geological and geochemic .f ffipptpd:t

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.f FfiPPtPd:t 1 Geological and Geochemic - on the - Mac Property Kamloops Mining Division, British Columbia 92P/lW and 921/16W - for - Eighty-Eight Resources Limited #904 - 675 west Hastings Street Vancouver, R. C. V6B 1N2 Prepared by: G. Belik h Associates 1815 North River Drive Kamloops, B. C. V2B 7N4 - - __ ASSESSMENT REPORT

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Page 1: Geological and Geochemic .f FfiPPtPd:t

.f FfiPPtPd:t 1 Geological and Geochemic

- on the -

Mac Property

Kamloops Mining Division, British Columbia 92P/lW and 921/16W

- for -

Eighty-Eight Resources Limited #904 - 675 west Hastings Street

Vancouver, R. C. V6B 1N2

Prepared by:

G. Belik h Associates 1815 North River Drive

Kamloops, B. C. V2B 7N4

- - _ _ A S S E S S M E N T R E P O R T

Page 2: Geological and Geochemic .f FfiPPtPd:t

Table of Contents

INTRODUCTION . CLAIMS

LOCATION AND ACCESS . PHYSIOGRAPHY AND VEGETATION

GENERAL GEOLOGICAL SETTING

PREVIOUS EXPLORATION

PROPERTY GEOLOGY

Sedimentary Rocks

Intrusive Rocks

Plateau Basalts

Quartz Veininq . SOIL GEOCHEMISTRY .

Discussion of Results

ROCK GEOCHEMISTRY . CONCLUSIONS

REFERENCES

Figures :

1064-1 : Location Map

1064-2 : Claim Map . 1064-3 : Geological Plan and Sample Locations

1064-4 : Rock Sample Locations 94 Mac 15,16,26-44,46-48

1064-5 : Gold in Soils

Paqe No.

2

3

5

5

6

6

7

8

8

9

9

10

11

12

12

16

1

4

pocket

13

pocket

Page 3: Geological and Geochemic .f FfiPPtPd:t

Appendix :

I: Soil Geochemical Results

11: Rock Geochemical Results

111: Statement of Expenditures

IV: writer's Certificate

Page 4: Geological and Geochemic .f FfiPPtPd:t

I MAC CLAIMS I KAMLOOPS Ma 92 P/0.

Page 5: Geological and Geochemic .f FfiPPtPd:t

.

2 .

INTRODUCTION

This report summarizes the results of soil sampling, prospec-

ting and geological mapping carried out over parts of the Mac

1-20, two-post claim block during June 8-10, 13, 14 & 20,

July 12, August 15 and September 5 , 1994.

The Mac claims cover the western part of the former Bona-

parte East Property. The Bonaparte Properties, consisting of

the Bonaparte East, Bonaparte Discovery and Bonaparte West,

were staked in stages between 1984 and 1987 by MineQuest Ex-

ploration Associates Limited of Vancouver, B. C., as a result

of the discovery by MineQuest of widespread, high-grade, gold-

quartz float in a area centered about 500 metres west of the

Mac claims. Subsequent drilling and trenching by MineQuest

identified six close-spaced, narrow, steeply-dipping, en ech-

elon vein structures in this area trending approximately north.

In 1994, selective, shallow open-cut mining was carried out

along segments of some of the veins by Cleveland Capital Cor-

poration which resulted in the removal of approximately 10,000

tons of material grading approximately 0.9 oz/ton gold.

During their tenure, MineQuest completed detailed soil

sampling over a large part of the Bonaparte Project Area which

resulted in the identification of several strong, albeit some-

what spotty, gold anomalies with values up to 3270 ppb. Sev-

Page 6: Geological and Geochemic .f FfiPPtPd:t

3

era1 of the strongest anomalies occur within the Mac claim

area.

The main focus of the 1994 program was to locate targets

for evaluation by trenching or drilling within the known soil

anomaly areas by utilizing a combination of confirmatory/infill

soil sampling, float prospecting and detailed mapping.

CLAIMS

The property is comprised of 20 contiguous two-post claims

as detailed below:

Claim

Mac 1 Mac 2 Mac 3 Mac 4 Mac 5 Mac 6 Mac 7 Mac 8 Mac 9 Mac 10 Mac 11 Mac 12 Mac 13 Mac 14 Mac 15 Mac 16 Mac 17 Mac 18 Mac 19 Mac 20

Record NO.

323605 323623 323624 323625 323626 323627 323628 323629 323630 323631 323632 323633 323634 323635 323636 323637 323638 323639 326159 326160

Date Recorded

Feb. 1, 1994 Feb. 1, 1994 Feb. 1, 1994 Feb. 1, 1994 Feb. 1, 1994 Feb. 1, 1994 Feb. 4, 1994 Feb. 4, 1994 Feb. 4, 1994 Feb. 4. 1994 Feb. 4, 1994 Feb. 4, 1994 Feh. 4, 1994 Feb. 4, 1994 Feb. 4, 1994 Feb. 4, 1994 Feb. 4, 1994 Feb. 4, 1994 May 30, 1994 May 30, 1994

The owner of record for the Mac 1-20 claims is Eighty-Eight

Page 7: Geological and Geochemic .f FfiPPtPd:t

\ P \

/ J

EIGHTY - EIGHT RESOURCES LTt

CLAIM SKETCH M A C C L A I M S

KAMLOOPS M.D. 9 2 P / 8

DATE JAN./95 I SCALE 1.30,OOO

DWN BY DBM DWG NO 1064-2

Page 8: Geological and Geochemic .f FfiPPtPd:t

5

Resources Limited, #904 - 6 7 5 West Hastings Street, Vancouver,

B. C.

LOCATION AND ACCESS

The Mac claims are located in south-central British Colum-

bia about 30 km north of the city of Kamloops. The geographic

center of the claim area is at 5 1 ' 0 1 ' north latitude, 1 2 0 ' 2 5 '

west longitude.

The property can be reached by travelling north from Kam-

loops, along the Westsyde/BlackPine road, then up Weyerhauser's

Jamieson Creek haul road to sign post 14K, thence up the Went-

worth Creek road for about 4 km, then up the Bob Creek road

which connects with the Bonaparte Mine access road which passes

through the northern part of the claim area. The total trav-

elling time from Kamloops to the property is about 1 hour.

