and windjammer power and gas ltd. - ontario · ling programme completed on the briscoe-bryce gold...

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41P89NEee46 63.3987 BRYCE 010

DIAMOND DRILL REPORT

BRISCOE-BRYCE GOLD PROSPECT

BRYCE TOWNSHIP, ONTARIO

1981

for

Yvanex Developments Limited

and

Windjammer Power and Gas Ltd.

Toronto, Ontario, February, 1982.

W. E. Brereton, P.Eng., MPH Consulting Limited.

m SUMMARY

A gold exploration programme involving 4,489 ft. of diamond dril-

I ling in 13 holes has been completed on a 1,320 acre property in

Bryce Township, northeastern Ontario, for Windjammer Power and Gas

l Ltd. and Yvanex Developments Limited.

The claims encompass the former Briscoe-Bryce No. l Vein Zone gold

l prospect which saw limited production in the I960 1 s. The rock

that was milled reportedly graded in the 0.5 to 0.6 oz Au per ton

l range. The gold occurs in quartz-pyrite-chalcopyrite vein

m material within a steeply dipping shear structure which is appro

ximately conformable with host intermediate volcaniclastics. The

l shear is a strong, through-going feature which has been defined

over a strike length in excess of 850 m by the previous and pre-

I sent drilling and is open in both directions and to depth.

Pre-1940 surface trenching indicated three surface oreshoots as

l follows:

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Oreshoot Length (ft) Width (ft) Grade (02 Au)

A 135 4.0 0.29

B 165 1.6 0.373

C 80 3.0 0.194

The 1981 drilling was carried out east of the old workings in a

previously relatively unexplored area. The grades in the 1981

drilling in this eastern sector are, in general, significantly

better than grades in the previous drilling under the old surface

workings.

Vein intersections on the No. l Vein Zone are summarized

following:

Hole No.

1

2

3

4

5

11

12A

13

Collar

1+OOE, 0+50S

2+OOE, 0+50S

3+08E, 0+25S

4+OOE, 0+1 5S

5+OOE, 0+25S

6+OOE, 0+80S

7+OOE, 0+40S

8+OOE, 0+40S

Intersection oz Au/ True Width (ft)

0.11 over 1.0 ft

0.41 over 3.2 ft

0.80 over 1.0 ft

0.73 Au, 0.56 Ag

Q.44% Cu over 1.6 ft

0.20 over 3.8 ft

0.05 over 1.7 ft

0.055 over 1.0 ft

Vertical Depth

200

243

145

129

99

247

248

0.155 over 3.5 ft (#2 vein) 236 0.27 over 0.8 ft (#1 vein) 269

The No. l or "main" vein shows a distinct stratigraphic control

being located in a chloritic tuffaceous unit in the basal portion

of a feldspar porphyritic crystal tuff which in turn is located

between two thick units of coarse intermediate volcanic breccia.

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Gold values are closely restricted to a narrow, generally central,

quartz-sulphide vein within the shear. These high grade sections

often assay more than l oz Au per ton. Subordinate veins on

either side or sections of mineralized shear material generally do

not carry gold values.

Four holes were drilled elsewhere on the property to test geo

physical targets. No gold intersections of potential economic

significance were recorded. These holes were technically success

ful, however, in that the cause of the geophysical anomalies has

been explained in every case.

Several old trenches excavated by previous workers were located

and re-sampled. The trenches invariably expose quartz-pyrites

chalcopyrite vein material in chloritic shear zones. The veins

are generally very narrow and irregular. Values of up to 0.30 oz

Au per ton were recorded in selected grab samples. More syste

matic chip samples across vein structures returned low values.

Although none of the trench areas appear to have any immediate

economic significance, they do emphasize the widespread distri

bution of gold mineralization in the property area.

It is concluded that the No. l Vein Zone has potential to host an

economic tonnage of gold-bearing rock. The area between present

sections 0+00 and 5+OOmE is of greatest interest based on the work

to date. Potential grades of 0.20 oz Au per ton over mining

widths of 5 ft. are indicated.

A programme of additional diamond drilling totalling 7,100 ft is

recommended to further develop the economic potential of the No. l

Vein Zone with a minor amount of footage devoted to testing two

other geophysical targets on the property.

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41P89NEW46 63.3967 BRYCE 010C

TABLE OF

PAGE

SUMMARY

1.0 INTRODUCTION l

2.0 HISTORY AND PREVIOUS WORK 2

3 . O PROPERTY 6

4.0 LOCATION, ACCESS AND INFRASTRUCTURE 8

5.0 DIAMOND DRILLING PROGRAMME - 1981 115.1 Drilling 115.2 Assaying 125.3 Other 13

6 . O GEOLOGY 146.1 General 146.2 Mineralization 16

7.0 DESCRIPTION OF PROPERTY GOLD OCCURRENCES 197.1 Contact Zone 19

7.1.1 Sampling - 1980 207.2 Briscoe-Bryce No. l Vein Zone 22

7.2.1 Sampling - 1980 24

8.0 DRILL RESULTS - 1981 268.1 Summary 268.2 Holes 1-5, 10-13; No. l Vein Zone 29

8.2.1 Lithology and Stratigraphy 298.2.2 Ore Microscopy 368.2.3 Discussion 37

8.3 Holes 6 to 9, Geophysical Targets 388.4 Trench Re-Sampling 41

9.0 CONCLUSIONS AND RECOMMENDATIONS 44

CERTIFICATE

REFERENCES

APPENDIX A - Assay Results - 1981 APPENDIX B - Drill Logs: Holes 81-1 to 81-13 APPENDIX C - Drill Sections: Holes 81-1 to 81-13 APPENDIX D - Photomicrographs

l lm l .O INTRODUCTION

l This report presents a summary of the results of a diamond dril

ling programme completed on the Briscoe-Bryce gold prospect in the

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Kirkland Lake area of northeastern Ontario during 1981 on behalf

of Yvanex Developments Ltd. and Windjammer Power and Gas Ltd.

l The drilling was concentrated on the so-called "No. l Vein Zone".

This gold-bearing vein saw limited production approximately (100

l tons) in the I960 1 s. The rock that was milled reportedly graded

m in the 0.5 to 0.6 oz Au per ton range. The gold occurs in quartz-

sulphide vein material within a steeply dipping shear structure

l which is conformable with host intermediate pyroclastics.

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Results of exploration completed both by previous workers and

within the context of the present programme prior to the 1981

drilling are presented following in summary fashion.

lThis report describes the drilling programme carried out, outlines

exploration results to date and presents recommendations for fur-

I ther exploration in the property area.

Expenditure details re OMEP programme OM81-6JV-7 are presented

under separate cover.

11l1111111111111111

*2.0 HISTORY AND PREVIOUS WORK

Previous trenching on the No. 1 Vein Zone indicated

oreshoots as follows (Moorhouse, 1941):

Oreshoot Length (ft) Width (ft)

A 135 4.0

B 165 1.6

C 80 3.0

2

three surface

Grade (oz Au)

0.29

0,373

0.194

These surface zones are located between present baseline co

ordinates 0*25mW to l-*-25mE (Map 3c).

A total of approximately 6,000 ft. of various sizes

drill coring has been carried out on the No. 1 Vein

1930 and 1975 by previous workers including Noranda

Mining Projects of Canada Ltd., Briscoe-Bryce Mines

Mining and Exploration Ltd. and the Rip Van Winkel

All of the drilling was carried out between present

to 4+OOmE with the large majority between 0+SOmW to

3c).

The previous drilling established the continuity to

the host shear zone and gold-bearing vein material.

of diamond

Zone between

Mines Ltd.,

Ltd., Trihope

Syndicate.

lines H-50mW

1+SOmE (Map

depth of both

All of this

l lm drilling has been relatively shallow with vein intersections

generally in the range of 50 to 100 ft (15 to 30 ra) vertically

l below surface.

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Previous drilling between 0+SOmW to O+TSmE established that the

mineralized structure here continues to depth with generally low

gold values present. The best value recorded was 0.53 o z Au per

l ton over 0.3 m (previous hole MP-6, Map 3c).

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Drilling immediately to the east of the above returned higher gold

values and substantially increased amounts of vein material within

the shear structure. The zone appears to dip approximately 75 e S

l in this region relative to a more vertical dip in the area of the

headframe. A previous hole in the vicinity of present line 1+OOmE

" returned 0.22 oz Au per ton over 1.0 meters (Noranda hole N-l).

B Another hole immediately to the east returned a 5.5 m section of

shearing and vein material with one section averaging 0.06 oz Au

l over 1.95 m. Contained within this was a 0.3 m section which

returned 0.32 oz Au per ton.

l A previous hole on the vein at present 2*75mE intersected a 0.8 m

section which returned 0.51 oz Au. A hole 60 m east of the above

g intersected the vein and returned an assay of 0.15 oz Au over

. 0.8 m.

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llm Other known and reported gold prospects within the present pro

perty include the Contact Zone, South Zone/ J.R. Campbell occur-

I rences and the H. Briscoe Jr. (Honeymoon Lake) occurrence.

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A 1980 programme completed on behalf of Windjammer-Yvanex con

sisted of geological reconnaissance and surface trenching and

sampling along with a programme of linecutting and ground geo-

I physical surveying (magnetics, VLF-EM, Induced Polarization).

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The 1980 trenching and sampling on the No. l Vein generally con

firmed previously indicated gold tenors. A systematic chip sample

in the shaft beneath the headframe on the previous "C" zone re-

I turned 0.414 oz Au per ton over 0.7 m. Six selected grab samples

returned 0.270, 0.184, 0.149, 0.254 and 0.02 oz Au per ton. A

l

3216 Ib bulk sample taken from the shaft by previous operators

reportedly averaged 0.38 oz Au, 1.10 oz Ag per ton.

l A 3.0 m chip sample taken in 1980 across a trench in the previous

"A" surface zone returned 0.204 oz Au per ton. A chip sample

B across a 0.3 m massive pyrite band in the trench returned 1.04 oz

U Au. A 2.6 m sample across the vein in the existing shaft in the

"A" zone returned 0.270 oz Au per ton. A previous 1990 Ib bulk

l sample from the shaft reportedly averaged 0.76 oz Au per ton.

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Geophysically, there is a complex and very low amplitude IP res

ponse locally associated with the No. l Vein Zone. The PFE (per-

I cent frequency effect) signature improves to the east and to

depth. The host shear zone appears on some lines as a distinct

l anomaly in the IP resistivity data. The anomaly is indicative of

m a vertical source which extends to depth. There is a flanking

VLF-EM response associated with part of the No. l Vein Zone.

l There is no magnetic signature associated with the No. l Vein.

m Induced Polarization surveying over the Contact Zone to the north

M o f the No. l Vein Zone indicates a strong resistivity-PFE anomaly.

This zone represents the contact between Catherine Group basalts

l to the north and Skead Group volcaniclastics to the south. The IP

anomalies probably relate to pyrite-chalcopyrite mineralization

known to be present in the interflow sedimentary Contact Zone.

B There is a strong VLF response along the Contact Zone. Previous

drilling encountered low Au values.

lIt was concluded that results of the above exploration were suf-

ficiently encouraging to warrant an aggressive diamond drill

l evaluation of the property. A programme of 2500 ft of N-size dia

mond drilling in 9 holes, which subsequently became 4500 ft in 13

l holes, was therefore recommended with drilling to commence in

early April of 1981. The above drilling was completed and is the

" subject of this report.

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3.O PROPERTY

The property on which exploration work was completed consists of

20 patented and unpatented mining claims and one half-lot in Bryce

Township, District of Timiskaming, Larder Lake Mining Division as

follows:

Claim No. T 25691 T 25692 T 25693 T 25694 T 25695 T 25696 T 25697 T 24227 T 24228 T 24229 L 578257 L 578261 L 578263 L 578264 L 578265 L 578266 L 579216 L 579217 L 579215 L 579218 North Half

NENWNENWSWNESESWSESENWNWSWNESESWNWSWNWNE

1/41/41/41/41/21/41/41/41/41/41/41/41/41/41/41/41/41/41/41/2

Lot 9

LocationNNNNNNNNNNSSSSSsNNSS

Con

1/21/21/21/21/21/21/21/21/21/21/21/21/21/21/21/21/21/21/21/2. 4

LotLotLotLotLotLotLotLotLotLotLotLotLotLotLotLotLotLotLotLot

1010111111121210111011121212121112121010

Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.Con.

44444444444444444444

StatusPatentedPatentedPatentedPatentedPatentedPatentedPatentedPatentedPatentedPatented

UnpatentedUnpatentedUnpatentedUnpatentedUnpatentedUnpatentedUnpatentedUnpatentedUnpatentedUnpatented

Patented

Surface rights are also held to patented claim T 24227.

The following nine claims are also held under option by Wind

jammer -Yvane x but were not worked on in the context of the present

programme:

l l l l l l l l l l l l l l l l

L 579219 L 579220 L 579221 L 579222 L 579223 L 579224 L 579225 L 585682 L 585683

NW 1/4 SE 1/4 SW 1/4 NW 1/4 NE 1/4 NW 1/4 SW 1/4 NE 1/4 SE 1/4

S 1/2 Lot S 1/2 Lot S 1/2 Lot S 1/2 Lot S 1/2 Lot N 1/2 Lot N 1/2 Lot S 1/2 Lot S 1/2 Lot

9 Con. 10 Con.9 Con.

12 Con. 12 Con.11 Con.12 Con. 9 Con. 9 Con.

444333344

Unpatented Unpatented Unpatented Unpatented Unpatented Unpatented Unpatented Unpatented Unpatented

8

4.0 LOCATION, ACCESS AND INFRASTRUCTURE

The property is located some 30 miles (50 km) south of Kirkland

Lake in northeastern Ontario (Figure 1).

It is readily accessible via Highway 560 which leads to Charlton

from the TransCanada Highway, No. 11, at Englehart, Ontario. Con

cession roads and finally a bush road lead directly to the pro

perty from the end of Highway 560.

The one mile bush road to the property was constructed by former

operators and is best traversed by 4-wheel drive or all-terrain

vehicle.

Bush roads also lead into adjoining Tudhope Township from High

way 65, 4 miles south of the property at Leeville. Hydro

electric power and a spur-line of the Ontario Northland Railway

are located at Leeville. There is also hydro-electric power

transmission to the Hills Lake fish hatchery less than 5 miles by

road to the east.

lMiners and general labour are available from surrounding centres

l of service and supply such as Kirkland Lake, Elk Lake, Matachewan,

Earlton, Haileybury and Cobalt.

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REGIONAL LOCATION MAP

ONTARIO

-.-.-IV...

PROPERTY LOCATION

U.S.A.

SCALE100 O tOO

1-17,000,000BOO 800 TOO

•d-L-Aai KILOMETRES

MATACHEWAN

ELK LAK

GOWGANDA NOTRE-DAME-OU-NORD

SHININGTREE PROPERTY v LISKEA LOCATION HAILEYBU

DETAILED LOCATION MAPSCALE 1 11,600,00020 O 80 40 60

KILOMETRES

YVANEX- WINDJAMMER J.V.

PROPERTY LOCATIONFroJtctN* C-409

FIGURE l

WE. BREBETON60S LIMITED

Os't FEB. I98Z

M PH Consulting Limited

l l j The closest gold mills potentially available at present for custom

milling are at Kirkland Lake (Macassa Division, Willroy Mines Ltd.

l - 40 miles by road via highways 573, 11 and 66) and at Virginia-

town (Kerr Addison Mines Ltd. - 50 miles by road via highways 624

and 66).

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115.0 DIAMOND DRILLING PROGRAMME - 1981

l 5.1 Drilling

Drilling operations were carried out by Barron Diamond Dril

ling Ltd. of Haileybury, Ontario.

A total of 4,489 ft. of NQ drilling was completed in 14

l holes. One of the holes, No. 12, was lost in overburden and

had to be re-drilled as hole 12A so that a total of 13 holes

l was actually completed.

Core recovery was, in general, excellent. Recovery was poor

l in isolated instances where the rocks were heavily fractured

and sheared. Recovery in the No. l Vein Zone was very good.

l A few instances of locally poor recovery are a reflection of

open cavities in the vein rather than actual loss of core.

All drilling was carried out with a Longyear 38 machine sup

ported by a small tractor.

Drilling operations were completed in the period April 9 to

July 9, 1981.

