r y s t a l s commonly s c a t t e r e d throughout .

-- __

From 374 .1 - 374.7m rock is b recc ia t ed i n p a r t w i t h 10.0cm a t base b recc ia t ed w i t h ca lc i te m a t r i x , c o n t a c t s from 22 deg . t o 40 deg. t o co re .

398.2 - 4 0 8 . 5 S i l t s t o n e and A r g i l l i t e : medium anc t h i c k bedded sediments wi th i n t e r b e d s of t h i n n e r , more a r g i l l a c e o u s sed imen t s . T h i s i n t e r v a l is s i m i l a r t o more t y p i c a l Lower A l d r i d g e t y p e beds d i s p l a y i n g more b i o t i t i z a t i o n and Fe con ten t t han usual Middle Ald r idge type d e p o s i t i o n . Bedding 70 - 7 5 deg. t o c o r e .

S a m p l e No. From To - Au Ag Pb Zn c u

ppb m m % % m m

~ B F ~ E E ~ o E E p k e E ~ z i 5 0 N s Property: Vine Hole No.: KV-90-38

Paae: 9

Location: Sect. 5+17W


408.5 - 432.2 Quartzites and Siltstone: medium an thick bedded sediments. Rock is we1 fractured to 411.3m, causing moderate t severely broken core. Approximately10.0cmgougeandbrecciate sediment, 20 deg. to core, at 411,0111

-_ -.---- --

432.2 - 433.8 Lamprophyre sill, reacts well with 10 HC1. Base contact 62 deg. to core, ver close to parallel to bedding.

433.8 - 494.5 Quartzites and Siltstones: similar t interval from 408.5 - 432.2m. Fault from 434.3 - 43-4..-6m, brecciate sediments healed in part by calcite minor gouge, sharp base contact at 1 deg. to core (normal to bedding). Similar type break at 465.7m, 1 - 2cm o brecciated sediments in aouge at 15 deg

I ..

KOKANEE EXPLORATIONS L T D . DRILL HOLE RECORD


M E T E R A G E D E S C R I P T I O N From To ~ ____ - .. - ____

to core, normal to bedding indicating breaks are approximately perpendicular to main Vine vein structure. Occasional calcite healed breaks up main Vine vein structure. Occasional calcite healed breaks up to a few cm wide, 15 deg. to core, also normal t o bedding. Sediment fragments noted in some of the breaks, e.g. 457.6q. At 489.0111, a 15.0mm gouge filled break at 15 deg. to core, containing small brecccia fragments. Core from 490.2rg to top of vein zone at 494.5qmoderate to well fractured in part causing some broken segments.

Top of Vine vein structure at 494.5m. Base at 559.8111.

494.5m Haningwall of vein structure cuts core at 45 deg. ?

494.5 - 494.8 Massive Sulphide and Quartz Vein: mainly pyrrhotite with minor sphalerite. Rot sampled - too small and isolated.

494.8 - 511.2 Gabbro: medium to finely crvstalline, lamprophyric in part. Scattered thin, irregular quartz and calcite veinlets. 510.2 - 511.2m: gabbro waste.

KV- 90 - 38

Page: 10

L.ocation: Sect .5+17W

From To Au Ag Pb Zn cu E L - _ _ _ _ _ _ - ~ m b Dpm % % RDm

84476 510.2 511.2 75 0 O . O ? 0 . 0 9 54



5 1 1 . 2 - 5 1 3 . 7 Massive Sulphides and Quartz: some thin gabbro partings. Mineralized zone is strongly brecciated and is in a broken rubbl y condition. 5 1 1 . 2 - 512.2m: massive sulphides and quartz, minor calcite. some altered gabbro waste parting. Interval strongly sheared and brecciated. Sulphides are mainly sphalerite, minor pyrite and pyrrhotite. (30% core loss). 5 1 2 . 2 - 513.6m: massive sulphides and quartz. Some gabbro partings, all general 1 y very sheared and brecciated. sulphides are mainly arsenopyrite with abundant galena and sphalerite, some pyrite, some siderite is present. sphalerite is coarsely crystalline and orange brown. Finel y crystal 1 ine, massive arsenopyrite is commonly banded at 45 des to core. Core loss is 20%.

5 1 3 . 6 - 5 2 4 . 8 Gabbro: general medium crystalline. Brecciated from zL5_.:-_5?_4_,&3. Breccia is i n part lithified, matrix of breccia is formed by gabbro rock flour, gabbrc is altered to lamprophyric for a meter adjacent to sulphide veins.