PHYSIOGRAPHY AND VEGETATION

The Mac property is situated along the southern edge of

the Fraser Plateau. Relief within the claim area is gentle

to moderate. Elevations range from 5000 ft. to approximately

5 8 0 0 ft.

Page 9: Geological and Geochemic .f FfiPPtPd:t

6 .

The property is covered for the most part by mature

stands of spruce, balsam and fir with relatively thin under-

brush. Some logging has occurred on the Mac 7, 16 & 18 claims.

GENERAL GEOLOGICAL SETTING

The claim area is predominantly underlain by argillite,

greywacke, phyllite and slate of the Late Paleozoic Cache

Creek Group. Dark green augite porphyry flows and black ar-

gillite, similar to the Triassic Nicola Group, outcrop imme-

diately east of the claim area. Basement lithologies in the

northwest sector of the claim area are concealed beneath flat-

lying Miocene basalt flows.

Two small stocks and several dykes of hornblende diorite

of probable early Mesozoic age are partly exposed within the

claim area. The stocks contain marginal zones of foliated

diorite interlayered with siliceous pyritic hornfels and minor

skarn which grade outward into broad zones of dark grey to

black pyritic hornfels.

PREVIOUS EXPLORATION

Between 1969 and 1979 exploration for molybdenum was

Page 10: Geological and Geochemic .f FfiPPtPd:t

7.

carried out within the area of the Mac claims. In 1973,

Amoco Canada completed geological mapping, soil sampling,

induced polarization/magnetic surveys and drilled two core

holes on the Mac 12 claim totalling 299 metres.

In 1984 MineQuest, on behalf of the GoldQuest I Limited

Partnership discovered high-grade gold quartz float about 500

metres west of the Mac claims. Subsequent drilling and trench-

ing identified six close-spaced, narrow, en echelon auriferous

quartz veins trending north to northeast. Concurrent with

the drilling and trenching programs, MineQuest conducted de-

tailed geological mapping, extensive soil sampling and both

ground and airborne magnetic/VLF-electromagnetic surveys.

During June to September, 1994, Cleveland Capital Corpora-

tion carried out a pilot mining program in the Discovery Area

and removed approximately 10,000 tons of material for custom

processing at the Trail smelter.

PROPERTY GEOLOGY

Results of the geological survey are presented in Map

1064-3 at a scale of 1:5000. A ribboned survey grid, con-

structed by MineQuest between 1984 and 1988, was utilized for

control.

Page 11: Geological and Geochemic .f FfiPPtPd:t

8

Sedimentary Rocks

The claim area is mainly underlain by fine-grained black

clastic units of the Late Paleozoic Cache Creek Group. In

the southern part of the area mapped these units are comprised

of fissile black slate, siliceous argillite, thinly laminated

grey arenaceous phyllite and grey to black micaceous phyllite.

Bedding is highly variable but has a overall general east-west

strike with moderate southerly dips. Conformable, predefor-

mational, quartz vein/lenses locally are developed.

In the northern part of the area mapped, sediments sur-

rounding several diorite intrusive bodies have been converted

into a broad zone of resistant, hard, dense, light grey to

black, pyritic hornfels. The immediate contact area along

two of the intrusive bodies is marked by a zone of foliated,

silicified pyritic diorite interlayered with pyritic, light

grey/green, siliceous hornfels and minor garnet-epidote skarn.

Intrusive Rocks

A number of small, irregular-shaped diorite stocks and

dykes intrude the claim area. Diorite stocks typically are

fine-to medium-grained with less than 10% quartz, 5% to 10%

Page 12: Geological and Geochemic .f FfiPPtPd:t

9.

hornblende and minor biotite and pyrite. Dykes tend to be

finer-grained and locally porphyritic.

Plateau Basalts

Flat-lying olivine basalt flows cover most of the Mac 3,

5 S. 6 claims. The flows are grey to dark brown, fine-grained

and locally vesicular. Columnar jointing is well-developed

in flows exposed in bluffs north of the claim area and to the

southwest along the upper reaches of Wentworth Creek.

Quartz Veininq

Quartz veins and quartz vein float are common within and

peripheral to the diorite intrusions. All vein orientations

mapped trend northerly with near verticle to steep easterly

dips. The maximum exposed width noted is about one metre.

Most of the exposed quartz veins and quartz float are

milky white to translucent white with minor sulphide. Pyritic

quartz float was noted at a few locations and a 30 cm wide

vein of pyritic quartz with minor chalcopyrite is exposed on

the left bank of Cooler Creek at approximate grid co-ordinates

2930N, 4740E.

Page 13: Geological and Geochemic .f FfiPPtPd:t

SOIL GEOCHEMISTRY

During the 1994 program, 168 soil samples were collected

to confirm previous survey results in two areas of the prop-

erty. Samples were collected at 20 metre intervals along

pre-existing grid lines in order to provide uniformity for

comparison with previous results. Minor infill sampling was

carried out in one area to provide further detail.

Samples were obtained by digging with a maddock to a

depth of 30 cm to 40 cm. The "C" horizon was sampled or in

some cases the " R " horizon depending on soil development at

each site. In most cases the material collected consisted

of tan, compact, moist, clay-rich till.

Samples collected were placed in kraft envelopes with

the grid co-ordinates marked on each envelope with an indel-

ible felt pen.

All samples were shipped to Acme Labs located in Vancouver,

B. C. and analysed for gold by F.A./I.C.P. from a 10 gm of

-80 mesh material. Results are presented in Plan 1064-5 at a

scale of 1:5000.

Page 14: Geological and Geochemic .f FfiPPtPd:t

11.

Discussion of Results

Gold values from the sites sampled range from less than

1 ppb to 440 ppb with 22 of the samples exceeding 20 ppb which

is considered to be the anomalous threshold for this area.

Ten samples returned values greater than 100 ppb and are

categorized as definitely anomalous. In general the 1984

sample results confirm previous survey results although there

is a large discrepancy between individual sample sites which

may be due to a nugget effect.

Based on the results of this year's sampling, a large

anomalous zone identified by MineQuest in the west-central

part of the property has been divided into three possible sub-

anomalies designated anomalies 'A', ' B ' and 'C' on Plan 1064-5.

Anomalies 'A' and 'BE are parallel en echelon features with an

apparent northwesterly elongation, which may be the result of

glacial down-ice dispersion. Anomalies 'A' and 'B' may have

a single source located up-ice to the northwest. Alternately

the anomalies may have separate sources located near their

northwest leading edges.