Drill core is presently being stored in core racks in a cabin

I X on the property.

l lM The drilling programme was managed by MPH Consulting Limited

of Toronto on behalf of Windjammer and Yvanex.

l5.2 Assaying

l All assaying and analytical work was carried out by Swastika

m Laboratories Limited of Swastika, Ontario.

l Gold and silver determinations were made by fire assay tech

niques. Copper, along with occasional Pb and Zn, were deter-

I mined by atomic absorption.

Intersections of vein material were sampled in very short

l lengths, generally l ft. Such samples were completely pul

verized in the laboratory and two cuts taken for fire assay.

l

This minimized the effects of any erratic coarse gold and

provided for very uniform and representative assay results.

l Any core sections which appeared to have any Au potential

were split and assayed.

B Unused sample material has been collected from Swastika and

is being stored for possible future use.

lThe entire assay results for the 1981 programme are presented

l as Appendix A.

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13

5.3 Other

A minor progranune of trench re-sampling and geological recon-

l naissance was carried out in conjunction with the drilling.

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14

6.O GEOLOGY

6.1 General

The property straddles the boundary between the Catherine

j Group and the Skead Group of earliest Precambrian (Archean)

mm metavolcanics. The Catherine Group is comprised of Mg-rich

and Fe-rich tholeiitic basalt flows with Fe-rich tholeiites

l predominating at the top of the group.

l The Skead Group consists mainly of massive calc-alkaline vol-

M canic fragmental rocks of basalt, andesite, dacite and rhyo-

lite composition. Some flows are present in the group. The

l fragmental rocks range from crystal tuff to tuff-breccia and

flow breccia. The coarser fragmental rocks contain a wide

l variety of felsic fragments. The main source of the volcanic

M ejecta appears to have been a large volcanic centre in Skead

Township to the north of the present property area. Recent

l government mapping has defined an additional volcanic centre

in the vicinity of Heather Lake immediately south of the

l present ground.

The contact between these two formations, the "Contact Zone"

l of previous workers, crosses the property in the vicinity of

detail baseline 4+OON. Present and previous work on the

l "Contact Zone" indicates that there is a major unit of inter-

l

l

l l j flow metasediments consisting of laminated cherty and

tuffaceous rocks containing pyrite and chalcopyrite sepa-

I rating the two formations.

m Porphyry and lamprophyre dykes intrude the volcanic rocks.

m An elliptical stock of feldspar porphyry containing several

gold veins is centered 2 miles east of the property. Another

l porphyry body located by recent government mapping occurs on

the west portion of the present property immediately south of

l Honeymoon Lake.

The Round Lake granitic batholith occurs directly north of

l the property area.

B Rock units on the property strike east-northeast and are

B steeply to vertically dipping. There is no evidence of any

fold closures in the immediate property area. Stratigraphic

l tops in the area are indicated to be to the southeast.

B The property is located between two major regional faults

H striking N40 0W, the Cross Lake Fault and the Montreal River

Fault. A study of the fracture pattern in Bryce Township in-

I dicates 3 prominent fracture directions; northwest, northeast

to east-northeast and north-south. A major northeast-

H trending airphotographic linear herein termed the "Sunday

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16

Creek Linear" passes to the south of the property. These

fractures are important in that most of the gold minera

lization recognized to date in the area is controlled

by one of the above fracture directions, e.g. the Briscoe-

Bryce No. l Vein Zone along an east-northeast structure.

6.2 Mineralization

A 1941 Ontario Department of Mines report describes 34 gold

prospects in the Bryce-Robillard area (Moorhouse, 1941).

This author classified the more important gold occurrences

into a number of types according to structure and minera

lization as follows:

a) mineralized shear zones

b) mineralized porphyries

c) mineralized joints and shear zones in granite

The first group consists of deposits that occur ins

1) northeast-trending zones? (2) north-south zones and

3) northwest-trending zones. In the northeast-trending

zones, three types were recognized, i) those mineralized

with disseminated pyrite and other sulphides with quartz,

ii) those mineralized with massive pyrite * quartz and

iii) those mineralized with pyrite accompanied by chrome,

mica, and quartz.

17

The Briscoe-Bryce No. l Vein Zone would be an excellent

example of a mineralized shear zone of type ii).

There is an additional and very important type of gold occur

rence in the area, namely gold associated with laminated in

terflow sedimentary horizons consisting of cherty and tuf

faceous material containing stratiform laminae and dis

seminations and stringers of pyrite and chalcopyrite. These

units are typically sheared and show varying degrees of seri

citization, carbonatization and chloritization. This variety

would be analogous to Moorhouse's "mineralized shear zones of

type a-1". The Contact Zone on the Briscoe-Bryce property

and reported occurrences on the J.R. Campbell property would

be of this type. Much of the ore from some of the world's

major gold deposits such as Amoco's Detour deposit and the

Dome Mine at Timmins is or will be derived from orebodies of

this type.

The only serious attempt at commercial gold production in the

area was from the Briscoe-Bryce No. l Vein Zone. There are

no accurate records of the work but, according to Harold

Briscoe Sr., a total of approximately 100 tons of ore was

milled in a 60-75 ton per day mill installed on the property

in the mid 1960"s. The rock milled was taken from the dec

line and No. l and No. 2 shafts on the "A" and "C" zones res-

l lm pectively. Average grade of the mill feed is reported to

have been in the 0.5 to 0.6 oz per ton range. The operation

l appears to have been relatively crude. In any event, the

mill burned down in 1967 "before steady production had been

l achieved".

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7.0 DESCRIPTION OF PROPERTY GOLD OCCURRENCES

There are several known and reported gold occurrences within the

confines of the present property area, the most important of which

are discussed following:

7.1 Contact Zone

During the early stages of prospecting in Bryce and Tudhope

Townships in the 1930's, considerable work was expended in

attempting to trench and sample a pyritic, carbonatized,

sericitized, silicified, sheared band of tuffaceous sedi

ments which occurs at the contact between the Catherine and

Skead Groups. This contact was apparently only exposed by

trenching in two locations along a strike length of over 3

miles. One of these trench localities was on claim T 25697,

now part of the property described herein. This so-called

"Bailey T-trench" was excavated in the 1930's and reportedly

returned 0.114 oz per ton Au across a width of 60 ft.

Five short holes were drilled in the T-trench area in 1939.

There were no Au values in the core above 0.02 oz per ton

although sludge samples reportedly returned up to 8 oz Au per

ton.

20

In 1967, two diamond drill holes were drilled 2100 ft. west-

southwest of Bailey's T-trench for Trihope Mining and

Exploration Co. to investigate a VLP-EM conductor on the

"Contact Zone". Although no ore values were reported, the

drilling did intersect bands of interflow tuffaceous and

cherty sediments with pyrite and up to ^ chalcopyrite.

In 1975, the Rip Van Winkel Syndicate investigated the zone

in the immediate area of the old Bailey Trench with a total

of 328.6 ft in two diamond drill holes. Both holes inter

sected the silicified, sericitized, pyritized "Contact Zone"

which varied in width from 13.3 ft. (Hole 1) to 30 ft. (Hole

2). Assay results were "disappointing" with the best value

being 0.03 oz Au over 10 ft.

7.1.1 Sampling - 1980

The Bailey T-trench was located during the 1980 explo

ration programme. An attempt to completely excavate

the old trench with a backhoe was only partially suc

cessful.

A portion of the actual contact zone was exposed im

mediately north of an old, cribbed, water-filled shaft

at the T-junction in the trench. All quartz *

21

sulphide mineralization was blasted and sampled.

There were no gold values of economic significance in

any of the samples with the highest value of 0.03 oz

Au per ton being from a thin massive pyrite band im

mediately adjoining the old shaft. It is probable

that the best mineralization is present at the bottom

of the shaft. This could not be sampled during the

present work as this area of the trench was beyond the

reach of the backhoe.

An additional trench to the north that reached bedrock

likewise failed to return any values of significance.

Although disappointingly low in an economic sense, the

values are in accord with previous drill results and

indicate that this interflow unit is distinctly ano

malous geochemically in gold. Such a unit may have

acted as a source rock or protore for subsequent gold

concentrations in favourable structures elsewhere

along this auriferous sulphidic unit.

The original assay value of 0.114 oz Au over 60 ft in

the Bailey T-trench must be totally discounted. If

real, it is possible that the value represented a sur-

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face enrichment not representative of the underlying

bedrock.

7.2 Briscoe-Bryce No. l Vein Zone

l The original showing was found by the Briscoe Brothers by

m trenching through clay after they had found mineralized auri

ferous float along the old wagon road in this vicinity in

l 1935. Between 1935 and 1957 much laborious trenching was

done between the present two shafts and eastward by hand,

l horse-drawn scoop or scraper and by drilling and blasting.

m Most of these old trenches reportedly never reached bedrock.

An eastward sloping, 40" decline was sunk at the west end of

l the surface workings (headframe - Map 3c) and a vertical

shaft was sunk and timbered to a depth of 32 ft. toward the

east end of the surface workings, above present hole 81-1.

In his 1941 report, Moorhouse notes that

"......after trenching had exposed the mineralized zonein some 15 pits...sampling indicated an ore shoot 450 ft. long and 3 to 4 ft. wide, averaging 0.20 to 0.28 ounces of gold per ton."

Subsequent workers determined that the surface zone,(between

present 0*25mW and 1+251HE on Map 3c), consisted of 3 indi-

vidual "oreshoots" as follows:

23

"A" Oreshoot - This was exposed on surface for a length of

135 ft. It is reported as averaging 0.29 oz Au per ton over

an average width of 4.0 ft. Mining Projects of Canada Ltd.

subsequently extended this oreshoot an additional 185 ft. to

the east by diamond drilling. Gold values in the drill-

M indicated extension are low being in the 0.04 to 0.06 oz per

ton range. Harold Briscoe Sr. showed the author assay

B results which indicated that a 1990 Ib bulk sample from the

shaft in the "A" zone returned 0.76 oz Au per ton and

B D.40% Cu. There was no silver assay performed.

"B" Oreshoot - This is located immediately west of "A" and is

l reported to average 0.373 oz gold per ton across an average

width of 1.6 ft. for a length of 165 ft.

lB "C" Oreshoot - This is reported as grading 0.194 oz Au per

ton across an average width of 3.0 ft. for a length of 80 ft.

B based on surface sampling. There is an approximately 60 ft.

section of "very low-grade material" separating the "B" and

l "C" oreshoots. A 3216 Ib bulk sample taken from the shaft in

m the "C" oreshoot returned 0.38 oz Au and 1.10 oz Ag per ton

according to old assay results. Additionally, it is reported

l that virtually every round in the decline exposed visible

gold.

l

l

l

l lm 7 .2.1 Sampling - 1980

Considerable difficulty was encountered in reaching

l bedrock with a backhoe in the vicinity of the pre

viously reported "A", "B" and "C" oreshoots. Clay

l

overburden in these areas is deeper than 15 ft., the

maximum penetration capability of the backhoe.

l Sampling at the top of the now filled-in #1 shaft

beneath the headframe appears to confirm previously

l indicated gold tenors. A 0.7 m chip sample across the

m vein exposed on the west wall of the shaft returned

0.414 oz Au per ton. Four selected grab samples re-

I turned 0.270, 0.184, 0.149 and 0.254 oz Au per ton.

Two massive pyrite grab samples from the decline re-

I turned Au values in the 0.02 oz range.

Sampling in the area of the No. 2 shaft on the "A"

l oreshoot (line 1+OOmE) returned the most encouragement

of the programme to date. A 3.0 m chip sample on the

B east wall of trench #5 on the vein at line 1+OOmE

B returned a weighted average of 0.204 oz per ton Au. A

2.6 m chip sample across the west face of the No. 2

l shaft returned a weighted average of 0.270 oz per ton

Au.

l

l

l lm Examination of selected grab sample values from within

the zone strongly suggested that the average grade in

l a bulk sample would be higher, possibly substantially

so, than the previous values. For example, in the

l above trench, the central 1.0 m chip sample returned

m only 0.002 oz Au yet a grab sample, #5, from within

this zone returned 0.63 oz Au per ton. Likewise, the

l northernmost chip sample returned 0.002 oz across

0.5 m yet two grab samples from within this zone

l returned 0.72 oz Au and 1.04 oz Au per ton respec-

m tively. The latter value represents a sample across a

0.3 m massive pyrite pod on the west side of the

l trench.

l Several old trenches excavated by previous workers were

j located and re-sampled during the 1981 drill programme.

The trenches invariably expose quartz-pyrite

l j- chalcopyrite vein material in chloritic shear zones.

The veins are generally very narrow and irregular.

B Values of up to 0.30 oz Au were recorded in selected

B grab samples. More systematic chip samples across the

vein structures returned low values. Although none of

l the trench areas appear to have any immediate economic

significance, they do emphasize the widespread distri-

bution of gold mineralization in the property area.

l

l

11

1 1 1 1 1 1 1 1 1 11 1 11111

t26

8.0 DRILL RESULTS - 1981

8.1 Summary

The 1981 drilling on the No. 1 Vein Zone in combination with

previous work has established that the vein extends from at

least 0+SOmW to 8+OOmE, a distance of 850 meters (2800 ft.).

The vein is open in both directions and to depth.

The present drilling was carried out on 100 m centres east of

the old surface workings towards a previously unexplored

area. The grades in the 1981 drilling in this eastern sector

are, in general, significantly better than grades in the

previous drilling under the old workings.

Drill results on the No. 1 Vein Zone are summarized

following:

Hole No. Collar (m) Intersection oz Au/ VerticalTrue Width (ft) Depth (ft)

1 1+OOE, 0+50S 0.11 over 1.0 ft 200

2 2+OOE, 0+50S 0.41 over 3.2 ft 243

3 3+08E, 0+25S 0.80 over 1.0 ft 145

4 4+OOE, 04-15S 0.73 Au, 0.56 Ag 129Q.44% Cu over 1.6 ft

5 5+OOE, 0+25S 0.20 over 3.8 ft 99

* 10 4+50E, 1+50S see below

11 6+OOE, 0+80S 0.05 over 1.7 ft 247

27

12 abandoned in overburden

12A 7+OOE, 0+40S 0.55 over 1.0 ft 248

13 8+OOE, 0+40S 0.155 over 3.5 ft 236(#2 vein)

0.27 over 0.8 ft 269 (#1 vein)

*It appears that Hole 10 did not intersect the No. l Vein

Zone. A narrow quartz-pyrite vein was intersected at the ap

proximate projected location of the vein at depth. A 1.0 ft

section returned 0.03 oz Au. Completion of subsequent Holes

11, 12 and 13, however, indicate that this is not the main

vein. It is therefore concluded that the dip of the main

vein steepens to vertical or, possibly to steep north at

depth in this region.

The No. l Vein Zone consists of narrow quartz-pyrite j^ chal

copyrite vein(s) occupying a strong shear structure in inter

mediate volcaniclastics. Individual veins are conformable

with the shearing which is in turn conformable with the host

rock units. Maximum width of gold-bearing vein material to

date is approximately 4 ft. Minimum width is l ft.

The No. l Vein Zone shows a distinct stratigraphic control,

being located in a chloritic tuffaceous unit in the basal

portion of an intermediate, ashy feldspar porphyritic vol-

ll 28

B caniclastic which is in turn located between two thick units

of coarse intermediate fragmental.

lGold values are closely restricted to a narrow, generally

l

central, quartz-sulphide vein within the shear i These high-

grade sections often assay more than l oz per ton Au.

l Subordinate veins on either side or sections of mineralized

shear material generally do not carry gold values.

j Carbonitization is ubiquitous within the shear along with

variable silicification, pyritization and sericitization.

l There may be some green chromian mica. The zone of shearing

and hydrothermal alteration may be up to 10 ft. or more in

B width.

lGold values generally show a 1:1 correlation with copper

l values. Textural relationships indicate that the Au-Ag-Cu

mineralization may be paragenetically later than the quartz-

pyrite mineralization.

lThere is minor sphalerite and galena within the vein zone.

lg The easternmost hole, 113, intersected a second Au vein iden-

tical to, but stratigraphically above the No. l Vein.

l

l

29

Further drilling will be required to delimit the two vein

structures.

Four holes were drilled elsewhere on the property to test

geophysical targets. No gold intersections of potential eco

nomic significance were recorded. These holes were techni

cally successful, however, in that the cause of the

geophysical anomalies has been adequately explained in every

case.