KV - 90 - 3 8

Page: 11


S a m p l e From To AU Pb Zn cu

-!?-a -_____-_______

8 4 4 7 ? 5 1 1 . 2 5 1 2 . 2 8 9 5 0 . 4 0 2 . 1 8 166

1 6 3 0 1 3 2 . 1 5 1 . 0 7 2451 8 4 4 7 8 5 1 2 . 2 5 1 3 . 6

KOKANEE EXPLORATIONS L T D . DRILL H O L E RECORD

property: Vine Hole No.:


Shearing cuts core at 45 deg. 513.6 - 514.6tq: gabbro waste. 523.8 - 524.8m: gabbro waste, very lamprophyric. Scattered irregul ar veinlets of sphalerite and galena.

524.8 - 525.8 Quartz Sulphide Vein: 40 to 60% suaphide. Mainly pyrrhotite and pyrite, but re 1 at ivel y abundant galena and arsenopyrite near base of interval. Core loss 10%. Footwall of vein cuts core at 55 deg.

525.8 - 554.2 Gabbro: medium to coarsely crystalline, lamprophyric adjacent to footwall of sulphide vein. 525.8 - 526.8m: gabbro waste. 537.5 - 557.6m: mainly lamprophyric gabbro, generally finely crystalline, locally abundant, reddish brown finely crystalline biotite. 537.5 - 549.2tq : strongly brecciated, rubbly broken core, scattered thin gouge zones. 549.2 - 554.2m: Hagen Fault. Fracture type mineralization (pyrite, sphalerite, galena scattered throughout interval, scattered we1 1 rounded clasts of quartz - sulphide occur i n Hagen Fault breccia).

Qage: 12

Location: Sect.5+17W KV - 90 - 38 S a m p l e

- No. From - To Au Ag Pb Zn cu

a4479 513.6 514.6 3 1 0.03 0.04 a9

pDh p pm % % ppm

84480 523.8 524.0 10 2 0.13 0.20 146

84481 524.8 525.8 640 46 5.39 .78 735

a4482 525.8 526.8 6 1 0.01 0.02 155 a4483 543.2 544.2 I. 0 0.01 0.03 99

e



From To ___-_I _ _ . ~ -

544.2 - 545.2m: lamprophyric gabbro, minor fracture mineralization. Rare galena and sphalerite. 545.2 - 546.2m: lamprophyric gabbro. Re1 at ive 1 y abundant fracture mineralization, mainly aresenopyrite and p y r i t e . Sheared broken ground. Core loss 25%. 546.2 - 547.2m: fine grained lamprophyric gabbro relatively abundant. Fracture mineralization, mineralized fractures are very thin and irregular. Sphalerite, pyrrhotite commonly found in fractures. Galena is rare, pyrite is common, arsenopyrite is rare. 547.2 - 548.2m: crackle brecciated lamprophyric gabbro, with scattered small quartz-sulphide veins. Spha 1 eri te , galena, pyrite and pyrrhotite occur in quartz vein and hairline fractures.

548.2 - 549.2m: gabbro waste, brecciated and lamprophyric. 549.2 - 550.2m: brecciated gabbro. Hagen Fault - scattered sulphides in matrix - some sulphide clasts. 550.2 - 551.2m: Hagen Fault. Breccia scattered sulphides in clast and matrix.

Page: 13

KV- 90 - 38 Location: Sect.5+17W

- .. S a m p l e

.-

84484 544.2

84485 545.2

94487 547.2

84488 548.2

84489 549.2

84490 550.2

545.2

546.2

547.2

548.2

549.2

550.2

551.2

Au Pb Zn cu pph p pm % % ppm

0.04 0.06 123 37 1

0.04 1.09 159 6 1

270 1

5 1

49 1

12 1

4 90 4

0.10 0.25 185

0.01 0.02 22

0 . 0 3 0.04 66

0.05 0 . 0 7 65

0.44 0.04 341



M E T E R A G E D E S C R I P T I O N From To -

551.2 - 552.2m: brecciated gabbro, rare sulphides. 552.2 - 553.2~: brecciated gabbro. Minor scattered thin sulphide veinlets, mainly pyrite, rare sphalerite. 553.2 - 554.2m: brecciated gabbro as above. Minor scattered thin veinlets 0T-Su-l phides .