Anomaly 'C' is essentially a two-station anomaly which

straddles a swampy draw located between 4600E and 4660E on

line 3500N.

Page 15: Geological and Geochemic .f FfiPPtPd:t

Anomaly ' D ' is located about 1 km southeast of anomaly

'A'. A large discrepancy also exists in this area between

previous results and this year's results. The source of the

anomaly is not known.

ROCK GEOCHEMISTRY

Sampling of exposed quartz veins and quartz vein float

within the area surveyed failed to locate mineralization sim-

ilar to that located on the adjacent Bonaparte property. Of

the 68 samples collected, only two (Mac 1 and Mac 22) returned

moderately encouraging values of 480 ppb and 7 5 0 ppb gold re-

spectively. Both samples are from angular quartz float loca-

ted within the area of soil anomaly 'A'.

A complete list of all sample assay results

Appendix 11. Sample locations are shown on maps

1064-4.

CONCLUSIONS

s given in

064-3 and

1. The Mac claims are underlain by deformed black clastic

units of Late Paleozoic age which have been intruded by

Page 16: Geological and Geochemic .f FfiPPtPd:t

3000 N

2950 N

2900 N

M27 \ , M E ..-.,

M33 I . . .?., , . 3 : ...,. . . I

. i

t I . . .. .

'.__.

I

W

0 ID I0 rt

...... .. . '._ ....' I

W 0 U b U

0 10 20 30 40 50metres

BAR SCALE: 1.1000

LEGEND

T.. \...

...... . .. . . %._. , .: '

,;'fl. ._ . ,.. .. 4m /--

/

/M34

X

CREEK

OUTCROP

QUARTZ V E I N

CLUSTER O F ABUNDANT QUARTZ FLOAT BLOCKS

PROJECTED EXTENSION O F QUARTZ V E I N STRUCTURE

QUARTZ VEIN 0 RI E NTATl ON

SAMPLE LOCATION

FLOAT LOCAT

SAMPLE ON

EIGHTY -EIGHT RESOURCES LTD

MAC PROPERTY ROCK S A M P L E L O C A T I O N S

94 MAC 15,16, 2 6 - 4 4 , 4 6 - 4 6

IDate' NOV. 1 9 4 rechnlcol Work by:

)rawn by : G. D. BELIK

Figure No. 1064 - 4 DBM

Page 17: Geological and Geochemic .f FfiPPtPd:t

14.

small diorite stocks and dykes. Broad zones of pyritic

hornfels are developed adjacent to the intrusive. Mio-

cene plateau basalts cap sections of the property.

2. A large number of anomalous to highly anomalous gold

values in soil occur scattered over most of the claim

area. Clusters of anomalous values appear to define a

broad anomalous 'zone' within the west-central part of

the property which has a general northwesterly trend.

3 . Assay results of samples collected from a number of quartz

veins and extensive quartz float within and peripheral

to the main soil anomalies were disappointing. Mod-

erately encouraging values of 480 ppb and 7 5 0 ppb gold

were obtained from two samples of angular quartz float

in one soil anomaly area.

4. Detailed mapping and prospecting failed to locate a def-

initive source or sources for the extensive gold soil

anomalies located within the claim area. A possible

source may be low-grade gold mineralization within seg-

ment of quartz veins similar to those mapped. The pres-

ence, however, of high-grade veins similar to those on

the adjacent Bonaparte property, is also a definite poss-

ibility; the geological setting in both areas is similar

and large areas of the Mac claims are totally concealed

Page 18: Geological and Geochemic .f FfiPPtPd:t

15.

by overburden.

5. Further work on the Mac claims is warranted. A trenching

program, to evaluate the up-ice leading edges of soil

anomalies ' A ' and ' B ' , is recommended.

Page 19: Geological and Geochemic .f FfiPPtPd:t

16.

REFERENCES

Campbell, R.B., and Tipper, H.w., (1965): Geology of Bonaparte Lake Map-Area, British Columbia; G.S.C. Memoir 363

Dvorak, Z., (1987): Airborne Geophysical Survey, Bob Claims; Assessment Report 16,137

Gourlay, A.W., (1985): North Thompson Claims Geology and Geo- chemistry, Kamloops Mining Division; Assessment Re- port 13,908

Gourlay, A.W., (1988): Bonaparte Discovery Belt, 1988 Summer Field Program, Geochemistry, Geophysics and Geology, May-August, 1988; Assessment Report 17,904

Page 20: Geological and Geochemic .f FfiPPtPd:t

Appendix I

Soil Geochemical Results

Page 21: Geological and Geochemic .f FfiPPtPd:t

3

ACME ANALYTICAL LABORATORIES LTD. 852 E. HASTINOS ST. VANCOUVER B.C.

GEOCHEMICAL ANALYEIIB CERTl 0. Belik h Aasoc. Ltd. F i l e i

1815 North River Drive, Kaloops SC Y;

SAMPLE#

MAC L37+00N 43+20E MAC L37+00N 43+403 MAC L37+00N 43+60E MAC L37+00N 43+803 MAC L37+00N 44+00E

MAC L37+00N 44+203 MAC L36+50N 43+203 MAC L36+50N 43+403 MAC L36+50N 43+60E MAC L36+50N 43+80E

MAC L36+50N 44+00E MAC L36+50N 44+203 MAC L36+50N 44+40E MAC L36+00N 43+603 MAC L36+00N 43+80E

MAC L36+00N 44+00E MAC L36+00N 44+20E MAC L36+00N 44+403 MAC L35+75N 43+803 MAC L35+75N 44+00E

MAC L35+75N 44+203 MAC L35+75N 44+403 RE MAC L35+75N 44+40E MAC L35+75N 44+603 MAC L34+25N 44+603

MAC L34+25N 44+80E MAC L34+25N 45+00E MAC L34+25N 45+20E STANDARD AU-S

Au* PPb

2 2 2 9 9

4 3 3 3 2

2 3 2 7 <1 2 1 <1 3

13

2 11 7 4 2

2 13 A 6

- SAMPLE TYPE: SOIL AU* ANALYSIS BY ACID

DATE RECEIVED: SEP 14 1994 DATE REPORT MAILED: CERTIF IED B.C. ASSAYERS

Page 22: Geological and Geochemic .f FfiPPtPd:t

G. Belik & Assoc. Ltd. PROJECT 1061 FILE # 94-2790 Page 3

AU* DDb

SAMPLE# m r -"lN

MAC 35+25N 44+00E MAC 35+25N 44+20E MAC 35+25N 44+40E MAC 35+25N 44+60E MAC 35+25N 44+80E MAC 35+25N 45+00E RE MAC 35+25N 45+00E MAC 34+75N 44+40E MAC 34+75N 44+60E MAC 34+75N 44+80E

3 6

130 5 3

4 3 1 7 18

MAC 34+75N 45+00E STANDARD AU-S

4 8

110 8 5

3 50

Sample tYDe: SOIL. Samples beqinninq 'RE' are duplicate samples.