Logs and sections for the 1981 drilling are presented as

Appendices B and C respectively. Hole locations are shown on

Map 2c.

8.2 Holes 1-5, 10-13? No. l Vein Zone

8.2.1 Lithology and Stratigraphy

Diamond drilling during 1981 in the interval between

section 1+OOmE to 8+OOmE has defined a relatively con-

sistent volcaniclastic stratigraphic picture as out-

H lined (Appendix C).

lThe gold-bearing No. l Vein Zone is generally loca-

I lized within a chloritic to dacitic tuffaceous unit at

the base of an intermediate crystal tuff which in turn

l

l

ll 30

is sandwiched between two units of coarse intermediate

* volcanic breccia.

lThe host chloritic tuff is generally a grey to

l greenish-grey, fine-grained rock with greenish chlori-

. tic clots. The unit may be very similar to the over-

lying crystal tuff but missing the characteristic

l feldspar phenocrysts and crystal fragments. In

hole l, the upper contact of the chloritic tuff with

l the overlying crystal tuff is gradational while the

m lower contact with underlying coarse intermediate vol

canic breccia is sharp.

lThe chloritic tuff is well-bedded in hole 3 suggesting

l a waterlain origin for the rock. The chloritic tuff

m has also been the locus of a major shear zone, which

is in turn host to the No. l Vein, such that original

l textural structural features in the tuff have been

largely obliterated. The chloritic tuff varies from

l approximately l m to 5 m in true thickness.

The overlying unit of feldspar porphyritic crystal

l tuff is a generally massive, featureless ash tuff of

probable andesitic composition. An ash flow origin is

l

l

l l. suggested by the lack of internal organization or

structure in the unit.

lThe crystal tuff, in core/ consists of white plagio-

g clase crystals and darker green chloritic clots in a

chloritic matrix. There are scattered quartz eyes.

The rock is typically weakly carbonitized where tested

l with HC1. There may be local traces of pyrite on

slip/fracture surfaces, in veinlets with quartz-

I carbonate and as fine disseminations.

A weak schistosity may be present in the rock which

l appears to be grossly parallel to lithologic

contacts.

la* The tuff is variably fractured with the fractures

filled by one or more generations of quartz, carbonate

l

l

l

^ hematite.

There are occasional block-sized fragments of fine

grained, greyish dacitic volcanic within the tuff.

l Material identical to this crystal tuff forms an ashy

matrix to the overlying and underlying volcanic brec-

I cia units.

l

l

32

Where the determination can be made, the tuff varies

from 10 m (hole 13) to in excess of 60 m (hole 2) in

thickness. There is a general thinning of the unit to

the east which may be a reflection of initial deposi

tion on an irregular, pre-existing volcanic topo

graphy, possibly coupled with a volcanic source area

to the west.

Units of andesitic volcanic breccia, typically feld

spar porphyritic, overlie and underlie the proceeding

units of finer volcaniclastic material.

The overlying breccia unit was variously described as

a coarse andesitic fragmental, coarse fragmental

dacite, etc. in field logs. It consists of fragments

locally to 0.5 m or more of several types of feldspar

porphyry, dacitic and andesitic tuffs and fine-grained

dacitic volcanic in a feldspar porphyritic (andesitic)

crystal ash tuff matrix.

The rock is generally greenish-grey and may display a

crude parallelism of the major plane of rock clasts.

Rock fragments are typically angular to surrounded.

There are local traces of pyrite, often with quartz *

33

carbonate veinlets. The rock generally displays weak,

pervasive carbonatization.

The rounding of the fragments and lack of internal

organization is again an indication of a chaotic

debris or avalanche-flow type of deposit. There were

no obvious clast size gradations to suggest a trans

port direction. The coarseness of the rock suggests a

relatively proximal deposit. Its thickness is inde

terminate but, considering hole 10, is at least

locally greater than 50 m.

The coarse fragmental unit underlying the No. l Vein

Zone is essentially as that described above, i.e. a

coarse, intermediate, pyroclastic volcanic breccia

with a variable component of feldspar porphyritic

clasts. There may be minor pyrite and

quartz-carbonate veining.

The contact of this unit with the overlying tuffaceous

section may be very sharp, indicating a discrete

hiatus in volaniclastic deposition.

The No. l Vein Zone is expressed at surface as a well-

laminated quartz-pyrite-chalcopyrite vein(s) within a

34

zone of strong shearing up to 10 ft (3 m) or more in

width within intermediate tuff. There is an obvious

intense greenish chloritization associated with the

shearing.

In core, the No. l or "Main" Vein Zone consists of a

zone of strong shearing with associated chloriti

zation, carbonitization, silicification, sericiti

zation and pyritization along with some development of

probable fuschitic mica. There is variable chalco

pyrite within the vein material. As in the surface

exposures, the vein material is distinctly laminated

parallel to schistosity with alternating quartz (±

carbonate) and sulphide-rich bands or zones. Pyrite-

rich bands are typically 1-5 cm in width. The pyrite

is often of a medium-grained, granular aspect

and, in hole l, appears to float in fine, clear to

whitish quartz.

In this hole, minor chalcopyrite is present as fine

splashes in quartz and is generally separate from the

main pyrite zones. In hole 2, chalcopyrite fills

cracks and vugs in quartz.

35

It was often noted that individual pyrite-rich bands

are surrounded by narrow (l cm *) bleached alteration

halos. An intense light greenish sericite-fuschite(?)

-silica alteration also accompanies the vein material

in several holes, e.g. 5A.

There is minor sphalerite in the vein zone in hole 4.

The most easterly holes show an intense chert-like

silicification associated with the quartz-pyrite-

chalcopyrite vein material.

The vein zone intersections vary in width from less

than l m to approximately 3 m (hole 4). Not all of

the vein material carries Au values however. These

are typically closely restricted to a narrow, often

central section of the vein zone. Assay values here

are often in excess of l oz Au per ton. Detailed

assay data are presented on the drill logs with higher

values summarized in the proceeding section.

Drilling revealed the presence of two virtually iden

tical Au-bearing vein zones in hole 13. The present

interpretation indicates that the deeper of the two

corresponds to the No. l Vein. This would require

36

that the host structure has possibly "stepped-down"

" stratigraphy here or that an additional unit of coarse

B fragmental has appeared. This interpretation is

tentative and more drilling will be required for

l corroboration.

8.2.2 Ore Microscopy

l A total of 5 polished sections was cut from the No. l

Vein Zone, 3 from hole 2 and l each from holes 4

and 5, to assist in determining the nature of gold

occurrence, grain size, overall vein mineralogy, etc.

Vein mineralogy in the sections examined is extremely

simple, consisting of dominant pyrite with subordinate

l to nil chalcopyrite in mainly siliceous gangue.

Pyrite occurs as a mosaic of relatively coarse, inter-

I locking anhedral grains and as scattered grains or ag

gregates which typically show better developed crystal

l outlines. The pyrite typically shows evidence

m o f brittle fracture in the form of cracked and shat

tered grains and masses. There has been local dis-

I location of shattered fragments.

l

l

l

l l 37

Chalcopyrite, in amounts from l to 10%, occurs as

interstitial fillings between pyrite grains, as fil-

fl lings of cracks within pyrite, as rims on pyrite

grains and as discrete masses and blebs in siliceous

l gangue separate from pyrite.

' Three polished sections were cut in the vicinity of

l 341 ft. in hole 2. Six discrete grains of gold were

observed. These ranged in size from 15 to 100 mic-

J rons. The gold is very clearly associated with the

chalcopyrite occurring as discrete, angular grains

within the latter mineral. Appendix D presents

photomicrographs of gold grains from hole 2.

There was little or no chalcopyrite present in the

polished sections for holes 4 and 5. There was also

no gold observed.

There was no indication of a discrete silver phase.

l This element is probably associated with the gold as

m electrum.

l 8.2.3 Discussion

The microscopic information supports the megascopic

l conclusion that the Cu-Au-Ag mineralization, in its

l

l

l l l

l

l l

38

present form, is distinctly later than quartz-pyrite.

H Whether this truly represents a discrete, later stage

of Cu-Au-Ag mineralization or a re-distribution of

l existing elements during a metamorphic or defor-

mational event is uncertain. In any event, increased

Cu tenors should be directly associated with Au-Ag

B concentrations so that Cu may be a very valuable path

finder in further exploration.

l 8.3 Holes 6 to 9, Geophysical Targets

' None of the four holes drilled on Induced Polarization j^

l resistivity * VLF-EM targets away from the No. l Vein Zone

returned any gold intersections of significance.

l The holes are summarized as follows!

Hole No. Collar Target

6 2+50W, 2+20S strong IP-resistivity m feature

CommentslExtensive shearing in several zones accounts for the resis

tivity anomaly; there is sufficient disseminated pyrite to

explain IP. Twenty-four sections of mineralized core were

l l l l l

l l l l l

39

submitted for assay. Values ranged from nil to 0.002 oz Au

per ton with one value of 0.005 oz Au per ton.

Hole No. Collar Target

7 0+50W, 4+40S strong VLF anomalyin area of "South Zone" reported Au

l showing

Comments

l The VLF anomaly is due to a strong, 10 ft wide fault zone.

There is no significant mineralization in the hole. Eight

l samples of weakly mineralized rock were submitted for assay.

B Values ranged from nil to 0.002 oz Au per ton? five of the Cu

values are anomalous being in the 100 to 4300 ppm range. The

l Cu is present in hole 7 as very thin chalcopyrite-quartz-

carbonate veinlets.

lB Hole No. Collar Target

" 8 11+OOW, 5+25S IP target in vicinityof reported quartz-

I pyrite Au veins

Comments

Hole intersected numerous thin quartz-carb-py-cpy veinlets in

intermediate pyroclastics in explanation of IP effects; 10

sections of mineralized core were sent for assay; values

40

ranged from nil to 0.005 oz per ton Au with up to 1530 ppm

' Cu.

lHole No. Collar Target

l

l

l

5+OOW, 3+85N strong VLF-IP targeton Contact Zone

Comments

Hole intersected two interflow sedimentary units aggregating

28 ft core length with up to 25% pyrite in explanation of

VLF-IP anomalies? 11 samples submitted for assay returned

l negligible values (to 0.005 oz Au); Ag values ranged up to

0.04 oz which is geochemically anomalous; Cu values ranged up

l to 1530 ppm.

A polished section was cut from a very narrow intersection of

l heavy sulphide mineralization in the Contact Zone in hole 9.

Mineralogy consisted of pyrite-sphalerite-chalcopyrite in

B siliceous gangue. Pyrite forms scattered, often equant

B grains and appears to have crystallized early. Sphalerite

forms a narrow veinlet which transects the slide. Chalco-

I pyrite occurs mainly as small irregular blebs within spha-

lerite. Tiny rounded to elongate chalcopyrite blebs are dis-

' tinctly aligned along sphalerite crystallographic direction

l in some areas and appear to represent exsolution phenomena.

l

l

41

A small gold grain approximately 25 microns across was iden

tified within sphalerite (Appendix E).

8.4 Trench Re-Sampling

Previous surface workings in the form of old trenches and

pits were systematically located and sampled during the

course of the drilling.

Samples of quartzose vein material in old trenches at 3+25S

on line 2+0OW returned values of nil to 0.03 oz Au and trace

to 0.03 oz Ag per ton. These values are not considered sig

nificant.

Three samples of vein material from a trench at 3+65S, 1+OOW

all returned 0.01 oz Au and trace to 0.02 oz Ag. No further

work is warranted here.

A total of 14 selected grab samples was collected from an

irregular, narrow (6 inch), quartz vein zone containing

pyrite-chalcopyrite in an old trench at 44-755, 8+OOW. The

vein dips vertically and strikes approximately 070". Seven

of the samples returned Au values in the 0.15 to 0.30 oz per

ton range with nil to 0.04 oz Ag and up to 1530 ppm Au. A

6 ft chip sample straddling the vein across unmineralized

wallrock returned nil Au, Ag, 48 ppm Cu. These gold values

l l 42

attest to the widespread occurrence of gold mineralization on

B the property. They also underscore the distinct localization

M of gold values within the quartz-sulphide veins. However,

this particular occurrence is felt to be too narrow and gold

l distribution too irregular relative to the values obtained to

be of any immediate economic interest.

B Four selected grab samples were taken from an old trench near

4+47S, line 12+OOW. The trench exposes narrow quartz-

I pyrite-chalcopyrite veins in intermediate tuff. The veins

strike 070" and dip 80 0 N. Sample results were as follows:

Sample No. o z Au oz Ag ppm Cul

14937 0.01 0.47 9670

14938 0.10 0.38 11000(1. U)

14940 0.18 0.25 5180

H A 3 ft systematic chip sample across the mineralized zone

returned 0.005 oz Au, 0.13 oz Ag and 1260 ppm Cu.

l Gold values are therefore highly localized and this occur-

rence does not warrant any further action at this time.

lTwo samples from an old trench at 1+5 OS on line 14+OOW

l returned 0.05 oz Au, 0.16 oz Ag, 9300 ppm Cu and 0.19 oz Au,

l l 43

0.27 oz Ag and 11300 ppm (1.131;) Cu. The occurrence is

similar to the previous, i.e. very narrow and irregular zones

l of quartz-pyrite-chalcopyrite vein material. This occurrence

is not deemed to have any immediate economic potential.

l. The two foregoing occurrences are an indication of increased

gold tenors in the general Honeymoon Lake area and suggest

l that further exploration should be carried out in this

region.

l

l

l

l

l

l

l

l

l

l

l

l

l l l

l

44

9.0 CONCLUSIONS AND RECOMMENDATIONS

l The No. l Vein Zone is economically the most significant gold

occurrence on the property.

m The No. l Vein is a classic example of a so-called hydrothermal,

structurally-controlled epigenetic vein deposit. Examination of

l the vein indicates that the present quartz-sulphide mineralization

is a result of both the replacement of chloritic shear material

and open space filling. Abundant rusty vugs containing small

quartz crystals attest to the latter style of mineralization.

l There are typically some secondary structural features which con

trol the exact deposition of orebodies within the main fault or

l shear zone in deposits of this type elsewhere in the world. In

m some cases, oreshoots occupy fault intersection; others are in

open zones where the fault has changed attitude or formed

l branches, loop structures and feather joints. In other places,

ore is deposited when the fault crosses a contact between dif-

H fering rock types. Ore may also be deposited preferentially in

l one rock unit that has anomalous mechanical properties, such as

the ability to fracture more readily, relative to the surrounding

l strata.

l\

l

l

l l 45

In the case of the No. l Vein, it appears that there is a distinct

stratigraphic control to the vein material and host shear struc-

I ture, namely within a particular chloritic tuff unit at the

base of a feldspar porphyritic volcaniclastic unit. This may

l reflect on the genesis of the mineralization in that the present

vein may represent remobilization of a syngenetic auriferous

' interflow sediment during a hydrothermal /def ormat ional event in

l the area.

l Compilation and examination of previous work indicates that the

m No. l Vein Zone consists of two parallel structures in the west

" which merge to form a single vein zone in the area between lines

l 0+SOmE and 1+OOmE. The best widths and Au values to date are in

the vicinity of this junction, namely at the No. 2 shaft - No. 5

l trench area. The vein then appears to continue to the east as a

single structure which is wider and/or richer than the sub-veins

to the west.

lResults in hole 13 indicate that a second vein has appeared in the

J east. The potential junction area of these veins is located bet-

g ween present sections 7+OOE and 8+OOE. A concentration of vein

material may be present at this postulated junction.

lThe Britcana feldspar porphyry intrusive is located immediately to

l the northeast of the property. Favourable structural sites for

l l 46

gold deposition may have been created in the general area where

" the No. l Vein Zone intersects the intrusive, i.e. in the extreme

l northeast portion of the property.