554.2 - 557.6 Siltstone: silicified in part. Abundant chloritic pyrite, minor disseminated sulphides, in chloritic fractures mainly pyrite. 554.2 - 555.2~1: altered siltstone, minor fracture mineralization.

557.6 - 560.0 Quartz Sulphide Vein 557.6 - 558.6a: qua.rtz and sulphide - 50% sulphide, mainly arsenopyrite. pyrrhotite, galena and sphalerite in roughly equal amounts. 558.6 - 560.0111: quartz and sulphide. As above but a little less sulphide in quartz near footwall side. 560.0 - 561.0111: waste sediments.

KV-90-38

Paae: 14

Location: Sect. 5+11W

From To No. I . __ . -_ -__. . .

84491 551.2

84492 552.2

84493 553.2

a4494 554.2

a4495 557.6

a4496 558.6

a4491 560.0

552.2

553.2

554.2

555.2

558.6

560.0

561.0

A 1-1 Aa Pb Z l l cu D w b m m % % m m

0.03 41 4

3

101

280

27 90

1450

2

0 0.01

1 0.08

3 0.25

1 0.12

52 7.53

19 3.11

0 0.01

0.03

0.03

0.02

2.06

0.13

0.02

63

433

39

694

826

59


- .- -- -- - - - __ From T o

559.8 - 572.6 Quartzite and Siltstone: mediur (predominant) and thick bedded sediment: with thin intervals of more distal an( inter turbidite type beds. Some similarities to more typical Lowei Aldridge type deposition in bottom 4.6m

Bedding 70 deg. to core.

END OF HOLE KV-90-38 AT 372.6m.

Paae: 15

Location: S e c t .5+17W

.K 0 K A N E E>XPLO RA.XIO NS- .- L.-T-D.-,. .

DRILL HOLE RECORD Page No. 1


Hole No: KV-90-35, Length : 570.4m

Location: Sect .2+25W Start date: 1/5/90 Finish date: 1 3 / S ! Q @

Elevation: Azimuth: 030, Collar Dip: - 7 5 deg.

Core Size: HQ Tests at: see attached

M E T E R A G E D E S C R I P T I O N S a m p l e From To - .- --.---_--

0 - 5 . 8 Overburden

5 . 8 - 5 9 . 8 Medium to thin bedded argillaceous quart zi te, quartzite, and argi 1 1 i t es . Bedding 71 deg. to core. Occasional quartz veining. Beds are very thin to 5 . 0 to 10.0 cn thick. Some sections of core are badly broken due to near parallel fractures to the core. Evidence of weatherins extends down t c

Loqged by: DMM/DLP/ASH Date: May/90

N!-.-Fr&--To-- Au A? Pb Zn cu oub porn % 8. p mn

i . -

--. 38.5111. _- Occasional thick quartzite beds up to

I 1.0m thick. Bdding 70 deg. to core at 4-6LO~. Fractures 53 deg. to core occur frequently throughout interval and are healed with quartz and calcite, grading from 95% quartz to 2 0 % quartz.

I I I

5 B 4 ~ ~ E ~ o E ~ S P k ~ @ ~ ~ 6 0 N s L T D -


Paae: 2

Locatior?: Sact.2t25W

M E T E R A G E D E S C R I P T I O N S a m p l e - A u A g Pb Zn c u 001, vom % 9i D prn

From To -- - _ _ -. +. . - --. .. . .. - . G;: From To . I I I I

60.0 - 69.2

69.2 - 99.1

99.1 - 103.6

Thin to medium bedded siltstone. Argillaceous siltstone and argillites are typically thinly laminated to 20.0~17 in thickness. Occasional quartzites. Occasional quartz/calcite veining infiilinc fractures. Bedding at 64.9m at 70 deg. to core.

Quartzite and Siltstone: Medium and thick bedded sediments with usual intervals of thinner, more argi 1 laceous distal and inter turbidite type sediments in thinly laminated t o medium beddec range. Fracturing from 23.9 - 75.6rq and 79.3 - 8 4 . 8 ~ , no major break indicated. Bedding 7 0 deg. to core.

Siltstone and Argillite: thin1 > laminated to thin bedded distal and inter turbidite type deposition.