Page 23: Geological and Geochemic .f FfiPPtPd:t

0 . Belik h Assoc. Ltd. PROJECT 1060 FILE # 94-2140

L35+00N 44+20E L35+00N 44+40E L35+00N 44+60E L35+00N 44+80E L35+00N 45+00E

L35+00N 45+20E L35+00N 45+40E L35+00N 45+60E L35+00N 45+80E L35+00N 46+00E

L35+00N 46+60E L35+00N 46+80E L35+00N 47+00E L35+00N 47+20E L34+50N 44+60E

RE L34+50N 44+60E L34+50N 44+80E L34+50N 45+00E L34+50N 45+20E L34+50N 45+40E

L34+50N 45+60E L34+50N 45+80E L34+50N 46+00E L34+50N 46+20E L34+50N 46+40E

L34+50N 46+60E L34+50N 46+80E L34+50N 47+00E L34+50N 47+20E L34+00N 44+80E

L34+00N 45+00E L34+00N 45+20E L34+00N 45+40E L34+00N 45+60E L34+00N 45+80E

STANDARD AU-S

Page 2 QQ 2

110 11 11

2

2 3 2 3

4 6

2 2 0 5 3 3 4

3 3 7 0

7 2 7

4

33 3 4 5 3

5 3 3 3

11

8 6 9 8 6

Sample tvpe: SOIL. Samples becrinnins 'RE' are duplicate samples.

Page 24: Geological and Geochemic .f FfiPPtPd:t

SAMPLE#

L34+00N 46+20E L34+00N 46+40E L34+00N 46+603 L34+00N 46+80E L34+00N 47+00E L34+00N 47+20E L34+00N 47+40E L34+00N 47+60E L34+00N 47+80E L33+50N 44+80E

L33+50N 45+00E L33+50N 45+20E L33+50N 45+40E L33+50N 45+60E L33+50N 45+80E

L33+50N 46+00E L33+50N 46+203 L33+50N 46+403 RE L33+50N 46+403 L33+50N 46+60E

L33+50N 46+80E L33+50N 47+00E L33+50N 47+203 L33+50N 47+40E L33+50N 47+60E

L33+50N 47+80E L33+00N 45+403 L33+00N 45+60E L33+00N 45+803 L33+00N 46+00E

L33+00N 46+203 L33+00N 46+403 L33+00N 46+603 L33+00N 46+80E L33+00N 47+00E

m r W I L I T l O L

Au* PPb

STANDARD AU-S

1 1

13 2 2 3 3 1 2 7

3 4 2 12 4

2 3 4 3 2

7 4 3 2 2

24 8 5 5 11

5 4

440 8 4

Samule tvue: SOIL. Samules besinnins 'RE' are duulicate samules.

Page 25: Geological and Geochemic .f FfiPPtPd:t

SAMPLE# AU* pub

Sample type: SOIL. Samples beqinninq 'RE' are duplicate samples.

L33+00N 47+20E L33+00N 47+403 L33+00N 47+60E RE L33+00N 47+603

3 8 10 1 3

Page 26: Geological and Geochemic .f FfiPPtPd:t

SAMPLE#

MAC 31+50N 4 6 + 6 0 E MAC 3 1 + 5 0 N 4 6 + 8 0 E MAC 31+50N 4 7 + 0 0 E MAC 3 1 + 5 0 N 4 7 + 2 0 3 MAC 3 1 + 5 0 N 4 7 + 4 0 3

MAC 3 1 + 5 0 N 4 7 + 6 0 E MAC 31+50N 47+80E MAC 31+50N 48+00E MAC 3 1 + 5 0 N 4 8 + 2 0 3 MAC 3 1 + 5 0 N 48+40E

MAC 31+50N 4 8 + 6 0 E MAC 3 1 + 5 0 N 48+803 MAC 3 1 + 5 0 N 4 9 + 0 0 E MAC 10+00N 2+40E MAC 10+00N 2+60E

MAC 1 0 + 0 0 N 3+00E MAC 1 0 + 0 0 N 3+20E MAC 1 0 + 0 0 N 3 + 4 0 E MAC 1 0 + 0 0 N 3 + 6 0 E MAC l O + O O N 3+80E

MAC 1 0 + 0 0 N 4+00E MAC 10+00N 4+20E MAC 1 0 + 0 0 N 4+40E RE MAC 10+00N 4+40E MAC 10+00N 4 + 6 0 E

MAC 1 0 + 0 0 N 4+80E MAC 10+00N 5+00E MAC 1 0 + 0 0 N 5+20E MAC 1 0 + 0 0 N 5 + 4 0 E MAC 1 0 + 0 0 N 5 + 6 0 E

MAC 10+00N 5 + 8 0 E MAC 1 0 + 0 0 N 6+00E STANDARD AU-S

AU* PPb 11

8 2 2 1 4

6

8 2 2 97 98

1 2 0

2 5 7 4 '4- 4

1 0 3

1 2 4 7

1 2 100

1 6 13

7

430 1 2 2 4 2 1

5

5

Sample type: SOIL. Samples beqinninq 'RE' are duplicate samples.