J Exploration results to date on the No. l Vein Zone have been ex-

tremely encouraging. There appears to be definite potential for

an economic tonnage of gold-bearing vein material within the

l structure. The most encouragement to date has been in a 500 m

portion of the vein from sections 0+00 to 5+OOmE. Here, based on

l the limited drilling to date, potential is indicated for a tonnage

of vein material averaging approximately 0.20 oz Au per ton with

minor Ag, Cu over a mining width of 5 ft.

lIt is recommended that a programme of diamond drilling be under-

H

l

l

taken primarily to further explore the No. l Vein Zone. This

drilling should take the following form:

l a) No. l Vein Zone Stepout s

Holes should be drilled on 100 meter stepouts to test the

J inferred eastward extension of the vein to the east property

boundary as indicated on Map 2c. It is possible that the vein

' is offset to the south along the "Campbell Fault" between

l sections 12+OOmE and 13+OOmE. This would be determined during

the course of drilling.

l

l l l

47

These holes will probably average approximately 250 ft in

length at -55". A total of eight holes (2000 ft) should be

l budgeted for this drilling.

l l

b) Testing of No. l Vein Zone to Depth

The area between 0+00 and 5+OOmE should be tested to depth in

a series of -55 0 , 750 ft fill-in holes on sections 0+SOmE,

l 1+SOmE, 2+SOmE, 3+SOmE, 4+SOmE and 5+SOmE (6 holes,4500 ft).

This drilling will test the vein at an approximate vertical

l

depth of 500 ft. It may be possible to re-collar in and

deepen previous hole 10.

l Previous hole 81-1 did not intersect the well-developed mine

ralized zone exposed in trench 5 directly above the hole

B at surface (0.2 oz/10 ft). This suggests that this zone, if

B it does extend to depth, may have a plunge which is other than

at 90". This hypothesis will be tested further by the deep

l holes on sections 0+SOmE and 1+SOmE.

lc) Other Targets

B Two 300 ft, -50 0 holes should be drilled to test geophysical

targets remote from the No. l Vein Zone with the holes located

J at 4+lSmS, line 13+OOmE and 4+eOmN, line 10+SOmW (Map 2c).

l

l

l

l lm Total costs for the recommended 7100 ft drill programme should

be a maximum of approximately $284,000.00, inclusive of all

l direct drill costs, supervision, analytical, reporting,

travel, land management, etc.

m Drilling should recover N-size core. Slightly increased

footage costs are more than offset by the larger amount of

l rock recovered and the greater probability of getting core in

badly fractured or vuggy vein zones.

m The subordinate programme of geological mapping and trench

location and re-sampling should be continued to further

l develop a picture of the geological setting of Au minerali

zation in the area. Consideration should be given to ex-

I tending the existing line grid over the remainder of the claim

m group for geophysical/geological control.

l RespedtfuWty submitted,

l

• Toronto, Ontario, W.E. Brereton, P.Eng, January, 1982.

l

l

l

l

CERTIFICATE

I, W.E. Brereton of Toronto, Ontario, hereby certify that:

1) I hold an Honours Bachelor of Science degree in Geology

and Physics from Queen's University at Kingston and a

Master of Science (Applied) degree in Mineral Explo

ration from McGill University in Montreal.

2) I am a Professional Engineer registered with the Asso

ciation of Professional Engineers of the Province of

Ontario.

3) l have practised my profession as a mining explorationist

since 1967.

4) I have based conclusions and reconunendations contained in

this report on my experience and knowledge of the area

and on observations made during the summer and fall of

1981.

W.E. Brereton, P.Eng.

Toronto, Ontario, January, 1982

REFERENCESl1 Johns, G.W., Hoyle, Warren and Good, David. 1981: Precambrian

Geology of the Hill Lake Area, Bryce and Robillard Townships,

I Timiskaming District; Ontario Geological Survey Preliminary Map, p. 2415.

Moorhouse, W.W., 1941: Geology of the Bryce-Robillard Area jji ODM Annual Report, Vol. l, Part 4, 1941.

l

l

l

l

l

l

l

l

lit

l

ll l

o

"HV(S itTAL.. &F

, SOME OF wrtM BEEN.. CULLED

FiuE. TrtE CULUE MATERIAL .....ri Ab.

-f


APPENDIX A

ASSAY RESULTS - 1981

l l l ll ReceivedApri] 16, 1 Q#1

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(brttftaitt nf

Certificate No. 51251 Date: April ?4, 1

Samples of split core

Submitted by M.P.H ^ Consulting Limited, Toronto, Ontari

l Pro-L^C-jLOQ

J2———i-J———————fi—HOU-, i-

SAMPLE NO.

14801

14802 '

14803

14804

14805

14806

14807

14808

GOLD Oz./ton

NIL

0.002

NIL

NIL

0.06

0.11

0.002

0.002

SILVER Oz./ton

NIL

NIL

trace

trace

0.02

0.04

trace

NIL

.ore. W-y

i.a'5-0

^ (H—— \

d . Z.

J. O

A*

Per.G. Lebel, Manager

ESTABLISHED 1928

l

l

l

l Received Apr,


TELEPHONE: (705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

ffl*rtfftrat0 of Analyaia

Certificate No. 51233 Date: JLprJJ, 1Q31

12 Samples of s pi j t. norp

Submitted by M.P.H. Consulting T.-irm't.sd, Topont.n, nnt.ario

(4ile 5L

I

l

l

l

l

l

l

l

l

l

l

l

l

SAMPLE NO.

14309

14310

14313

14314

14315

14316

14317

14313

14319

14320

GOLD Oz./ton

NIL

0.01

0.002

NIL

NIL

0.005

'l!25

^1.34

0.12

0.002

NIL

0.002

NIL

SILVER COPPER Oz./ton PPM

NIL

0.07

trace

trace

0.01

0.01

0.62

0.07

0.01

0.01

0.02

NIL

47

322

10

170

421

35jOO

1730

91

62

146

3

l- 3

l . o 0-5

^ - 3

2.o

i.5 J.o

G. Lebel, ManageESTABLISHED 1 928

l l l l

SWASTIKA LABORATORIES LIMITEDP - Q - B OX 1 0 - SWASTIKA, ONTARIO POK 170

TELEPHONE: (705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Okrtiftrat* iif Analyaia

Certificate No. 51334______________ Date:

Received May 6 1981____ 7_____ Samples of ——

Submitted by M.P.H. Consulting Ltd., Toronto. Ontario

Ma 8 1 Qfil

Split Core

1111111111111

SAMPLE NO.

14856

14857

14858

485914861

14862

14863

GOLD Oz./ton

0.030.002Nil

Nil

Nil

0.002Nil

SILVER Oz./ton

0.03

Nil

0.01

0.005

Nil

0.02Nil

COPPER PPM

184

G. Lebel - ManagerESTABLISHED 1928

l

l l l

Certificate No. ^^^^,-^

l Received May 11/81


TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS* ASSAYERS* CONSULTANTS

i *

Qkrfiftrat? xrf Analysis

51348 Date: May 19 1981

1 Sampled of Split Core

Submitted by M.P.H. Consulting Ltd.. Toronto, Ontario

C-409

l

l

l

l

l

l

l

l

l

l

l

l

l

SAMPLE NO. GOLD SILVER COPPER Oz./ton Oz./ton PPM

14860 0.01 Nil 8500

6. Lebel - Manager

IST-JML- ESTABLISHEO 1 928

11111

^t-thfe, SWASTIKA LABORATORIES LIMITEDlEJBlB^^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO^ Hyypr- TELEPHONE:

ANALYTICAL CHEMISTS *(705) 642-3244

ASSAYERS * CONSULTANTS

(Errtiftralr of AttalysiB

Certificate No. 51 303

Received Apr. 29/81 10 Samples of

Date: May 4 1981

Split Core

Submitted by M. P. H. Consultina Ltd.. Toronto. Ontario

l

1

1

1

1

1

1

1

1

1

1

1

1

1

Acct. No. C-409

SAMPLE NO. GOLD SILVEROz./ton Oz./ton

14821 Nil Nil

14822 Nil Nil

14823 Nil Nil

14824 Nil Nil

14825 Nil Nil

14826 0.02 0.09

14827 0.80 OJ5

14828 0.01 0.01

14829 0.002 Nil

14830 Nil Nil

W/fe. 3

COPPER A f * Jwu i **.^ A 1 p -4A /i T"Tylrt r\ii V.C/l-C V-CTVXI *l / fi \ \y'

39 3.0

44 1 . G

36 l. o

36 '2.*0

34 1*0

818 1.5 1^-^5-5

3980 1 'Z- /^3^- i^^-C*

420 1*0 fyb (^^

46 i . o64 l.O

NOTE: Sample No. 14827 was assayed in replicate. The average 0.80 Oz./tongold was obtained from the following values: Q ^ -,

__ ESTARI IRHFD 195*

0.830.79

1

y /i .

y/ Y /YpAr X s/' yJ(rV\

G. Lebel - Manager

i

11111i1111111111111

,A.K Sil

^^^r

•^•••^ m. m A *^,4^.*"fe m.m*m*±.m^.mmmm*^ m mm mm^fmm^m^

S, SWAS 1 IIVA LAbUKAI UKIbS LIMI 1 tUr p .o. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705)642-3244ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Certificate No. 51324

Received May 5/81

Submitted by

SAMPLE NO

1 48341484914850

* 14851

14851B14852

* 14853

14853B

* 14854

14854B

14855

M. P. H. Consulti

.GOLDOz./ton

Nil0.002Nil0.020.010.010.780.780.060.060.05

0.020.020.020.005

NOTE: * denotes where wholeas requested.

'

(fkriiftrate iif Analysis

Date: May 7 1981

8 Samples of Split Core

ng Ltd., Toronto, Ontario

SILVER COPPER ZINC LEADOz./ton PPM PPM PPM

Nil 480.01 4020.02 — 116000.01 — 1710

0.34 ' — 213

0.05 — — 52

0.02 — 954

0.02 228 1010

sample was pulverized and assayed in duplicate

/i *. *

A fits l \ 0 A t yPer *S\1 l Y*S\fW

6. Lebel - Manager lPRTARI I.QUPfl 1Q9R

1111111111111111111

Vfh^ SWASTIKA LABORATORIES LIMITEDiMllJLJJ^ p-0 - B OX 1 0' SWASTIKA, ONTARIO POK 1TOW^l^ TELEPHONE: (705) 642-3244

ANALYTICAL CHEMISTS *ASSAYERS* CONSULTANTS

Certificate No.

Received Mav 4 1981

Submitted by M. P. H.

SAMPLE

1483114832

* ^ 14833* 14835

* 14836

148371483814839

* 14840

* 14841

14842148431484414845148461484714848

NOTE: *

.

Otertifirate of ,

51317

1 7 Samples

\nal80iB

Date: Mav 7 1981

of Split Core

Consulti no Ltd.. Toronto, Ontario

NO. GOLD SILVEROz./ton Oz./ton

Nil NilNil Nil0.0020.002 0.01Nil 0.01'0.0020.002 Trace0.0020.002Nil NilNil Nil1.33 1.041.350.11 0.080.110.12 0.110.002 0.010.005Nil Nil0.002 Nil0.002 Trace0.002 NilNil Nil0.002 Trace0.005 0.01

Indicates where whole sampleduplicate as requested.

ESTARI ISHEH

COPPERPPM

4846

330980

242

52no

7500

1350

,478

i 72160

506280

410

was pulverized and assayed iny .

Jf 7 IPP*r ^vA Y&W^

G. Lebel - Manager ) ia?ft

1 1 1 1 111 1 1 1 1 1 1 1 1 1 1 1 1

^•ftW SWASTIKA LABORATORIES LIMITED•fipPS^^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO ^^P^ TELEPHONE: (705) 642-3244

ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Ckrtifirate of Analyafa

Certificate No. 51334 Date: May fi 1QR1

Received May 6 1 981 7 Samples of Sp! i t Core

Submitted bv M. P. H. Consulting Ltd.. Toronto

SAMPLE NO. GOLD Oz./ton

14856 0.03 14857 0.002 14858 Nil 14859 Nil 14861 Nil 14862 t 0.002 14863 Nil

'i

FRTARI I RU

. Ontario


0.03 Nil 0.01 184 0.005 Nil 0.02 Nil

JtlLfP*r ^/J * l***\

G. Lebel - Manager ipn iQ9ft

l l l



flferttfirate nf Analysis

Certificate No. 51334 Date: Mav 8

Samples ofl Received May 6 1 981 7

Submitted by M.P.H. Consulting ltd;. Toronto. OntarioSplit Core

l l l l l l l l l l l l l

SAMPLE NO.

14856148571485814859

^148611486214863

GOLD Oi./ton

0.030.002MlMilNil0.002Nil

SILVER COPPER Oz./ton PPM0.03N110.010.005N110.02N11

184

ESTABLISHED 1 928G. Lebel - Manager

bain te&l

1111111111111111111

ST ,MAY2GM

^•fh^ SWASTIKA LABORATORIES LIMITEDjjfcdigifepp^w*ip^

Certificate No.

Received May 15/81

Submitted by M. P. H

SAMPLE

14912

149131491414915148641486514866148671486814869

** 14870

1487114872

**14873

** 14874-

1487514876

1487714878

14879 14880 14881

P.O. BOX 10, SWASTIKA, ONTARIO POK 1TOTELEPHONE: (705)642-3244


Gfcrtifintt? of Analysis

51393 Date: May 22 1981

22 Samples of Ore, Split Core

. Consulting Ltd., Toronto, Ontario

NO. GOLD SILVER COPPER ZINCOz./ton Oz./ton PPM PPM

0.26 0.37 336000.05 0.05 7990.03 0.08 10000.10 0.37 95000.002 Nil — !Nil NilNil NilNil Nil 27Nil Nil 33Nil Nil 13Nil Nil 21Nil Nil Nil

i

0.002 Nil0.002 0.005 ' 211 ;0.002 S0.002 trace 2230.002Nil Nil — 39

Nil Nil

Q! 002 Nil —Nil Nil

Nil Nil — . j 0.005 Nil — if {P tt fl

0.002 Nil ;;r" ^/J t \)jb\G. lebel - Manager \

CCTARI ICUPn 1QOD ,

W V

1 1 111

^•ftW SWASTIKA LABORATORIES LIMITEDjBs&iW^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO W^ipr" TELEPHONE: (705)642-3244


ffi? rtifiratp nf AnalyaiB


Received May 25, 1Q#1 T 0 Samples

Date: Mgy 23, 1Q31

of nrp and split, nnr-A*

Submitted by MPH P.nnsnl t. -i no- Litrrit.Prt. Trvrnnt.n. Pin-hat-in

|

1

1

1

1

1

1

1

1

1

1

1

1

1

SAMPLE NO. GOLDOz./ton

14934 0.005

14935 NIL

14332 NIL

14333 0.002

14334 0.002

14335* 0.002

NIL

14336 0.002

1433? 0.002

14333 0.002

14339 NIL

NOTE: ^Completely

SILVEROz./ton

NIL

NIL

NIL

NIL

0.01

0.01

0.01

0.02

NIL

NIL

pulverized.

PCTARI ICWPr

i

Pro i. 0-A.OQ

COPPERPPM

3

32

163

1930

2100

3000

1920

4300

532

110

... J.tLfG. Lebel, Manager ^

t IQ-JO

1 1 11111111111111111

^Jfh^ SWASTIKA LABORATORIES LIMITED|MBgMfi^^ P.O. BOX 1 0, SWASH K A, ONTAR IO POK 1 TO W *jjpr TELEPHONE: (705)642-3244


Gfertiftrate of Analysis

Certificate No. 51 574

Received June 5 1981

Submitted by M. P. H. Consult!

SAMPLE

149471494814950149511495214953149541495514956149571495814959149601496114962149631496414965

o C 14891JX- 8 f 14897

Date: June 16 1981

20 Samples of

ng Limited, Toronto, Ontario

NO. GOLDOz./ton

NilNilNilNilNilNil0.005NilNil0.060.002Nil0.002NilNilNilNil0.002Nil0.002

F.CTARI 1*

SILVEROz./ton

TraceTraceNilNilNilNil0.13NilNil0.02Nil0.010.04Nil0.01TraceNil0.02NilNil

Per

IMPn 1Q9ft

Ore, Split Core

Att'n: Mr. W. Brereton

COPPERppm

wwv

-----~......1 260

4857

36172

179990

62128117130200460710

k-PhfjA \JJ(G. Lebel - Manager

11111

Certificate No. —^——^-—

Received June l 1981

JUN f f miSWASTIKA LABORATORIES LIMITED

P.O. BOX 10, SWASTIKA, ONTARIO POK 1TOTELEPHONE: (705) 642-3244


Qkrtifirate of

51493 Date: June 8 1981

Samples of Split Core

Submitted by M. P. H. Consulting Ltd., Toronto, Ontario

1111111111111

SAMPLE NO.