From To-....-- _______ __- _I_______________I_

Page: 3

No. F r o m ! - T o Au A g Pb Zn cu oob DDm % % npm

E € F E E f S E W o E E ~ h e E ~ ~ 6 0 N ~ LTD-

P r o p e r t y : Vine Hole No.: KV-90-39

M E T E R A G E D E S C R I P T-I 0 N - _ _ From To -__I_..-_-__ ~ .

163.1 - 184.5 Q u a r t z i t e and S i l t s t o n e : medium and t h i c k bedded , o c c a s i o n a l i n t e r v a l s of t h i n n e r , more a r g i l l a c e o u s d i s t a l and i n t e r t u r b i d i t e t y p e b e d s w i t h th i cknesses of up t o 3O.Ocm. Note: c rushed zone from _sP__1..,2-'.-=_5_92A5?_s' w i t h b r e c c i a t e d rock and gouge m a t e r i a l ,

184.5 - 202.9

202.9 - 203.2 203.2 - 220.9

220.9 - 225.9

Limy, t h i n t o medium bedded s i l t s t o n e s and a r g i l l i t e b r e c c i a s . I n c e r t a i n s e c t i o n s t h i n beds of p y r r h o t i t e o c c u r . The c o l o r is l i g h t e r t h a n i n p rev ious s e c t i o n s .

Crushed zone. some qouge m a t e r i a l .

S i m i l a r t o s e c t i o n 184.5 - 202.9m. Limy t h i n t o medium bedded medium urey s i l t s t o n e s and a r g i l l i t e s . O c c a s i o n a l q u a r t z v e i n i n g .

Limy, t h i n t o medium bedded, medium t o d a r k g r e y s i l t s t o n e s and a r g i l l i t e s . Thin t o medium bedded. O c c a s i o n a l q u a r t z v e i n s .

Page: 4

Loca t ion : Sect.2+25W


property: Vine Hole No.


2 2 5 . 9 - 262.4

Small interval s of crackle breccias. Crushed zone with some gouge material from 2 1 7 . 1 - 2 1 7 . 5 ~ ~ . Fractures occur at 32 deg. to the core, bedding occurs at 7 0 deq. to the core. Both measurements at 2 2 3 . 4 m .

Siltstone and Quartzite: medium to thick bedded, light to medium grey. Common occurrences of laminated argillite from a few cm to in excess of 1. Om thickness. Broken zone occurs from 260.9 - 261.5m. Minor amount of gouge material. The quartzites are becoming light and appear to contain fine grains of biotite. There are also small intervals of crackle breccias. Quartz veins normal to bedding mineralized with pyrite and pyrrhotite.

2 6 2 . 5 - 3 0 1 . 2 Quartzite, Siltstone and Argillite: medium to thick bedded. The argillite is thinly laminated. The quartzite is similar in character to the previous section. Quartz veining occurs toward bottom of section. Veins are normal to bedding and contain biotite, pyrrhotite and pyrite.

P a q e : 5

: KV-90-39 Location: Sect.2+25W


_____ ______ Zn C,U From To

301.2 - 328.2 Medium bedded siltstones and argillites. Occasional thick bedded siltstone. Crack1 e breccias are not uncommon. Quartz veining also common, normal to bedding. Other vein minerals include brown biotite, pyrrhotite and pyrite.' Crushed zone occurs from ,318.2 - 319.lm, 15 deg. t o core, some gouge material present.

No Fro!? To A u A 4 Ph -- ~ -.-- - n&L E!!! ~ Sj % PPPl

328.2 - 356.6 Medium bedded to thick bedded siltstone and argillite. Crackle breccia and quartz veins occasionally. Dominant fractures 20 deg. to core. Fractures are infilled with quartz and appear to be chloritized, there is also pyrrhotite present, as in previous sections. Crus-hed zone occurs from 319.7 - 320.0m, near parallel to bedding. Some gouqe rnaterial and slickensides present.

KOKANEE G X P L 0 R A T I O N . S LTD DRILL HOLE RECORD

Property: Vine Hole No.

M E T E R A G E D E S C R I P T I O N F r b m T o -I____ . .

356.7 - 361.3 Predominantly thin to medium bedded si 1 tstone , argi 1 1 i te and quartzite . Crackle breccias not uncommon a s is the case with small quartz. veins <5.0mm wide. The quartz veins, as in previous sections, contain pyrite and pyrrhotite. A significant breccia zone occurs from X ? . L , 8 ! 3 7 2 , 7 m . Zone is cemented with quartz, calcite, pyrrhotite and pyrite. There is not much indication of movement as no significant amount of gouge material is present. The brecciated material is altered with pyrite.