- - - - - - - - - - - - -

Page 27: Geological and Geochemic .f FfiPPtPd:t

L23+00N 50+40E L23+00N 50+60E L23+00N 50+80E L23+00N 51+00E L23+00N 51+20E

L23+00N 51+40E L23+00N 51+60E L23+00N 51+80E L23+00N 52+00E L23+00N 52+20E

L23+00N 52+40E RE L23+00N 52+40E L23+00N 52+60E L23+00N 52+80E L23+00N 53+00E

L22+50N 51+00E L22r50N 51+20E L22+50N 51+40E L22+50N 51+60E L22+50N 51+80E

L22~50N 52+00E L22+50N 52+20E L22+50N 52+40E L22+50N 52+60E L22750N 52+80E

L22+50N 53+00E STANDARD AU-S

. V6A 1 R 6 PIiONE(604)253-3158 FAX(604)253-1716

'IPICATE le # 94-1777 Page 2 I20 7N4

Au* --

9 2 5 2 4

5 17 5

20 4

7 4 3 5 3

2 2 2 5 11

6 4 4 4 4

150 -..

- SAMPLE TYPE: P 1 ROCK P 2 S O I L AU' ANALYSIS BY ACID LEACH/AA FROn 1 0 GM SAMPLE. Samles beginnins 'RE' are duplicate samples. L9

DATE RECEIVED: JUN 22 1594 DATE REPORT HAILED:

- - - - - - - - -

SIGNED BY. . . . . . . . . . .D.TOYE, C.LEONG, J.UANG; CERTIF IED 0.C. ASSAYERS c. 1c-1

Page 28: Geological and Geochemic .f FfiPPtPd:t

Appendix I1

Rock Geochemical Results

Page 29: Geological and Geochemic .f FfiPPtPd:t

~

ACKa ANALYTICAL LABORATORIES LTD. 852 E. BASTINGS ST. VANCOUVER

GEOCHEMICAL ANALYSIS 0 . Belik & Assoc. Ltd. PROJECT 1062

1815 N o r t h R i v e r D r i v e , Kamloq __ -

SAMPLE# -

RE MAC #19

STANDARD AU-R

- 1.C. V6A 1R6 PBONE(604)253-3158 FAX(604)253-1716-

:RT IF I CATE QQ F i l e d 94-1652 Page 2 BC V2B 7h4

_.___ . _ _ __ .-

480 17 3 1 23 12

18 25 11 6 9

9 5 4 16

3

3 4 4 5

3 3

750 17

7

69 4 3 4 2

- SAMPLE TYPE: P 1 TO P 3 ROCK P 4 S O I L AU* ANALYSIS BY ACID LEACHIAA FRO# 10 GM SAMPLE. SamDleS beainninq 'RE' are duplicate sameles.

DATE RECEIVED: JUN 1 3 1 5 9 4 DATE REPORT MAILED: .D.TOYE, C.LEONG, J.UANG; CERTIF IED B.C. ASSAYERS

Page 30: Geological and Geochemic .f FfiPPtPd:t

SAMPLE # Au* Dub

RE MAC #37 MAC #38

Sample type: ROCK. Samples becrinnina 'RE' are duplicate samples.

4 3 4 2 3

MAC 39

MAC 41 STANDARD AU-R MAC 140

5 7 7

470

Page 31: Geological and Geochemic .f FfiPPtPd:t

.~ ACME ANALYTICAL LABORATORIES LTD. 852 E. BASTINGS ST. VANCOUVER B.C. V6A lR6 PHONE(604)253-3158 FAX(604)253-1716

ASSAY CERTIFICATE G . B e l i k h Assoc. Ltd. PROJECT 1062 File t 94-1777 Page 1

SAMPLE* IAu** 1815 horth R i v e r Drive, Ksrnloops BC V2B 7Nk

94MAC-42 .OOl 94MAc-43 .OOl 94MAc-44 .001 94MAc-45 .OOl 94MAC-4 6 .OOl

94MAc-47 .OOl 94MAC-48 .OOl 94MAc-49 .OOl 94MAC-50 .OOl 94MAC-51 .001

94MAC-52 .001 94MAc-53 RE 94MAc-53 94MAc-54 94MAc-55 .OOl

94MAC-56 94MAc-57 STANDARD AU-1

AU" BY F I R E ASSAY FROn 1 A.T. SAWPLE. - SAHPLE TYPE: P 1 ROCK P 2 SOIL

DATE RECEIVED: JUN 22 1994 DATE REPORT . .D.TOYE, C.LEONG, J.YANG; CERTIFIED B.C. ASSAYERS

Page 32: Geological and Geochemic .f FfiPPtPd:t

.p ANALYTICAL LABORATORIES LTD. 852 E. EASTINGS ST. VANCOW

GEOCHEMICAL ANALYSIl

G. Belik h Assoa. Ltd. PROJECT 101 1815 North River Drive. K a n

___ SAMPLE# I I

< B.C. V6A lR6 PEONE(604)253-3158 F111(604)253-1716w

CERTIFICATE # 1 File # 94-2140 Page 1

Au*

bs BC V2E 7W4 _. -

9 4 m c - 5 a 94MAc-59 94MAC-60 94MAC-61 RE 94MAC-61

- SAMPLE TYPE: P1 ROCK P 2 TO P 4 SOIL Sanwles k s i r n i n s 'RE' are duplicate sanwles.

AU* ANALYSIS BY ACID L E A C H I M FRCU 1 0 GM SAMPLE.

DATE RECEIVED: JUL 1 9 1994 DATE REPORT MAILED:

5 9 4 9 4

Page 33: Geological and Geochemic .f FfiPPtPd:t

94G0R-225 94GBR-247 94G0R-248 94GBR-249 94G0R-250

9460R-254 94GBR-254 dup.

94GBR-255 946011-256 9460R-257 9460R-258 94GBR-259

94G0R-260 PCGBR-261 94GBR-262 94G0R-263 9460R-264

94G0R-265 RE 94GBR-265 94GBR-266 94GBR-267 94GBR-268

94G0R-269 94G0kZZO 94MAC-0627

~ 94MAC-063 . STANDARD C/AU-R

BORATORIES LTD. 852 E. HRSTINGS ST. VANCOUVER B.C. V6A 1R6 PBONE(604)253-3158 PAX(604)253-1716

GEOCHEMICAL ANALYSIS CERTIFICATE G. Belik h Assoc. Ltd. PROJECT 1061 F i l e # 94-2790 Page 1

1815 h r f h River Drive, Kmloops BC VZB 7W4

lo Cu Pb Zn Ag N i Co Hn Fe As U AU Th Sr Cd Sb B i V Ca P La C r Us 08 T i 0 At Na K u A@* m mmppnppnmmm %ppnppnppnmmmmmm x x m p p n xppn % m % % xppn Pca