148921489314894148951489614898

GOLD Oz./ton

NilNil0.02Nil0.005

0.005

SILVER Oz./ton

0.010.010.01TraceTraceTrace

COPPER PPM

8780 287—

448

ZINC PPM

32


111111111l111111111

^ftfey SWASTIKA LABORATORIES LIMITED^Kjg*l"Ljp^

^•ffisB^ffiipW^IP^


Received June 12, 1931

Submitted by MPH Consul

SAMPLE-

149661496714963149691497014971149721497314974149751497614977149731497914930

P.O. BOX 10, SWASTIKA, ONTARIO POK 1TOTELEPHONE: (705)642-3244


(Errtifirate of AtmlysiB

Date: June 23 T 1931

15 Samples of ore and split core

ting Limited, Toronto, Ontario

Pro.i.C-409

NO. GOLD SILVER COPPEROz./ton Oz./ton PPM

NIL NIL :.i#40.005 0.03 1200

. 0.002 NIL 15300.002 0.03 269NIL trace 420.03 0.01 610.03 0.05 572NIL NIL :690.005 NIL 46NIL NIL 1410.01 0.02 3930.01 trace 400.01 0.03 243NIL NIL 7NIL trace 10

JkrfLfG. Lebel, Manager

FSTARI ISHFn 1Q9R

l

l

JUN o


TELEPHONE: {705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Ok rttfirat* of

* Certificate No. 51624

l Received June 17. 1981

l

Date: June

Samples of split,

Submitted by MPH ..Consulting Limntgri, Tnrnnt.n,

Proj.C-409

SIMPLE NO. GOLD SILVER COPPER Oz./ton Oz./ton

14982*

14983*

14984

14985*

14986

NIL NIL 80

0.05 0.07 7700.05

0.05 O.Q3 572 0.06

0.002 NIL 69

0.05 0.02 3080.05

0.02 0.03 298

NOTE: *V7hole sample pulverized and duplicate assays.

G. Lebel, ManagerESTABLISHED 1 928

1111111111111111111

V-ftW SWASTIKA LABORATORIES LIMITEDjBj^sl^^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO^ ̂ Jtpr T ELEPHONE: (705) 642-3244


(Ekrtiftrat* nf Analyaia

Certificate No. 5172g Date: July 2

Received June 25, 19&1 3 Samples of split core

Submitted by MPH Consulting Limited, Toronto, Ontario

SAMPLE NO. GOLD SILVER COPPEROz./ton Oz./ton PPM

. 14994- 0.05 0.02" 4170.06

14995? 0.005 0.01 5500.005

14996 0.005 NIL 237

NOTE: * Pulverize whole sample.

,^'G. Lebel,

—.. FRTARI I.CMFft 1Q9ft

•IQSl

Manager

11111 111111111 1111 l

.^B^^BW M m m. *^.**r*mm * m i1 A ••fe^MK BB*k MMBM^VkBMBkBBB^Bk B BK m m BBB HB BHk.

ÔTW SWASIIKA LAbUhAIUKItb LIMI 1 bU(SJjiiE^^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO™ 1*P^ TELEPHONE: (705)642-3244



Received June 29, 1981

Cferttfirai

nSubmitted by MPH Consulting Ldmdted.

SAMPLE

14987

. 1498814989

149901499114992

1499314997 14998

1499915000

. — 26405*

26406

NOTE:

NO . GOLD Oz./ton

NIL

.NIL

NIL

NIL

NIL

NIL

NIL

NIL

0.005

0.005

NIL

0.02 0.02

0.07

îndicates that

pulverized.

te nf Au

Samples of

Toronto,

SILVER Oz./ton

NIL

NIL

NIL

NIL

NIL

NIL

NIL

NIL

trace

NIL

NIL

0.16

0.09

alBBiB

Date: Julv 13, 198l

split core and ore

Ontario- ' ), -*

COPPER PPM

52

---

——

40139

140

195

35 2170

830

this sample was completely

Â-MG. Lebel, Manager

r-, ^ ESTABLISHED 1928

1111111111111111111

i,

JUN 0 fi 1081

^•flK SWASTIKA LABORATORIES LIMITEDijiJBBjg^gr^^^n^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS


Received May 27, 1981

Submitted bv MPH Consulting

SAMPLE NO.

J4890

1493714938

149391494014941

14942

1494314944

1494514946

-

(Hrrtifiratr of Analyst*

Date: June 3, 1981

11 Samples of ore

Limited. Toronto, Ontario

Att: W. Brereton

GOLD SILVER COPPEROz./ton Oz./ton PPM

*-x.0.18 0.37 4270 ]

0.10 0.47 9670 (^jT^ 1

0.10 0.38 11000 /4fSoS CMooJ0.18 0.35 4650

\0.18 0.25 5180 J

0.05 0.16 9300 ") rj7^ ^JL

0.19 0.27 11300^5 USoS MHOOW^0.005 0.02 3430^

l .--r* \0.002 trace 1920 W ' l f̂ c^^c. n.'0.005 0.01 610 C400S (S-f-I^Vv/

1 ; 0.002 0.01 1850 J

•w*'

-

x

A wG\ Lebel, Manager

FCTARI I.CMPn 1Q9R

SWASTIKA LABORATORIES LIMITED1 w^&r

11™ Certificate No. 51 424

| Received Ms y ?1 , 1 Q Si

r.\j. o v^/x iv, ovvfAO iii\rv,vmir\niwrvix iivTELEPHONE: (705)642-3244


(Ewtifirat? nf Atmlyaia

Date: May 27, 1981 .

IS Samples of ore

Submitted by MPH nonsnlt.inp T, i mi tad. Toronto. Ontario

|

1" SAMPLE NO. GOLD SILVER COPPER

1" , 14916

14917

1 14918 1491914920

1 14921 14922 14923

. 149241 14925" 14926*

1 14927 14928*

1 149291493014931

1 14932 14933

| NOTE :"

111

Oz./ton Oz./ton PPM— ~-

0.002 NIL 83 \0.26 0.04 411 \0.27 0.04 390 0.22 0.03 9460.22 0.02 448 ^-' ,0.002 NIL 40 V •'\fc\v2- k NIL NIL —— f 0.26 0.04 1530 7 yjorv ^4-^nu/0.17 0.03 567 -MT7S -^ OT^^VS/0.002 NIL 270.30 0.03 529

- 0.310.15 0.03 420 0.002 NIL 39NIL }0.11 0.05 177 __ J .0.005 0.01 15"^ {"T]- f ^^ L0.04 0.05 130 V J ^^ c ;0.01 0.02 12 ( ^4CnU/ 0.04 0.14 24003 Of2-**J ; 6 "^SOW

^'Indicates samples that werecompletely pulverized.

.XA 7^/G. Lebel, Manager ^

F^STARI t.QMPH 1Q9fiCXXlM fet*

1111111111111111111

^ ^ OB •^•••K ̂ ^ÎB ̂ ^^h.

^ftV SWASTIKA LABORATORIES LIMITEDiSaiS^^ P .O. BOX 10, SWASTIKA, ONTARIO POK 1TOV^^ TELEPHONE: (705)642-3244


Qfcrtifirat* of Analysts

•4

Certificate No. 51337 Date: May 12 1981

Received May 8 1 981 6 Samples of Ore

Submitted bv M. P. H. Consulting Limited, Toronto, OntarioProject - C-409

i i i ^ . i , . - , - i iîj\'^ D '-3 A l-v^'p H-*! " 1 (-( a c r\

SAMPLE NO. GOLD SILVER COPPEROz./ton Oz./ton PPM

* 14905 0.005' 0.17 52000.002

* 14907 0.005 0.10 41000.005

* 14908 0.01 0.24 24000.01

14909 0.005 0.03

14910 0.002 Trace

14911 0.002 0.12

NOTE: * Indicates samples where the whole sample was pulverized.

Js -f jP*r Â/ v 1 14

^Do^7-(ooW

!/-^1G. Lebel -^Manager

PCTARI ICLJCn 1QOO(Mb. W*

l l l l l l



Qfcritfirate of

Certificate No. 51303-A

Received Apr. 29/81

Date: May 4 1981

Samples of Ore———.——————

Submitted by M.P.H. Consulting Ltd., Toronto. OntarioProject No-. C-409

k ^ M pSAMPLE NO.

1490114902149031490414905

. iGOLD

Oz./ton

0.030.010.01U.0050.04

- l r ^ Lt


0.350.310.320.030.46

l -i o o

1510

19900

lint*


1* Certificate No.

W SWASTIKA 1^^ P .O. BO)

ANALYTICAL

Okrtifiral

/n cJ \ r?p x 0/4. f

M Received July 9, 1931 6

i Submitted byii ij i

• 'it j^

MPH Consulting Li

SAMPLE NO.

26415

26416

26417

26413

26419

26420

mited,

GOLD Oz./ton

0.005

0.02

0.0050.002

NIL

NIL

LABOR)< 1 0, SWASTIKA TELEPHONE: {7C CHEMISTS* AS;

p nf Atralg,

rSamples of sp!

l

TORIES LIMITEDONTARIOPOK 1TO

)5) 642-3244 SAVERS* CONSULTANTS

ffi*

*ate: Julv 21, 1931

it core

Toronto, Ontario 1 rt

SILVER Oz./ton

0.01

0.01

trace

trace

trace

0.01

(^k i IS *

COPPER PPM

450 116

97

97

Per.G. Lebel, Manager

ESTABLISHED 1928

l l l


TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS *ASSAYERS* CONSULTANTS

drrtifiratr of Analysis

Certificate No. 51826 Date: July 21. 1981

l Received July 7, 1Q&1 Samples of split core

Submitted by MPH f.nn.qnl t,i ng T .i mi t. P-ri } Toronto, Ontario

l l l l i l l l l l l l l

SAMPLE NO.

26407*

2.4 S. S -^i- S

?, tt r - 2 s •v's

2 4?. S; - 2:43-53

26409*

26410

26411*

26412*

26413*

26414

GOLD ./ton

0.260.28

0.002

0.03

0.02

0.630.64

0.0050.002

0.040.04

0.12


0.23

trace

0.02

0.02

0.48

0.01

0.05

0.05

2400

93199

5973650

103

1170

305

i, 2.

1-0

3-o

NOTE: ^indicates that these samples were completely pulverized.

/.i.M /S-o'

G. Lebel, Manager

/ft)

ESTABLISHED 1 928du** fatal


APPENDIX B

DRILL LOGS: HOLES 81-1 to 81-13

DIAMOND DRILL RECORDHole No. 8 1 ~ 1

Hole No. 81-1Property Br i scoe-Bry ceTownch,p Bryceinr^lmn 1 + OOE

0 + 50Sloggedfiy W.BreretonCorel oration Core Shack ; 3+OOE , 0+

356 ft (107.8 m)1 engthBearing 340"Dip -50"Objective Test main zone under

surface trench

25N

Remarks Previous Noranda hole intersected o. 22 Au/3.8

Commenced April 11. 1981Completed April 14, 1981DriiiingCo Barron Dia.DrillindCoreRi7e NOCasing Left in Hole No

ft core len.orth.-

FootageFrom

0

34

To34 ft

134 ft

D E S C R 1 P

Dip: Collar - SO 0

Etch Test Depth Rdg. True

1. 150 ft 44 0

2. 350 ft 42 0

T 1 O N

OVERBURDEN

COARSE ANDESITIC FRAGMENTALqreenish-arey, generally crudely bedded with bedding defined by paral-lelism of major plane of fragments; fragments are predominantly ofblock and lapilli sized material which are typically sub-rounded torounded.Clast types include a med. gr. creamy to light-greyish, feldspar por-phyry, a dark feldspar-porphyry, and a light, fine-grained dacitic-looking volcanic and comprise 75% or more of the rock.Original f erromagnesians are altered to chlorite throughout; rock ingeneral shows weak carbonatization.Rock matrix consists of feldspar porphyritic (andesitic) crystal tuff.Unit is variably fractured; fractions are filled with quartz±carbonateveinlets .Fractures are of two predominant orientations with one set at approx.50" to 80 0 to c. a. and a second set at approximately 10 0 to 30" to c. a

Pyroclastic Bedding53 ft 40 0 to c. a.67 f t 45 0 to c. a .

1O7 f t- Aft 0 t-o r? . a -l Tfl f t- 4.^" to r? . a .

Trace to l-2% fine pvrite locally disseminated in unit as at 46 ft, 58ft.Thin hematite films on ioint and slip faces throughout unit.Local epidote patches and blebs 100-13098.3 ft:often cubic

ft.!X2in qtz veinlet at 20 0 to c. a. containing 1-2!* dissem.

pyrite mainly along fine fractures.

Sample No.

14801

1480:1

1480:

1480/

1480!

1480*

1480:

1480*

(ft) From

46

53

-97.5

236-'

277.:

281.;

282.'

287

(ft) To47

56

99*

238

278. E

282. i.

2B3.4

287 .i

(ft) Length1.0

3.0

1.5

1.1

1.2

1.2

1.0

0.8

Location Sketch

ozAu

nil

0.002

nil

nil

0.06;

0.11

0.02

O.OC

ozAg

nil

nil

tr

tr

0.02

0.09

tr

2 nil

N

Clai

Sea

lorth

mNo24227

e: r -

l

l

l

li

l l l l l l l l l l l l l

DIAMOND DRILL RECORD Note No.. Sheet No..

81-1

FootageFrom134

271

280.7

To271 ft

289.2

283.4

DESCRIPTION

ANDESITIC TO CHLORITIC CRYSTAL TUFFrelatively massive, featureless, coarse feldspar porphyritic crystaltuff. This material forms the matrix to above unit; contact with abovpyroclastic is marked by a 1 ft band of dark fine grained tuff or mud stone with quartz veining.The crystal tuff unit consists of white plagioclase crystals and da'rkgreen chlorite clots in a greenish chloritic matrix with scatteredquartz eyes. Rock is weakly carbonatized where tested with weak HC1.There is local, trace pyrite and variable hematite mainly on slip andfracture surfaces and in veinlets ± quartz-carbonate. There is anoticeable increase in hematization progressing down the hole.A weak schistosity is present generally at 60" to c. a.The tuff has been finely fractured with clear quartz ± carbonate andhematite forming hairline to 1/2 inch veinlets; one fracture set is at60 8 ro 80" to c. a.No appreciable sulphide association; there is a concentration of sili cification from 144 to 173; this veining is cut by later, thickerveinlets of white quartz, carbonate and hematite.JLby tt: B inch tragment of fine-grained volcanic (? ) showing chillededges against turt with 1* pyrite.175 ft: 2 inch quartz-carbonate-hematite vein zone alona local shearat JL5 0 to c. a.185 ft: 3 inch fraament of fine-grained volcanic.186.5 fti 1 inch vein of whLte quartz at 20" to c. a.209 ft: 1 inch qtz - carb. -hem. vein at 20" to c. a. with one smallcrystal chalcopyrite.221 ft: 1 inch atz-carb-hem vein at O 0 to 20 0 to c. a. as noted^ theseveinlets appear to be later than the foreqroincr fine, clear quartz-hematite filled fracturing.

CHLORITIC TUFFgradational upper contact with above, but sharp lower contact; green-grey, fine-gr rock with greenish chloritic clots similar to above tuffbut missing f sp phenos; becoming highly schistose toward vein zone(at 50% to c. a. ) .

MAIN VEIN ZONEzone of strong shearing ± chloritization, carbonatization, silicifica tion and pyritization., section from ' .281.6-282.2 is approximately 80** pyrite-quartz vein material; 1/2 inquartz pyrite veinlet at 282.9,; pyrite in the main vein is diatsihcttty

Sample No.

i

From To

*

Length

l l l l l l l l l l l l l l

DIAMOND DRILL RECORD Hote No.. Sheet No.