1163 - / / l a

361.3 - 378.2 Sullivan Horizon: thin beds of pyrrhotite, breccia zone as above. o-p&- IL3S Contact characterized by a fine mud sequence at the tou and bottom of the zone. Reddish biotite accqunts for the pink color of the surface of the r o c k s .

381.7 - 410.4 Siltstone and Argillite: thin to medium bedded. Common thin beds of pyrrhotite. Beds are cleaner than in previous

Siltstones frequently contain sericite mica which gives the cut

/W[ - 1338 sections.

Psae: I

: w - 9 0 - 3 9 Location: Sect.2+?5W

KOKANEE E X P L O R A T I O N S 1.TD - D R I L L HOLE RECORD

p r o p e r t y : Vine Hole No.: K V - 9 0 - 3 9

Page: 8

L o c a t i o n : Sect. 2+25W

M E T E R A G E D E S C R I P T T O N From To ~ . - - - - - __

4 1 0 . 4 - 4 3 6 . 3

[ ab -’Y-

s u r f a c e an even “ s a l t and pepper” t y p e of appearance. Crushed zone f r o m 385.2 - 385.6m, m i n o r gouge b c a l c i t e p r e s e n t .

T h i n t o medium bedded s i l t s t o n e , q u a r t z i t e and a rg i l l i t e . ’ Occasional t h i c k bedded q u a r t z i t e . A r g i l l i t e is l i g h t g r e y t o l i g h t g r e y g r e e n i n c o l o r . The q u a r t z i t e is p i n k i s h due t o t h e p r e s e n c e of red b i o t i t e . Thin bands of p y r r h o t i t e a r e n o t uncommon. A b r e c c i a zone occurs from 4 2 9 . 4 - 4 3 0 . 3 ~ 3 .

Medium t o t h i c k bedded q u a r t z i t e s and a r g i l l a c e o u s s i l t s t o n e . Thin bedded a r g i l l i t e s a re n o t uncommon. The s i l t s t o n e s a r e a l t e r e d and c o n t a i n s r e d b i o t i t e , some c o n t a i n s e r e c i t e m i c a and a i v e a peppery c h a r a c t e r t o t h e b e d s . B r e c c i a z o n e s o c c u r f r e q u e n t l y t h r o u g h o u t % h e s e c t i o n . Minor gouge is p r e s e n t i n s e v e r a l of t h e b r e c c i a zones b u t no s i g n i f i c a n t movement is i n d i c a t e d . Calcareous s i l i c e o u s v e i n i n g is common.

K O K A N E E EXPLORATIONS L T D - DRILL * H O L E R.ECORD

Prope r ty : Vine Hole N O . : KV-90-39

483.5 - 489.9

489.8 - 491.3

491.3 - 492.0

491.5

491.5 - 492.5

492.5 - 493.5

493.5 - 496.6

F a u l t zone c o n t a i n s f r a q m e n t s t h a t a r e a n g u l a r i n n a t u r e . S i g n i f i c a n t gouge m a t e r i a l , c a l c i t e and q u a r t z . Some of t h e f r a g m e n t s a r e q u i t e l a r a e , up t o 2 0 . 0 ~ ~ 1 long. S u l p h i d e s ( m o s t l y p y r i t e ) a r e a l s o p r e s e n t .

B r e c c i a t e d Lower A l d r i d g e . Minor gouge p r e s e n t .

Vein s t r u c t u r e c o n s i s t i n g p redominan t ly o f m a s s i v e s u l p h i d e s , p y r i t e . p y r r h o t i t e , g a l e n a a n d spha ler i te .

HANGINGWALL V E I N STRUCTURE, CUTS CORE AT 72 deg .

Massive S u l p h i d e Veins: 70% s u l p h i d e , mainly p y r r h o t i t e , l e s s o r g a l e n a and a r s e n o p y r i t e . Rare cha 1 c o p y r i t e .

Larnprophyr i c Gabbro : f i n e 1 y c r y s t a 1 1 i n e , f r a c t u r e d rubb ly c o r e . S c a t t e r e d i r r e g u l a r c a l c i t e v e i n l e t s , u s u a l l y w i t h weak1 y d i s s e m i n a t e d s u l p h i d e .

S i l t s t o n e : c r a c k l e b r e c c i a t e d , p y r i t e , p y r r h o t i t e , r a r e s p h a l e r i t e and galena i n f r a c t u r e s .