3 4621 24 50 4.2 9 6 961 2.41 2 <5 <2 6 74 1.6 4 23 144 1.26 .047 8 10 .36 124 .09 3 .45 .05 .48 1 19 3 14 2 54 .2 52 18 932 3.02 2 <5 <2 3 70 <.2 <2 <2 49 9.45 .OD8 <2 8 6.40 5<.01 ~2 .03 .01 .01 3 7 3 6 <2 71 <.l 73 24 1234 3.77 <2 8 <2 4 114 .2 <2 <2 26 12.89 .007 <2 6 7.29 8<.01 <2 .05 .01<.01 2 5 4 15 14 20 .6 10 4 274 1.48 18 7 <2 <2 7 <.2 3 3 29 .33 .015 <2 31 .39 15 .02 <2 .49 .01 .04 1 89 1 17 7 71 .4 20 10 1138 3.74 4 <5 <2 <2 ZOO <.2 <2 <2 17 2.53 ,067 7 10 .SO 214<.01 2 .44 .02 .24 4 10

2 29 4 24 c.1 23 9 857 2.99 9 <5 c2 c2 72 c.2 3 g2 12 l.U .018 2 13 .15 148<.01 2 .24 .03 .06 <1 10 !2 16 2198 47 7.3 13 7 314 3.15 130 <5 <2 2 82 .3 5 40 66 1.95 .842 60 10 .37 42 .01 5 .24 .09 .34 1 35 4 156 12 83 .5 ‘16 15 1099 4.74 15 4 <2 3 75 .3 <2 <2 93 2.61 .076 7 13 .66 219 .01 3 .26 .04 .24 4 59 i8 12655 265 238 16.0 6 8 1838 3.14 5 <5 <2 4 296 12.4 4 51 93 3.82 .037 11 3 .51 94 .02 3 .15 .05 .23 4 22 1 57 8 49 .2 17 2 210 .76 7 14 <2 <2 28 .2 5 <2 4 .61 .014 <2 11 .19 16<.01 2 .03<.01 .02 c1 6

4 15 3 7 .1 20 2 153 .60 8 16 <2 <2 19 <.2 4 <2 3 .34 .004 <2 17 .12 12C.01 2 .03<.01 .01 4 6 1 11 8 3 .2 9 1 151 .52 2 11 <2 <2 23 <.2 4 <2 ~2 .52 .003 <2 11 .18 9<.01 <2 .01<.01 . O l 3 4 2 8 6 63 .2 44 3 314 .96 55 <5 <2 <2 148 .2 3 <2 5 2.28 .011 <2 23 1.51 15<.01 c2 .05<.01 .04 2 2 3 10 <2 18 .2 38 2 361 1.41 15 12 <2 <2 34 <.2 9 <2 10 .79 .023 c2 15 .27 40<.01 2 .08<.01 .04 1 7 1 10 <2 7 .1 16 2 195 .85 4 11 <2 c2 42 <.2 4 <2 3 .93 .016 ‘2 10 .26 9<.01 <2 .04<.01 .02 4 5

:1 119 4 57 .3 727 41 1104 4.84 <2 4 <2 5 386 <.2 ‘2 3 97 8.61 .062 3 776 7.62 79 .01 2 1.06 .04 .01 2 6 ;1 23 5 68 <.l 714 38 1415 4.90 2 <5 <2 4 350 <.2 ‘2 ‘2 65 7.67 ,076 4 548 7.19 76 .01 3 1.23 .04 . l o 1 5 1 26 399 10 14.4 33 3 268 .86 21 7 <2 ‘2 187 c.2 3 2 3 1.67 .002 <2 22 1.17 18<.01 <2 .04<.01 .03 3 1850 1 864 1860 50 35.0 207 18 527 2.35 129 <5 4 c2 382 .4 7 8 7 3.23 .005 <2 40 3.87 44c.01 <2 .09c.01 .07 1 4298 2 189 815 19 57.2 116 8 414 1.35 89 <5 3 ‘2 241 .2 5 3 6 2.45 .008 <2 37 2.16 34<.01 <2 .08<.01 .06 2 6353

4 32 50 53 .5 387 28 1055 3.99 69 <5 <2 ‘2 520 .2 2 <2 16 4.18 .037 <2 70 4.33 98<.01 2 .23<.01 .14 1 27 3 30 49 52 .5 386 28 1042 3.94 68 <5 <2 2 516 .2 2 <2 16 4.16 .036 2 69 4.29 95<.01 2 .23<.01 .15 c1 26 2 190 760 14 66.9 54 4 316 .99 33 5 5 <2 206 .3 5 3 4 1.89 ,002 <2 23 1.18 30<.01 2 .04<.01 .04 5 10879 2 939 2350 35 31.6 72 23 86 1.88 36 9 2 c2 17 .2 10 39 2 .15 .002 <2 12 .06 12c.01 ~2 .01<.01<.01 1 1532 3 75 59 92 1.4 546 27 940 4.44 142 <5 <2 3 528 .4 2 2 20 5.69 .061 3 64 5.93 106<.01 3 .34 .01 .15 1 112

4 20 8 15 .5 16 4 70 1.56 14 8 <2 2 43 <.2 11 <2 16 .14 .019 2 20 .06 79c.01 <2 .37<.01 .13 4 21 2 65 79 7 3.7 20 3 146 .56 5 6 <2 <2 42 <.2 4 <2 2 .37.015 ~2 14 .12 1 8 ~ 0 1 2 .02<.01.01 4 342

18 69 21 8 .4 9 1 103 1.28 2 11 <2 c2 12 <.2 4 <2 14 .10 .008 <2 7 .02 15 .01 ~2 .12 .01 .02 1 8 !9 31 <2 47 .2 17 2 2641.84 3 4 <2 3 47 <,2 3 ‘2 91 .46.041 4 31 .24 53.10 <2 .91 .10.19 4 3 19 57 38 128 6.6 68 32 1093 4.01 40 23 6 37 53 16.6 15 23 61 .51 .092 40 58 .92 188 .08 34 1.81 .07 .16 10 467

I C P - .500 GRAM SAMPLE IS DIGESTED W I T H 3ML 3-1-2 HCL-HNO3-H2O AT 95 DEG. C FOR ONE HOUR AN0 IS DILUTED TO 10 ML WITH UATER. T H I S LEACH IS PARTIAL FOR MN FE SR CA P LA CR HG 0A T I 0 W AND LIMITED FOR NA K AND AL. ASSAY REWMENDED FOR ROCK AND CORE SAMPLES IF CU PB ZN AS > 1%. AG , 30 PPM & AU > 1000 PP0

~ SAMPLE TYPE: P l ROCK P2 SILT P3 SOIL AU** ANALYSIS BY FA/ICP FROM 10 GM SAMPLE. S a d e s besinning ‘RE’ a r e dupl icate samles.