81-1

FootageFrom

289.2

To

356 ft

IS. f. f 4

^

DESCRIPTION

med gr granular and appears to float in fine, clear to whitish quartzwith chloritic slips; there is minor chalcopyrite as fine splashes inquartz generally separate from the main pyrite zones.283.4 - 284.4 ft: dacite fragment, very f. g., greyish with scattered c

vesicules; contains 1-3*?. pyrite incl thin diss. 1/4in band at lower contact which is sharp at 40 0 to c . s

INTERMEDIATE BLOCK AND LAPILLI TUFFgrey, dacitic-looking ; not as noticeably feldspar porphyritic as pyro clastic from 34 to 134 ft; matrix is essentially a fsp ppy xtal tuffbut most of fragments are dacitic to chloritic rocks rather than fspppy as in 34-134; fragments to 1 ft or more.

END *~*F HOI^E

Sample No.

uart2

.

From To Length.1 II.— 1 — — 1 ' ~--

l l l lll l l l l l l l

DIAMOND DRILL RECORDHoteNo...

81-2

Hole No 8 1 ~ 2Property Briscoe-Brycer^nch-p Bryceinr-inn 2 + OOE

0+50SloggwiRy W.BreretonCore i oration C Qr e Shack ; 3 + OOE , 0 + 2

Remarks

, pngfh 376 ft(113.9 m)Bearing 340 0Dip -50-Objective Test main vein zone

5N

Comment April 15, 1981Completed April 20, 1981rviiiingCo Barron Dia. DrillingCorn SIT* NQCasing 1 eft in Hoto No

-

FootageFrom

0

48

1O5

To48 fi

105 ft

335 fi

D E S C R 1 P

Dip: Cottar -50"


1. 150 ft 46 0

2. 300 ft 42 0

T 1 O NOVERBURDEN

COARSE ANDESITIC FRAGMENTALconsists of fsp ppy fragments in finer, usually darker, fsp ppy ma trix; fragments generally lighter coloured and up to J. f t or more.74-76 qtz- C O 3 vein zone - split

ANDESITIC CRYSTAL TUFFm. g. fsp ppy rock with darker chloritic clots and whitish fsp pheno crysts; contains, at top of section, f. g., light greenish-grey da-citic - looking fragments which are typically speckled with Z-3%diss. py; there is minor hem on slip faces and scattered qtz-carbVe"lnlets , generally l"r at various angle to c. a.; these veinletsconsist of both white and finer veinlets of clear quartz. Lower con'contact is sharp and at 55" to c. a.124-125: shear zone; sericitized, chloritized; contains qtz-py vein-1 0 4- e 4- r* 1 -i n*"*lii m f t- i ';q -F*-. A" A stf-t+ir* f r-artc w {t- h 14 r? i e e nv

Core Angles: 115 ft - 45 0124 ft - 4O e248 ft - 65"

163—164 ft- few nartiallv diaested fraaments171 ft: 6" f .a- dacitic fraa.191—192 ft: atz— carb vein zone193 ft:226 ft:

1" chloritic zone z qtz2" atz — eo vein

241-242 ft: uartiallv diaested fragments186 ft onwards appearnce of qtz phenocrysts in addition to plagiccla

Sample No.

148091481014811148121481314814148151481614817148181481S1482C1485*1485S1485S1486CI486]

ses

(ft) From

73.7124 .5191.5

31C33C

338.734C343334365371

373.5339.2151. e149.1158.:128.6

(ft) To

76125,8192.5

311330.5

339341343336

366.5372

374.534C

152.8150. E158. S130.3

(ft) Length

2.31.31.01.00.50.31.02.02.01.51.01.00.81.20.80.60.7

Location Sketch t\

Clai

Sea

ozAu

nil0.01

).002nilnil

5.0051.2950.12

0.002nil

0.002nil0.03nilnil0.01nil

ozAg

nil0.07trtr

0.010.010.620.070.010.010.02nil

0.030.01

3.005nilnil

ppmCu

47822

10-

170421

85001730

9162

1468

—lS4—

.8500—

lorth

tm No 24227

le: 1"-

l l l

DIAMOND DRILL RECORD HoteNo. Sheet No..

81-2

FootageFrom

335

338.8

343

-

To

343 ft

343 ft

376 ft

376.ft

DESCRIPTION

277 ft: •lacitic fragl306-3O9 ft: darker,, fin^r grained fragmont-al section310-311 ff-.t 1* nv328.60330: 1-2* py in f sp ppy xtal tuff

CHLORITIC TUFF

MAIN VEIN ZONEzone of shearing and chloritization with heavy (80%) concentration ofquartz-pyrite vein material from 340-341.2 ft and scattered thinveinlets and disseminations over rest of zone.Section from 340-341.2 is distinctly banded parallel to schistosity,quartz is relatively clear and translucent containing tiny white crystal inclusions (plag?) . There is l-3*k chalcopyrite associated withthe quartz but generally removed from the pyrite; pyrite is medium-grained, granular as in hole 1.There is variable carbonate and sericite in the sheared/mineralizedarea; shearing and banding is at 45-50 0 to c. a. avg 48 0 . Individualpyrite-rich veinlets are typically surrounded by 1 cm bleached alteration halos; also, at 341 ft, cpy appears to be distinctly later thanqtz-py as the former fills later cracks and vugs in the quartz; thisveinlet is also somewhat vuggy with open cracks at right angles tove inlet- walls .

INTERMEDIATE BLOCK AND LAPILLI TUFFas in Sole 1 this section is noticeably less feldspar porphyriticthan overlying pyroclastic section.Note that overall section from 306 to 354 contains numerous narrow

cjenerallv unmineralized carb-qtz veinlets 1 mm - 1 cm in two mainsets - one fillina fractures at a hiah anale to c. a. and the secondat 20| and less.344 - 346 ft: tr py in coarse fragmental.365-366.8 ft: l-2@ scattered py cubes in sheared chloritic lapillituff.

END OF HOLE

Sample No. From To

*

Length

l l l l l l l l i i


DIAMOND DRILL RECORDHole No R 1 -

Hole No 81-3Prnrwrtv Br i scoe-Bry C6Tn*nQhip Bryre

3 + 08E0 + 25S

loggedRy W.BreretonCoreLorafion Core Shack ; 3 + OOE , 0 + 2 !

Remarks

length 261 ft (79.1 m)Bearing 340"Dip -50"Objective Test main vein zone

IN

Cnmrm.nced April 21, 1981 nip: Collar ~50 0Completed April 22, 1981Drilling Co Barron Dia. Drillin jEtchTest Depth Rdg. TrueCore Sire NQCasing left in Hote No 1* 2 61 f t 4 7 "

.

FootageFrom

r\

48

184.7

To—— 48 fi

184.7

193.2'

D E S C R 1 P T 1 O N

ovpRR-j ppEN

Sample No.

14821ANDESITIC FELDSPAR PORPHYRITIC CRYSTAL TUPP 1becoming dacitic tuff towards base of section as prov holec. r,,-,*-*, L4822that f sp pheno crysts disappear over last 2 ft before lower- ™r,i-^trel. abundant fracturing at verv low angle to c. a. fillet vn-h ^f.CO 3 vein material with l-3% disseminated ovrite. some f r-a^ i-nr-oc .-.re tain muddymovement.

fault gouge material and are slickensided suaoestinn cnme

76 ft: faint schistosity at 50 e to c.pheno crysts and plag clots68 ft: 1'

.a. defined by alignment- n f f *sp

1 v.f.g, hard siliceous fragment, light greenish-arev-rhvol -itic82 ft, 87 ft: 2" and 8" qtz-carb-ep-hem veins97-100 ft.113-133 ft:± qtz ± ep

101-103 ft qtz-carb vein material ± l -2t py ajt O 0 to c^a.Fault Zone - zone of fracturing, brecciation and carb

veining; some vuggy sections, variable oxidation of rock± b leaching; negligible sulphide143.6-147.3 ft: strongly sheared and clet at 144.159 ft: 4"

6; shearing at 60" to c. a.rhloritiy.pd wlfh — 1 r qt7-py voin-

aphanitic light arev siliceous fraament-183.8-184.7 ft: dacite fragment - aphanitic, greeni sh-gr-ey v n-t, 4- rfine pyrite

INTERMEDIATE CRYSTAL TUFFpredominant chloritic clots with lesser plaa Dhenoervst-ej . nr-r- f n -dacitic fragments with some soft sediment-like rlefor-maf- i *in

. . - .

L4823

L4824

1 4825

L4826

4827

i.4857

L 4 828

L4829

14830

(ft) From

96

101

127

128

130

144

93.4

.94.6

234

102

123

(ft) To

99

102

128

130

131

.45.5

.94. 6

.95.3

235

103

124

(ft) Length

3.0

1.0

1.0

2.0

l.O

1.5

1.2

0.7

1.0

1.0

1.0

Location Sketch N

Clai

torth

t25692

Scale: 1" -

ozAu

nil

nil

nil

nil

nil

0.02

0.80

).002

0.01

J.002

nil

ozAg

nil

nil

nil

nil

nil

0.09

0.35

nil

0.01

nil

nil

ppmCu

39

44

36

36

34

818

3980

-

420

46

64

DIAMOND DRILL RECORD HoteNo.. Sheet No..

FoeFrom

193.2

193.4

197.6

tageTo

197.6

195 ft

261 ft

261 ft

DESCRIPTION

DACITIC TUFFfine-grained, light greyish: well bedded in virHnit-.y n f i qq f t- 0 TROto c. a. and 193 ft @ 50" to c. a.Unit is well fractured with numerous carb-qtz veinlets 1 mm - 1 cm atlarge angles to c. a.

MAIN VEIN ZONE1-2" qtz-py cpy veinlets at 193.5 ft and 194.3 ft with DV dissemina tions and hairline veinlets over rest of section ; main sulphide vein lets show bleached alteration borders and fracturing perpendicular towalls of vein as prev. hole^there is some hematization .

INTERMEDIATE FRAGMENTAL LAPILLI AND BLOCK TUFFas prev. holes; several rel, large dacitic fragments e.g. 224.5-226,237-238.3 with l-5% very finely rtice py

and/or schistositv generally too indisf--* n^t- *-o Ho mo^ ?ura/-!246 ft: 1/4" qtz-py veinlpt

END OF HOLE

-

SampleNo. From To Length

lDIAMOND DRILL RECORD

Hole No..

HOIPNOPrnp^ty Briscoe-BryceT —— hip Bryce

4 + 05E 1 oralinnO4-15S

1 ogged By W RTpr-o-hnn

rnrn 1 raatinn Core Shack : 3 + OOE r 0 + 2

Remarks

ipnjh 201 ft (60.9 m)Reanno 340"

nip -55"Objective Test main Vein Z0ne

5N

m*™** April 23, 1981 nip- CoHar - 55 0roofed A?ril 2 7 ' 1 98 1nriiiinnCo Barron Dia. Drilling Etch Test Depth Rdg. TrueCoreSi7e N2Casing left in Hole No ^ ' 201ft. 48 0

FootageFrom

n

Q fi

134

141

151

To96 ft

1 ~\A •Ft-

151 ft

151 ft

201 ft

2O1 ft


OVERBURDEN

FELDSPAR PORPHYRITIC CRYSTAL TUFFacrain . aradual disappearance of f SD ohenocrysts towards bottom ofsection alona with aooearance of aohanitic dacitic fraas (e. a. 131 ft)96 104 ft: core is badlv broken UD — some bleachina and carb veininaalona^f ractures at low anole to c. a. - probable fault zone.

INTERMEDIATE TUFFchloritic crystal tuff very similar to above i.e. missing the placrphenocrysts, along with finer-grained dark chloritic tuff; whole sec tion sheared and exact relationships obscured.MAIN VEIH ZONB141 ft:141-143 ft:143-145 ft:

145-147 ft:

147-151 ft:

1/2" qtz-py veinlet j shearing at 45 e to c. a.sheared intermediate tuff with chloritic clotsbadly broken up zone - 50%oxide - fault zone.40% qtz - py vein material

core recovery - abundant iron

; locally intensely bleachedwith original tuff completely altered to ser * chl -f qtz.highly sheared chloritic rock wi,th local narrow seams andveinlets of py and calcite ;minor sphalerite xtals assoc.with carb.

INTERMEDIATE LAPILLI AND BLOCK TUFF152 ft:minor qtz i

sch at 65 0 to c. a.py veining at 152-154 ft, 158-162 ft, 171.5-172.5 ft,

188-189 ft.END OF HOLE

Sample No.ami.4832.4833.4834.4835L4836.4837.4838.4839.4840.4841.4842.4843L4844.4845L4846U847L4848.4849i.4850

[ft) From1 1 ^136137139140141142143145146147

.31.5152149159157

.71.5

.78.5147150

(ft) To1 Tfi137139140141142143145146147149

.32.5154151161159

72.51.79. 5L47.5151

(ft) Length1 O1 -02.01.01.01.01.02.01.01.02.01.02.02.02.02.01.01.00.51.0

(

(

Location Sketch IV

Clai

Sea

ozAu

nil

niJ.002nilnil.002nilnil1.34o.i:.003nil.002.002.002nil.002.005.002nil

ozAg

nil

rH 10.01nil0.01trnilnil1.040.080.01nilniltrnilniltr0.010.0]o.o;

ppmCi

AR

4633048

98024252

11075001350478-72

160506280

410402- 3

lorth

tmNo 25691

e: 1"-

ppmZn

1,60(

l DIAMOND DRILL RECORDHole No. 81-5A

LI i Ki 81-5A Hole No.Briscoe-BryceProperty " J . ..Bryce

location 5 + OOE0-1-7=1?;

logfjwlRy W RT-oi-pi-rm

Core location Core Shack : 3 + OOE . 0 + 2

Remarlcs Lose 7 ^pieces - 5

length IR c; f i- ( ^Ifi 1 m)Bearing 340Din -50 0Objective Test main vein zone

5N

ft NW casing in initial atte

Commenced April 28, 1981Completed May 6, 1981DriiiingCo Barron Dia.DrillinaCore Sire NOCasing left in Hole No

mpt at hole

FootageFrom

0

74

132.5

137

To

74 ft

137 ft

-

137 ft

185 ft

185 ft

D E S C R 1 P

Dip: Collar -50 0


1 185 ft 43"

T 1 O NOVERBURDEN

FELDSPAR PORPHYRITIC CRYSTAL TUFFa coarse' generally massive, green-grey crystal tuff of andesite corn-position as prev. holes88 - 90.3 ft: lost core mud seam - fault101 - 109 ft: coarser fragmental zone123-123.8 ft: narrow qtz-py veinlets with intense sericitic al

teration12b ft: 1/4" qtz-py veinlet in narrow shear at bU" to c. a.

MAIN VEIN ZONE132.5 - 134 ft: sheared but relatively barren chloritic tuff, broker

up134 - 135.5 ft: poor recovery - contains 20% qtz-pyritic vein ma-

terial as veinlets to 1/2" assoc. with intense lighlareenish sericitization ± fuschite (?)

135.5 - 137 ft: rusty, broken up zone with Fe oxide staining infracture surfaces - poor core recovery

INTERMEDIATE BLOCK TUFFcoarse andesitic pyroclastic fragmental as previous holes

END OF HOLE

Sample No.

14851

1485^

1485^

1485'

JL4SJ5J

(ft) From

132. E

133. E

134.1

135 e

122

(ft) To

133. E

134. E

135. E

l 1*"

123. E

(ft) Length

1.0

1.0

1.0

1 5

0.8

Location Sketch

ozAu

0.01

0.78

0.06

n 02

0.005

ozAg

0.01

0.34

0.05

Q 02

0.0^

N

Clai

Sea

ppmCu

-

-

-

228

*

Orth

tm Mn

e: 1"-

ppmZn

L710

213

-

Q^4

L010

l l

l l

l


DIAMOND DRILL RECORDMote No. —

81-6

Hole No 81-6Property Br i SCO6-Br VC6Township P f y r. p1 oration 2 + 50W

2 * 1 5 Slogged Ry H. TremblayCore Lor-ation Core Shack , 3 + OOE , 0 + 't

Length 328 ft (99.4 m)Bearina 340 0Dip -50'Objective Test geophysical ano

malies

5N

Remarks Lose 1 - NW shoe when peeling casing - have to c

Comment May 7, 1981 nin. Collar -50"complex May 15, 1981nriiiingco Barron Dia ,Drillin(tEtchTest Depth Rdg. TrueCoreSbe N O-Casing left in Hole N o 1 1^0 ft A 7 "

2. T2R ft- 43"

:ement upper portion of holef aul't zone

FootageFrom

Q

24

63.5

120.!

286

.