Paae: 9

Locat ion: Seck.?+25W

84463 490.5

84464 491.5

491.5 7 0.002 0.01 8 0

492.5 2870 21 2.98 0 . 0 2 1042

~ ~ F E E E 1 3 0 E ~ p k E i e ~ i 5 0 N s Property: Vine Hole N o . : KV-90-39

U E T E R A G E D E S C R I P T I O N From-20 __ __ -. .___-_._ _. _. . - -. . -_ _ _ , . . - __ __. _ _ - ..

492.5 - 493.5: fine arained. lamprophyric gabbro. Rare fracture mineralization. 493.5 - 494.5: crackle brecciated sediments. Minor sulphides in fractures. 494.5 - 496.6: mainlv fault gouge and brecciated sediments.

496.6 - 497.6 Quartz-massive Sulphide Vein: 50% sulphides, mainly pyrrhotite, rare arsenopyrite, abundant massive black chlorite in irregular fractures, chlorite appears to be late. Pyrite is relatively abundant.

497.6 - 5 2 8 . 0 Gabbro: general 1 y coarse grained gabbro - becomes fine grained adjacent to sulphide veins. Lamprophyric, thin mineralized quartz and calcite veinlets throughout. 497.6 - 499.8: brecciated with partlv lithified rock flour matrix. 520.4 - 520.2: quartz vein contains minor pyrrhotite. 497 L 5- - :..- _. -4_q8_.6 : aabbro waste (brecciated). 527.0 - 528.0: aahhro w a s t e .

528.0 - 531.5 Quartz-Sulphide Vein: 70% sulphide, mainly pyrrhotite, scattered crystals of arsenopyrite, estimated 2% t o 5%

Paae: 10


S a m n l e _-.~-__.____._________I___.__.____ .___ -- No: From To -. A u A 3 P b Z!-l c u

% % oDm pob D T ) ~ 0.01 0.02 69 84465 492.5 493.5 5 6 G 0

0.05 0.02 78 84466 493.5 494.5 1 1

84467 494.5 496.6 9 0 0.01 0.01 26

84468 496.6 497.6 2460 4 0.34 0.01 831

84469 497.6 498.6 21 0 0.01 0.02 10

? o.81 0.07 72 84470 527 .O 528 .O 11


property: Vine Hole No.: KV-90-39

Paqe: 11

Location: S e c t . 2+25W

M E T E R A G E D E S C R I P T I O N _ _ -

in patches. Some small scattered pyrite prophyroblasts, sphalerite and chalcopyrite are rare, abundant chlorite in late fractures. 5 2 8 . 0 - 529.0: quartz and massive sulphides. 529.0 - 531.5: auartz and massive sulphides.

531.5 - 533.6 Gabbro: fine grained and carbonatized adjacent to sulphide vein (1 meter). Brecciated to 532.6111. Footwall contact -sheer cut - breccia has lithifiec matrix. 531.5 - 532.51q: mainly carbonatizec gabbro. Scattered patches of pyrrhotite, lessor pyrite and arsenopyrite. 532.5 - 533.6m: uabbro breccia.

533.6 - 534.5 Quart z-Calci te Vein : 533.6 - 534.5m: quartz calcite vein, minor pyrrhotite. rare arsenopyrite, minor chlorite. Base of vine vein structure 534.5 - 570.4 Quartzite and Siltstone: medium and thick bedded sediments predominantlv, with intervals, less thar 1.0m of distal and inter turbidite type deposition (thinner bedded and m o r e argillaceous). This interval part of "Footwall Quartzites."

84471 528.0

84472 529.0

84473 531.5

a4474 532.5

a4475 533.6

529.0 1690

531.5 3310

532.5 125

533.5 5

534 * 5 13

2 0.14

1 2 2.0

9 1.47

0 0.01

0 0.01

0.01

0 * 2 @

0.12

0.01

0.003

1445

97 5

988

9

119

5 e F f e E E E i o E E ~ k E E B i s i 5 0 N s L T D -


Page: 12


M E T E R A G E D E S C R I P T I O N From To ~ _.

Erratic, calcite healed fracturinc common. A few cm of even. parallel laminated sediments at 5&z,_lm similar tc footwall uuartzite marker tvpe. Beddina 70 des. to core.

END OF HOLE KV-90-39 AT 570.4M

b kokanee explorations ltd, report on four …

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