DATE RECEIVED: AUG 23 1994 DATE REPORT MAILED: O.TOYE, C.LEDNG, J.UANG; CERTIFIEO 0.C. ASSAYERS

Page 34: Geological and Geochemic .f FfiPPtPd:t

- A C h Z ANRLY

Q4t ~. - SAMPLEY

94GBR-98 94GBR-99 94GBR-100 94GBR-101 94GBR-102 I 94GBR-103 94GBR-104 94GBR-105 94GBR-106 94GBR-107

RE 946811-107 94GBR - 108 94GBR-109 94GBR- 110 94GBR-111

94GBR-112 94GBR-113 94GBR-114 94GBR-115 94GBR-116

94CBR- 117 94GBR-118 94GBR-119 94CBR-120 94GBR-121

94GBR- 122 94GBR-123 94GBR- 124 94GBR-125 94CBR- 126

94CBR- 127 94GBR- 128 94GBR-129 94GBR- 130 94CBR-131

STANDARD C/AU-R

......... ._ ....... - .... . . . . . . .... :CAL LABORATORIES LTD. 8 5 2 E. BASTINGS ST. VANCOUVER B . C . V 6 A 1R6 P H O N E ( 6 0 4 ) 2 5 3 - 3 1 5 8 F A X ( 6 0 4 ) 2 5 3 - 1 7 16--.'

QQ GEOCHEMICAL ANALYSIS CERTIFICATE

G. Belik & Assoc. Ltd. PROJECT 1061 File # 94-1588 Page 1 1815 North River Drive, Kamloops BC V2B 7N4

. ..... ...... - -. . -. ...... . .- - Mo Cu Pb Zn Ag N i Co Mn Fe As U Ad I n S r Cd Sb B i V Ca P La C r Mg Ba T i B A l Na K U At.*

5 21 9 58 6 8 9 9

6 46 19 68

47 20 1 15 1 98 1 8 8

4 92

<1 92 2 90

22 130 1 117 1 155

2 210 1 97 4 46

< l 104 1 67

1 96 1 58 2 40 1 97 2 52

5 30 3 58 2 10 2 16 9 32

9 15 3 9

21 122 3 7 8 7

<2 3 <.l 3 2 53 <.l 26 3 52 .1 46 2 61 c.1 29

<2 53 <.l 40

12 173 1.2 23 62 6 .4 5 ~. ~ ~

5 25 .1 166 7 42 <.l 64 3 37 .1 85

4 37 .l 85 4 22 <.l 64 5 48 .1 197 3 45 c.1 84 4 37 .1 28

6 28 .3 57 5 25 .1 50 6 40 c.1 19 3 15 g.1 143 5 58 e.1 21

4 28 c.1 63 6 33 g.1 23 6 31 .1 35 7 61 .1 122

13 12 <.l 9

32 26 <.l 7 18 154 .1 25 32 35 <.l 4 28 11 .1 4 27 52 .2 5

42 60 .1 22 14 2 .2 5 18 118 .3 66 25 5 .2 5 64 2 1.0 4

1 106 .42 4 460 1.26 6 279 1.88 5 568 .97 6 255 1.14

3 363 2.67 2 178 .8i . . . . . . .

31 354 5.26 26 499 4.69 30 425 5.38

30 418 5.32 19 314 4.99 40 327 6.77 34 559 5.16 21 347 4.51

34 297 6.48 27 341 5.39

8 398 5.13 34 241 5.18 9 558 5.71

28 383 4.74 7 363 4.39

11 456 3.82 31 483 5.51 14 170 1.77

7 89 6.57 9 196 10.74 3 24 2.01

10 46 2.72 10 179 7.99

31 120 6.28 3 14 1.41 7 152 10.41 2 35 2.27

4 19 2.97

<2 8

<2 5 4

4 <2

2 2

<2

2 3

<2 c2 <2

<2 2

<2 2 3

<2 <2 2 2

19

43 34 31 16 74

47 21 52 42 44

L1

<2 3 g.2 <2 86 .5 2 81 .3

<2 136 .7 <2 90 .2

3 34 1.0 <2 60 <.2 <2 9 .2 <2 8 .3 <2 10 '4

<2 10 <.2 *2 10 <.2 <2 14 .4 <2 10 .2 <2 11 <.2

<2 11 .2 <2 23 .3 <2 21 <.2 <2 15 <.2 <2 12 .2

<2 5 .3 <2 5 .3 <2 6 <.2 <2 7 <.2 9 229 <.2

13 45 <.2 12 308 .8 11 81 <.2 8 93 <.2

10 78 <.2

18 65 .2 13 16 <.2 10 30 .5 3 10 <.2 2 13 <.2

<2 <2 c2 <2 <2 <2

<2 <2

<2 <2 <2

<2 <2 <2 c2

<2 <2 <2 <2 <2

<2 <2 <2 <2 c2

c2 <2 <2 2

<2

2 <2 <2 2 4

2 <2 .02 ,001 <2 31 1.19 .047 . . <I 59 1.51 .082 <2 25 1.20 .085 2 17 1.88 .061

<2 73 .23 .043 2 12 1.67 .008

<2 78 .69 ,033 <2 132 .46 .030 <2 100 .69 .030

<2 99 .67 .030 <2 114 .30 ,034 <2 132 .49 ,048 <2 119 .71 .034 ~2 125 .61 .043

<2 146 .44 .030 <2 59 1.24 .035 <2 104 .68 .039 <2 55 .69 .032 <2 161 .08 .034

<2 158 .30 .034 <2 122 .24 .029 <2 147 .25 .033 <2 99 .83 .032 <2 5 1.69 .068

<2 18 .14 .072 <2 37 .20 ,151 <2 5 .38 .069 <2 5 .61 .064 <2 20 .90 .084

<2 34 .60 .125 2 3 .01 .039

<2 34 .15 .121 <2 <2 .10 .017 4 <2 .01 ,009

c2 5 .02 12 <.Ol . . . . . . . . . <2 .08 .02 .01 3 4 17 .27 52 .06 6 .57 .03 .12 1 9 28 .41 83 .10 <2 .92 .09 .21 1

11 23 .36 64 .07 3 .72 .03 .08 2 5 14 .10 22 .07 185 .39 .01 .01 1

6 18 .64 90 .03 <2 16 -25 10 .01

5 1.21 .02 .19 4 . . . 2 .24 . O i .01 2 .