To

2-4 ft

63.5 ft

120.5ft

286 ft

—

328 ft

328 ft


OVERBURDEN

ANDESITIC LAPILLI AND BLOCK TUFFarev-areen , clasts consist of chloritic rocks, dacite and feldspar porohvrv; fraament to matrix contrast is not sharp, crude bedding obser vable as at 33 ft and 51 ft - both at 65 0 to c. a.53.5-54 ft:63.5 ft:

fault zonecontact at 50 0 to c. a.

CHLORITIC AND ANDESITIC TUFFSlight green, homogeneous, minor carbonate veining, trace pyrite.113-118 ft: 3— 5% atz— carb veinina wi th 1-2'fc DV

INTERMEDIATE CRYSTAL AND LITHIC TUFFfine to raed . arain: arev-areen. small scattered clasts throughout inclsmall chloritic fragments134-148.5 ft: thin pv veinlets143-150 ft:225-227 ft:

chloritic tuffchloritic tuffaceous zone, highly sheared, fragmentalarea with carbonate veinlets

227-286 ft: crystal carb tuff with f erromagnesium fragments at 60 0to c. a. grading to chloritic tuff 278-286 ft.

.FELDSPAR PORPHYRITIC BLOCK TUFFtrace sulphide, clasts consist of feldspar porphyry and chloritic rock

END OF HOLE

Sample No.

148&4

•14865

I486*

14867

14868

1 486C

1 4R7f

14871

1487:

1487'

1487/

1487!1467*

(ft) From

114

116

134

136

13E

13c

l 4f

(ft) To

116

ne136

13E

13S

14C

141j

1411142.?

142.!

144

14!

14(is:

14^

14!

14(

14(153 . "

14877 278 28(214978 } 8(14879 282

} 2 8;

1488Q 284 28(

(ft) Length

2.0

2.0

2.0

2.0

1.0

i r

l C

1.5

1.5

l.C

l.C

2. C1 . 32.02. C1.52.4

Location Sketch

DzAu

0.002

nil

nil

nil

nil

nil

nil

nil

0.002

0.002

0.002

nilnil

0.002

,zAg

nil

nil

nil

nil

nil

nil

nil

nil

nil

0.005

tr

nilnil

N

Clai

Sea

jpmCu

~.

—

-

27

33

13

21

—

-

211

223

-—

nil

nil nil0.005| nill

..——

orth K

t . 24228m No

e: 1"-

14881 286 287 1.0 0.002 nil -

DIAMOND DRILL RECORDHole No.

81-9

Hole No 81-9Property Br iscoe-B ry CPTownoh.p B rye eloratmn 5 + OOW

3 + 80NInggeriRy H.TremhlayCore t oration Cor e Shack ; 3+OOE . 0 + 2 !

Remarks .

326 ft (98.8 m)Bearino J 40 "

Dip -50"Objective Test aeophysical ano

malies on Contact Zon(

N

Commenced May 28 P 1981 Dip: Collar - ID 0Completed June 3 r 1 981nriiiinqCo Rarr-on n i x D T- i 11 i n jEtchTest Depth Rdg. TrueCore Size NQ

sCasing left in Hole No

-

FootageFrom

n

34

94

-

146

150

To34 f t

94 f t

146 ft

150 ft

161 ft

.


nvppRiTcnPN

INTERMEDIATE LAPILLI AND BLOCK TUFFfragments consist of dacite . andesite and feldspar porphyry along witfrblack chloritic clots and f raciments . fraament size to 10 inches, maxi—

veining from 47 to 52 ft* some hematitic staining along fracture sur faces, trace sulphide.45 - 57 ft: ash to lithic tuff finina up hole (implyina tops to

south)

ANDESITEdark areen. med to fine qr., even textured, somewhat tuffaceous lookincwith rare bandina at 60 0 to c. a.; upper and lower contacts sharp at 50'to c . a .137.5 ft: fine-gr. chloritic tuff band 2 inches thick at 60" to

c .a.141-141.5 ft: sericitic-chloritic tuff band at 45" to 70 e to c. a. witl

S-4% carb veining

TUFFACEOUS SEDIMENTSvery fine gr., greyish to locally cream-coloured, sericitic-onloriticsediment, tuff bedding at 60 0 to c. a.148 ft: 1 inch qtz vein or chert zone with 15** py ± cpy

ANDESITE TUFF AND TUFFACEOUS SEDIMENTmixed zone of fine-gr. andesitic tuff as 94-146 ft along with sericiticchloritic tuffaceous sediment

Sample No.

14956

14957

14958

14959

14960

14961

PL4962

14963

14964

14965

14966

—

(ft) From

146

L47.5

148. 5

197

L98.5

L99.5

210

211

231

234

29^7

(ft) To

L47.5

L48.5

150

1 QP. e;

L99.5

200.5

211

214

234

235

298

(ft) Length

1.5

1.0

1.5

l t;

1.0

i .0

1.0

3.0

3. O

1.0

1.0

Location Sketch Nlorth

tScale: 1 " -

ozAu

nil

0.06

).002

•n i 1

).002

nil

nil

nil

nil

).002

nil

ozAg

nil

0.02

nil

o m

0.04

nil

0.0

tr

nil

0.0

nil

ppmCt

57

361

72

170

990

62

. 128

117

130

: 200

184

l

DIAMOND DRILL RECORD Hole No. Sheet No.

FootageFrom

161

176

197

21C

To176 ft

197 ft

210 ft

326 ft

326 ft

DESCRIPTION

FELDSPAR PORPHYRY (CRYSTAL TUFF?)grey-green, med gr; massive, overall dacitic composition, upper andlower contacts sharp at 65 0 to 70 0 to c. a.

ANDESITIC TUFFfine gr. as 150-161; generally chloritic with very tine gr. portionsof chloritic-sericitic material194-197.3 ft: chloritic-sericitic tutt witn DiacK cnloritic llthlCT

fragments, carconate richjl* pyrite

BEDDED TUFF-SEDIMENTvery fine-gr. bedded carbonate to chlorite/sericite-ricn sediment;bedding at 60 0 to c. a.Carbonate-chertY bands 1/2 to 1 inch with 10*; to 25!* pyrite at 198 ft199 ft and 210 ft200.5 ft: graded bedding indicating tops up hole

PILLOW BASALTcarbonatized, chloritic, amygdular dark green, fine to very fine gr;generally 1-2^ pyrite as blebs and enhedral crystals throughout234 ft: li in massive band pyrite at 75 0 to c. a.

END OF HOLE

fc

Sample No.

.

From To

*

Length

l l l l l

DIAMOND DRILL RECORDHole No.. 81-10

Mn*.*, 8 1 ~ 10

1 nation 4 + 50E1 + 50S

loggedBy H.TremblavCore Location Core Shack ; 3 + OOE , 0 + 2

Remarks

length 716 ft (217 m )Bearing 3 4 0 0Dip - 5 0 0Objective Test main vein zone

5N

Commenced June 4 r 1981Completed .Tune 10 r 19R1Drilling Co Bf? r"rr)n n i a m-illinrjCore Size NQCasing Left in Hole No

FootageFrom

0

14

-

91

101

166

168.4

To14 ft

91 ft

101 ft

166 ft

168.4ft

186 ft

OVERBURDEN

D E S C R 1 P(0-18 casing)

Dip: ™" S 0 o Collar


i. i nn f* 4 flo

2. 400 ft 46 0

3 fiqfi f f. - 4^o

T 1 O N

DACITE FRAGMENTAL TUFFgrey, feldspathic, porphyritic; fragments and tuffaceoiis matrixmaterial very similar.The fragment to matrix contrast is generally poor; fragments vary upto 8" but generally measure around 3".5% qtz-carbonate veins ( 1.5 cm) occur at -3O-45" to c. a.; trace py-rite.14 - 27 ft: open fractures because of dissolved carbonate veins

CHLORITIC TUFFmassive f .g . to v.f.g. chloritic, greyat 1OJL ' fo"-lU2 ft; trace sulphide; upperc .a. , lower contact at 50 0 to c. a.

JolacK; /" fsp porpnyry rragmentcontact irregular at oO" to

DACITE-ANDESITE FRAGMENTAL TUFFgrey to dark grey with blocks to 1 ft of feldspar porpnyntic dacitein a fine-grained matrix. The fragmentand the unit becomes more mafic than at

to matrix contrast is poor14-y J. .

MAFIC FLOW OR INTRUSOVEv.f.g. to f .g. black, chloritic, schistose at 45 0 to c. a. aatygdular-like with carbonate-hematite fillings; lower contact -banded at 35"to c. a. (sharp).

COARSE DACITE FRAGMENTALdark grey, v.f.g. to f. g. with feldspar porpnyry fragments in a r. g.andesitic matrix, fragment to matrix contrast poor as 101-166; tracesulphides , 5* qtz— carbonate veining.

Sample No.

14972

14973

14974

14975

14979

14980

(ft) From

535.9

536.9

623

595.5

366

369

(ft) To

536.9

536.9

626

598.5

369

372

(ft) Length

1.0

3.0

3.0

3.0

3.0

3.0

Location Sketch

ozAu

0.03

nil

).005

nil

nil

nil

ozAg

0.05

nil

nil

nil

nil

tr

North

IScale: 1"-*

ppmCu

572

69

46

141

7

10

l l l l l l l

DIAMOND DRILL RECORD Hole No. Sheet No.

FoeFrom

1RP

196.6

206

212

-

256

387

tageTo

196.fi

206 ft

212 ft

256 ft

387 ft

407 ft

DESCRIPTION

M AFT C FT.OW OR INTRUSIONdar-lr gr-een r \r f ej n h i 1 1 od i-onf-sct with star-like feldspar aggregatesin r-onl-T-al jw-ir f-, i rm - Also minor carbonate amygdules: upper contact ati^no. lower contact at 60 0 to c. a., both sharp.

DACITE FRAGMENTALas at l68.4 - 184 ft, carbonate-quartz veining b* irregularly aisuriDu-ted throughout.205-206 ft: brecciated contact - fault zone at 25" to c. a. Open

drusy carbonate fractures at 206 ft. Trace sulphides.

MAFIC DYKE OR FLOWas at 186-196*6" with f. g. contacts and f. g. center; 212 ft sharp con tacts at 75" to c. a., upper contact fault at 25 0 to c. a. - brecciated.

DACITE FRAGMENTALas at 168*4" - 186 ft; grey, with predominantly grey to pinKisn nemati-zed feldspar porphyry fragments in a f. g. green andesitic matrix. Poorfragment to matrix contrast. Pyrite trace - 5%; carbonate-qtz veinirregularly distributed throughout.

ANDESITE FRAGMENTALmixed derivative fragmental with feldspar porphyritic, creamy f. g. da cite and chloritic andesite (sometimes anygdular) fragments in a crys tal tuffaceous to chloritic tuffaceous matrix. Fragment to matrix con trast is good to excellent.256-268 ft: dark chloritic feldspar porphyritic fragments in a light

green m. g. crystalline fsp matrix; fragments up to b" butgenerally less than 3"; unsorted.

284.5-285.5* :broken core, highly fractured - fault zone256-306 ft: 2-3** carbonate-qtz-veining - trace sulphide366-372 ft: hematite-stained fracture minor pyrite - mostly unminera-

lized throughout344-348*6" mafic dyke(?) contacts at 4b 0 appear, 25" lower.

CRYSTAL TUFF FRAGMENTALmnro r-na-r^t*! y i-T-y si-a i l l n section of tuffaceous matrix with mixed frag-

-*Q7-dno ft-- t-wn seotiions of graded tuffs over 12-18" thickness indi cate tops UD hole

397 ft- 1" f. 9. tuff band at 50 0 to c. a., trace sulphides

SampleNo. From To

*

Length

f l l l l l l l l l l l l l

DIAMOND DRILL RECORD Hole No.. Sheet No..

81-10

FootageFrom

407

417

432

477

"

506

571

To417 ft

432 ft

477 ft

506 ft

571 ft

—

716 ft

DESCRIPTION

ANDESITE FRAGMENTALas at 256-387 ft: contacts gradational

CRYSTAL TUFF FRAGMENTALas at 387 — 407 ft exhibits graded bidding in 3 spparal-p 1 7 — IR- 7 on p c-

indicates tops up hoi pBedding indicated by elongation o-F fragments in graded bedding sec tions at 50-55" to c. a. - contacts yradational

ANDESITE FRAGMENTALas at 256-387 ft; fragments rarely exceed 3", 5 * predominantly car bonate veinina447'6"-450 ft: v.f.g. green mafic dyke with contacts at 70 0 to c. a.461-462"6": v.f.q. green mafic dyke with contacts at 70" to c. a.451-453 ft: qtz-carbonate-epidote zone at 20 0 to c. a.446-456 ft: brecciated andesite fragmental (chloritic, epidotic)

annealed

ANDESITE BLOCK TUFFas at 256-387 ft except fragments up to 2-3" in section 477-489; fragmen t s decrease in size quickly towards base of section

CRYSTAL TUFF - FRAGMENTAL ANDESITEmixed zone of andesite fragmental with mixed derivatives; fragmentsnot usually exceeding 3". Several sections of crystal lithic tuffindicate tops up hole. 3 -4* carbonate-quartz veining.

DACITIC CRYSTAL TUFFlight green, m. f. g. relatively even-textured with black chloriticfragments to 2 mm throughout. White sub hedral feldspar phenocrystsalso occur throughout along with round to angular quartz phenos636-636 '6 1': mineralized zone - three quartz-carbonate veins to

1 cm with coarse to fine-grained pyrite, minor cpyand a silver ^teluride rjmineral in one of the veins.'i1 h e vein with possible telurides has small, openfractures and contains more sulphides (lQ-15%) thanthe overall S-4% pyrite, minor cpy.

704-704'2": q.v. at 20-45" to c. a.598-599.5; 602-603; 613-617; 619-620 ft: dark grey f. g. mafic

dykes with generally irregular contacts: contactsat 619 ft-70 0 ; 620 ft-35 0

Sample No. From To

'

Length

DIAMOND DRILL RECORD Hole No. . Sheet No..

81-10

FootageFrom To

715ift

DESCRIPTION694'9"-695, 695 ' 8"-696 ' 2" , 698'6"-698 ft: creamy tuff to cherty tuffbands - slumped bedding in two upper bands, bedding generally at 55-60" to c . a .

END OF HOLE

Sample No. From To

*

Length

DIAMOND DRILL RECORD81-11

Hole No Q 1 IT

Property Br i scoe-Brvc eT^wrKihip B r y C eInration 6 + OOE

0 + 80Si ogged By H . T r emb layCore Lor-ation Gore Shack ; 3 + OOE , 0 + 2 1

Remarks

44fo ft (1 Jb . 2 m) Length

Dip ^ 0Objective Test main V6in Z 0ne

IN

Commenced ,, J une -L J. , 1 J. Djn . Co||ar - D-

DriliingCo Barron Dia . Drillin jEtchTest Depth Rdg. TrueCore Sire 2Casing 1 eft in Note N O

-

FootageFrom

0

22

-

-

175

188

239

To22 f i

175 ft

188 fi

239 f i

266 ft

OVERBURDEN


FRAGMENTALqrey qreen

DACITEwith fraqments to 6 in but qenerallv less than 3 in. Fraq^

ments numerous and qenerallv liqht qrev in a dark arev matrix. Frag ments consist predominantly of f. q. dacite and andesite tuff withlesser med-qrained feldspar porphyry tuff.Open fractures 22 to 36 ft because of dissolved carbonate veinsCarbonate-qtz veins occur preominantly128-150 ft

22-41 ft (5%) .: abundant calcite and lesser calcite-quartz-epidote

generally at 45-70 0 to c. a.Minor pyrite

MAFIC DYKElight green, v.f. grained chilled contacts with epidot ized maficphenocrysts in central portion; 5% irregular carbonate veining, l-2%diss. pyrite - contact at 181-70 0 to c181-183.5 ft: fragmental as at 22-175Contact:Contact:

183.5-50 0 to c. a.188-20 0 to c. a.

Sample No.