<2 362 1.97 46 .17 <2 1.51 .02 .14 1 <2 152 2.56 134 .19 2 1.95 .02 .61 1 <2 172 2.25 17 .17 <2 1.74 .03 .04 1

<2 170 2.22 17 .17 ~2 157 2.24 56 .26 <2 316 2.31 83 .20 <2 114 2.65 59 .22 <2 57 1.79 55 .24

<2 92 1.49 58 .23 '2 a2 1.20 17 .it. <2 103 2.60 24 .33 <2 152 .@4 79 .16 2 157 3.86 66 .28

<2 1.74 .03 .03 1 <2 1.58 .03 .28 1 <2 2.07 .03 .30 1 <2 1.79 .03 .30 1 <2 1.93 .05 .77 <1

<2 1.81 .07 .78 4 <2 .96 .03 .05 1 <2 2.07 .04 .08 <1 <2 .96 .06 .32 4 <2 2.85 . O l .17 -4

<2 114 2.46 102 .21 <2 1.79 .03 .66 1 <2 133 2.34 111 .25 C2 1.71 .02 .41 1 <2 173 2.74 97 .28 <2 1.86 .02 .61 2 <2 174 2.29 97 .19 <2 1.50 .02 .44 <1 23 4 . l o 91 <.Ol 2 .31 .02 .24 1

27 2 .63 29 .15

12 3 .42 77 <.Ol <2 .76 .05 .15 4 16 28 .31 129 .09 <2 .79 .03 .22 4 20 5 .03 81 .01 2 .25 .03 .18 2 10 2 .02 84 <.Ol 2 .28 .01 .20 1

<2 1.02 .01 .ll 1

42 4 1.06 36 <.Ol <2 1.60 .02 .16 <1 34 4 .01 128 <.Ol 2 .29 .01 .29 4 21 22 .25 95 .04 <2 1.12 . O l .18 -4 10 5 .01 187 <.Ol 2 .20 .03 .10 2 9 5 <.Ol 227 <.Ol 2 .18 .03 .ll 1

12 7 3 2 3

6 5 2 3 4

2 1 3 4 3

2 2 2 3 3

2 1 2 2

12

15 5 4

10 10

5 4 6 9

46

18 58 38 125 6.7 72 29 1017 3.96 . . . . . 35 49 17.5 13 21 61 .49 .090 38 53 .88 179 .08 33 1.88 .05 .14 13 470

ICP - .500 GRAM SAMPLE IS DIGESTED UlTH 3HL 3-1-2 HCL-HN03-H20 A T 95 DEG. C FOR ONE HWR AND IS DlLUTEb TO 10 HL W I T H WATER. T H I S LEACH IS PARTIAL FOR MN FE SR CA P LA CR MG BA T I B U AN0 LIMITED FOR NA K AN0 AL. ASSAY RECOMMENDED FOR ROCK AND CORE SAMPLES IF cu PB ZN AS > 1%. AG > 30 PPH a AU > 1000 PPB - SAMPLE TYPE: P1 TO P2 ROCK P3 SILT AU* ANALYSIS BY ACID LEACWAA FROM 10 GM SAMPLE. Samples beqinning 'RE' are duol icate samles. I I7 /?

DATE RECEIVED: JUN 7 1994 DATE REPORT MAILED: f.0 /?#' SIGNED B Y . & C ' ~ y ~ . O . T O Y E . C.LEONC, J.UANG; CERTIF IED B.C. ASSAYERS

- - - - - - _ _

Page 35: Geological and Geochemic .f FfiPPtPd:t

Appendix I11

Statement of Expenditures

Page 36: Geological and Geochemic .f FfiPPtPd:t

Statement of Expenditures

Mac Claims, 1994

1. Labour:

G. Belik, M.Sc., P.Geo. -preparation; May 1&3, 1994 1.0 days -field work; May 30, June 8-10,

13-14,20, July 12, Aug. 15, 1994 8.0 days

-base maps; Nov. 11,14,15/1994 2.0 days -report; January 16-17, 1995 2.0 days

13.0 days @ $360/day $4,680.00

J. Belik, Assistant

July 12, Aug. 15, Sept.5, 1994

9.0 days @ $140/day 1,260.00

-May30, June 6-10, 13-14,20,

Expenses and Disbursements:

a) Geochemical Analyses $1,891.16 b) Truck Rental & operating

Expenses 770.00 c) Drafting 542.00 d) Field Supplies 100.00 e) Freight & Misc. Items 100.00

Report Preparation:

-Xerox, Map Prints, Binding, Secretarial

Sub T t

$ 5,940.00

3,403.16

150.00

1 $ 9,493.16

plus 7% G.S.T. paid on above fees and 664.52 disbursements

Total $10,157.68

Page 37: Geological and Geochemic .f FfiPPtPd:t

Appendix IV

Writer's Certificate

Page 38: Geological and Geochemic .f FfiPPtPd:t

GARY D. 8 E L l K . MSC. ,~.Geo. Consulting Geologist Mineral Exploration

1815 North River Drive, Kamloops, B.C. V2B 7N4 376 8351 /-

CERTIFICATE

I, GARY D. BELIK, OF THE CITY OF KAMLOOPS, BRITISH COLUMBIA, DO HEREBY CERTIFY THAT:

(1). I am employed as a geologist by G. Belik and Associates, located at 1815 North River Drive, Kamloops, B.C.

( 2 ) . I am a fellow of the Geological Association of Canada and a member of the Association of Professional Engi- neers and Geoscientists of British Columbia.

I (3). I am a graduate of the University of British Columbia with a B.Sc. in Geology (Honours) and M.Sc. in Geology.

I (4). I have practised continuously as a geologist since May, 1970.

( 5 ) . The geological and geochemical survey discussed in this report were carried out by me or under my direct super- vision.

January 17, 1995 KAMLOOPS, B. C.

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