.4981

.4982

.4983:

.4984

.4985:

.4986

.4987

.4988.a. lft 1.4989

ANDES HE ERAGMENIAl,chloritic andesite tuff, cream-coloured dacite and feldspar porphyryfragments in andesite matrix, unsorted3 in, fragments angular to sub-rounded

; to 6 in but predominantlyMinor carbonate veining and

trace pyrite

CHLORITIC ASH TUFF (Fragmental)mixed zone of f. g. to v.f. g. chloritic tuff with chloritic fragments

.4990

L4991

14992

L4993

26406

(ft) From

109

153.8

154.8

. 35i:

:74.2

261

271

271

258

358

366

175

.83.5

553.4

(ft) To

112

154.8

55.8

153.8

276

262

:74.2

!74.2

261

359

369

178

1.86.5

555.8

(ft) Length

3.0

1.0

1.0

2.8

1.8

1.0

3.2

3.2

3.0

1.0

3.0

3.O

3.0

2.4

Location Sketch

ozAu

nil

0.0!

0.0!

.002

0.0!

o.o;nil

nil

nil

nil

nil

nil

nil0.0'

ozAg

nil

0.07

o.o:nil

o.o;o.o:nil

nil

nil

nil

nil

nil

nil

O.OS

N

Clai

Sea

ppmCu

80

770

572

69

308

298

52

-

-

-

—

—

40

830

orth

tmNo 2f^(

e: 1"-

l

l

l l l l l


DIAMOND DRILL RECORD Hole No Sheet No.

FootageFrom

266

286.2

351

354

359

To

286.3 i

351 ft

359 ft

355.8 ft

446 fi

446 fi

DESCRIPTIONand 2 5* unsorted fragmental with chloritic (black) fragments andcreamy v.f.g. dacitic fragments in a chloritic tuff matrix; f. g. bed ding at 45 0 to c. a. at 245 ft. Minor py; minor carbonate veining.Minor coarse pyrite in chloritic tuff from 258 to 261 ft.

t CHLORITIC TUFFdark grey to green, f. g. - v.f.g. chloritic-sericitic tuft with bed-ding/schistocity at 35-45 0 to c. a.1-2 cm qtz-py veins at 270 ft, 276 ft

FELDSPAR PORPHYRITIC CRYSTAL TUFFgrey-green m. f. g. granular with feldspar crystals to 1.5 mm and chlortic fragments to 3 mmMinor qtz-carbonate veining

CHLORITIC TUFF

MAIN VEIN ZONEgrey "to dark green tuff; 2 0* py-qtz veins with minor cpy; pyrite iscoarse and brecciated

DACITE FRAGMKNTAL ~ BLOCK TUFFcoarse, strongly feldspar porphyritic fragmental; grey-green feldsparporphyritic tuff with a large proportion of fragments being of m. f. g.m . cj . feldspar1 poT-pHyr-y - f ran t-n 1 f t-END OF HOLE

Sample No.

,—

From To Length

l l l l l l l l l l l llfi

DIAMOND DRILL RECORDHoleNo. 81-12A

HoloNo 81-12APrnnerty Br iscoe-BryceTownship Brycelocation 7 + OOE, O 4 OS~

toggpdBy 3 r TremblayCnro l or-ation Core Shack : 3 + OOE . 0 + 2 !

Remark.; Hole 81-12 lost in

,pnn,n 2 8y f t ^ 7 ' 5 ^

Bearina 3 4 O eDip -70 eObjective Test main vein zone

N

overburden at 154 ft.

Commenced JU ne 17., . ..198 J, Dip- Collar -7O 0Competed June 25, 1981Drilling Co Barron Dia .Drill i in. jEtchTest Depth Rdg. TrueCoreSLre NQCasing l eft in Hole N O

FootageFrom

0

123

130

133.6

To123 ft

130 ft

133.6'

259.6'


OVERBURDEN

FELDSPAR PORPHYRY TUFFgrey-green, m. g. tuff with feldspar phenocrysts to 1 mm and dark greetchloritic fragments. Generally even-textured.128'4" - 1 cm qtz vein with 1(^ coarse pyrite

CHLORITIC CHERTY TUFFfractured chloritic tuff zone with 10%as breccia

irregular qtz-carbonate veinsfilling with coarse granular pyrite cpy 1 - 2*!;.

l32 I-6" - 133'6": f-9-creamy c he^t band contorted with 1-2 mm laminaeot tine pyrite. Banding at O-20 0 to c. a.

FELDSPAR PORPHYRITIC CRYSTAL TUFF(minor coarser fragmental sections) grey-green, m. f. g. Generally even-textured with fsp phenocrysts to 1-2 mm and dark green chloritic maficminerals to 2-3 mm, irregular chloritic fragments to 5 mm; minor py rite152.6 - 154'6: broken core, fault zone in chert - 153'6" then in

tuff to 154'6"Coarse fragmental bands at: 172 ft - 175 ft consisting of a f. g.chloritic tuff matrix with feldspar porphyry fragments.Mineralized gtz-carb. veins occur at:145*6" - 145*8": gtz veins at 45 0 to c. a. with 10% granular pyrite.

minor cpy and minor grey mineral?188*3" - 188*6": qtz-pyrite zone at 35 0 to c. a.Coarse granular pyrite with minor bright green fuschite ? and lightgreen bleaching of tuff around vein.

Sample No.

14994

14995

14996

1499^

1AQQB

14995

1SOOC

(ft) From

274.5

241.5

127. S

130

IRfl

145

25O. e

(ft) To

276.2

243.1

128.7

133.9

1 OQ

1 46

251 ,c

(ft) Length1.7

1.6

0.8

3.9

1 n

1 -O

1-4^

Location Sketch

3Z AuD. 055

0.005

3.005

nil

n nn";

0-OQ5

nil

DZ Ag0.02

0.01

nil

nil

t- f-

ni 1

nil

North

Clai

Sea

jpmCu417

550

237

139

140

t Q 5

•^*

tmNo *6^1o- 1" —


DIAMOND DRILL RECORD Hole No.. Sheet No.

81-12A

FootageFrom

259.5

274.6

276

X

To

276' ft

276 ft

287 ft

iJb / ft

DESCRIPTION

250*6" - 250*10"; oh 1 or it- i r f . g tuff band wa t-h 1cm ql-T-.-oar-hfinat-p' vpin

——————————————————— hematite — o tainod ; — S-% — f i g- 1 — pyrite — occurs — i-n — chloritict- 11 f f .

Carbonate and qtz veins occur throughout at 45-70 0 to c. a. with onlyminor pyrite except as noted above.

201-252': limonite and hematite stainina

CHLORITIC TUFFgrey to black and grey f. g. siliceous in sections but non porphyritic.Small lithic fragments observed in narrow sections.

MAIN VEIN ZONEat 45 " to c . a .274.6 - 275: chloritic tuff with l-2*fc pyrite275 - 276: siliceous tuff-quartz vein zone with ICK coarse py

rite mostly occurring in siliceous tuff. Hematitestringers also present (minor) .

DACITE FRAGMENTALt. g. to v.f.g. aacitic fragments (grey) in a r. g. chloritic matrixsuggests tuffaceous material tilling in Between fragments.

EtJt) OF HOLE

Sample No. From To Length

l l l l l l l l l l l l

DIAMOND DRILL RECORDHole No.. si-i:

Hole No 81-13Property Br i s coe -Br y c eTownch,p Brycelocation 8+OOE, 0 + 40S

1 onnpd Bv ™ * E * BlTGlTGtOn

Core Lor-ation Core Sfeack ; 3 + OOE r 0 + 2 1

Remarks

1 engthBearingrao -70"Objective Test main vein zone

.N

Comment ^6 26, 1981

Completed J^Y 6' 1 98 1nniiinoco Barron Dia. DrillingCoreSbe N2Casing Left in Hole N o

FootageFrom

0

102

160

172

208.5

To102 ft

160 ft

172 ft

208.5ft

263 ft

D E S C R 1 P

Dip: — 7O 0 Collar ' U


1 157 69 0

2 328 65 0

T 1 O N

OVERBURDEN

FELDSPAR PORPHYRITIC BLOCK TUFFa coarse pyroclastic fragmental with fragments of light green-grey, fine-grainedvolcanic along with darker and coarser feldspar porphyry in an intermediate ash tuffmatrix110-111 ft: parting planes at very low angle to c. a.111-113 ft: 5% disseminated cubic pyrite125-127 ft: lost core155 ft: weak foliation at 45 0 to c. a.

IJCTTPRMEDIATE CRYSTAL TUFFcharacteristic liaht creamy crreenish-arev colour, relatively soft with abundantquartz — chlorite crystals and patches and lesser whitish feldspar crystals— uooer and lower contacts at 5 0 to 10" to c. a. Weak schistosity in aeneral at O0to c. a.

INTERMEDIATE BLOCK TUFFmainly dark feldspar porphyry fragments in a lighter green ashy matrix- perfectly gradational contacts with underlying unit

200 ft: schistosity at 250 to c. a.

INTERMEDIATE TUFFrelatively fine-grained; gradational contacts top and bottom, greenish in colour -rock is relatively hard, competent (difficult to split) and is not noticeablysheared

Sample No.

2fidO7

26408

2640S

26410

26411

2641;

26412

26414

26415

26416

26417

26418

26419

26420

(ft) From2Q.2

291

295.5

256.5

255. 5

353.6

257.5

212

219.7

125

310.9

296.5

289

293.2

(ft) To

2 Q 3 . 2

292

296.5

257.5

256. 5

243.5

260.5

213.5

220.7

127

311.8

300

292

296.5

(ft) Length

1 . 2

1.0

1.0

1.0

1.0

1.0

3.0

1.5

1.0

2.0

0.9

3.5

3.0

3.3

Location Sketch North

Sea

ozAu

O 27

0.002

0.03

0.02

0.635

0.003

0.04

0.12

3.005

0.02

3.005

3.002

nil

nil

szAg

O. 23

tr

0.02

0.02

0.48

0.01

0.05

0.05

0.01

0.01

tr

tr

tr

0.01

ppmCu

24OO

93

199

597

3650

103

1170*

305

98

450

116

97

84

97

f f^lvl \n/ y*rf ^^

te: V- """"*

DIAMOND DRILL RECORD Hole No. . Sheet No.

81-13

FootageFrom255.5

263

292

302

327

To260.5ft

292 ft

302 ft

327 ft

DESCRIPTION

VEIN ZONE f #2)narrow qtz-py-cpy zones in intermediate tuff; mineralized sections are carbonatizedand show a licrht areenish sericitization/silicification; pyrite often has a coarsegranular fractmental aspect as in previous holes. Discrete mineralized sectionsare as follows :

1/2 in at 254 ft.1/2 in at 254.5 ft.3 in at 255.5 ft.1/2 in at 256.5 ft.1/2 in at 259 ft.

INTERMEDIATE LAPILLI AND BLOCK TUFF268-269 ft atz-chl porphyry as 160-172 ft.275.5 ft 2 in. qtz-py vein zone at 45" to c. a.280 ft weak schistosity at 45 0 to c. a.285 ft 2 in. fragment of arevish. v.f .q, cherty rhvolitic material287-291 ft minor qtz - py veinina and accompanyina lioht areenish sericitization

VEIN ZONE (#1)sheared, mineralized zone in fine-grained intermediate tuff and chloritic tuff.There is locally intense shearincr - liaht areenish silicification/sericitizationand some carbonatization. Silicification has been very intense in some sectionsgiving rock a faint, ghost-like lamination.

292-293 ft qtz-carb zone with intense areenish chert-like silicification and1 in. ouartz-py-cpy vein

295 ft 1 in. qtz-pv-cpy vein

INTERMEDIATE HICOCK TOFFfragments of qtz-chl porphyry and feldspar porphyry are aenerally vague andindistinct

311-312 ft 34 quartr.-py material315 ft schistosity at 40" to c. a., there is some fracturing and qtz-carb

veinina over most of this sectionEND OF HOLE

Sample No. From To Length

l

ls

l

l

l

l

l

l

APPENDIX C

DRILL SECTIONS: HOLES 81-1 to 81-13

metres 0+5OS 0+25S Baseline 0+25N 0+5ON

me t r e s 81-1,-50 0

J+OOEjO+SOSTrenchO.20471Oft.

LEGEND

PRECAMBRIAN

Diabase, mafic dikes

Quartz ± Feldspar Porphyry

Chemical and Tuffaceous Interflow Metasediments 4a: chert, siliceous sediments 4b: iron formation 4cs sericitic-chloritic tuffaceous sediments

Ultramafic Metayolcanics

Intermediate Metavolcanics-"Skead Pyroclastics"2O: massive and porphyritic lava

BHi chloritic tuff, dacite tuff ^2ffi| feldspar porphyritic crystal tuff[T—Tjandesific to dacitic, often feldspar porphyritic l±±J lapilli and block tuff

|2f; j cherty tuff, chert; pyritic

Mafic Metavolcanics-"Catherine Basalts"

B Vein Zone : qtr-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.0 oz. Au per ton X t rue width (ft.)

fS Schistosity

S S Bedding, indicating tops

Hole N-1 proj. to section

M/

YVANEX-WINDJAMMER J.V.

BRISCOE- BRYCE PROPERTYDIAMOND DRILL SECTION

HOLE 81-1l H. C-4O9

l -- 5OOW.E.BreretonGCS LtdAug. I98I

MPH Consulting Limited

metres O* 50S 0+ 25S Baseline 0 + 25N 0 + 50N

me t r es

— O

81-2- 500 2+OOE, O*SOS

— -25

—-5O

——75

Looking west

——IOO

2d

2c

2e

LEGEND

PRECAMBRIAN

10 l Diabase, mafic dikes

Quartz :t Feldspar Porphyry

Chemical and Tuffaceous Interflow Metasediments 4a: chert, s iliceous sediments 4b: iron formation 4C! sericitic-chloritic tuffaceous sediments

Ultramafic Metavolcanicsf

Intermediate Metavolcanics -"Skead Pyroclastics" 2a: massive and porphyritic lava

| chloritic tuff, dacite tuff feldspar porphyritic crystal tuff andesitic to dacitic, often feldspar porphyriticlapilli and block tuff cherty tuff, chert; pyritic


V Vein Zone: qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.O oz. Au per ton / true width (ft.)

Schistosity

f f Bedding, indicating tops


BRISCOE-BRYCE PROPERTYDIAMOND DRILL SECTION

HOLE 81-2Propel K* C-4O9

: 5OODraw.**

W. E.Breretoni: GCS L td

Aug. 1981


metres O*25 S Baseline 25N

me t r es

—— O

81 - 3 - 500 3+08E, 0+25S

Q

0 + 50N 0 + 75N

— -25

— -50

79.1 m.

——75

Looking west

——100

LEGEND

PRECAMBRIAN



Chemical and Tuffaceous Interflow Metasediments 4a: chert, siliceous sediments 46s iron formation 4c! sericitic-chloritic tuffaceous sediments


Intermediate Metavolcanics -"Skead Pyroclastics"2a: massive and porphyritic lava

@fl chloritic tuff, dacite tuff

jjZjtfj feldspar porphyritic crystal tuff

\ 9 l andesitic to dacitic, often feldspar porphyritic Ke'l lapilli and block tuff

\2f'-\ cherty tuff, chert; pyritic


B Vein Zone : qtz-carbipy, cpy, Au, sp, chl, hem, ser

O.8O/2.0 oz. Au per ton / t rue width (ft.)

jf Schistosity

S S Bedding, indicating fops



HOLE 81-3Cr.|.et M* C-4O9

l -' 5OOW.E.Brerefon

i: GCS LtdOn A ug. I 98I


m e tr es

— O

metres O * 25 S

Creek

Baseline

81-4,-55*4+055,0+155

0+25N 0 + 50N 0 + 75N

— -25

— -5O

—75

Looking west

— IOO

,0.73 Au; 0.56 Ag ; Q.44% Cu/.S ft. ,1.20XoZnX0.8ft.

61 m.

!

LEGEND

PRECAMBRIAN


Quartz ±. Feldspar Porphyry

Chemical and Tuffaceous Interflow Metasediments 4a: chert, siliceous sediments Ab5 iron formation 4cs sericitic-chloritic tuffaceous sediments


Intermediate Metavolcanics-"Skead Pyroclastics' 2a: massive and porphyritic lava

[chloritic tuff, dacite tuff S feldspar porphyritic crystal tuff -nandesitic to dacitic, often feldspar porphyritic

__l lapilli and block tuff |2f; | cherty tuff, chert; pyritic

Mafic Metavolcanics-"Catherine Basalts'

m Vein Zone: qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.0 oz. Au per ton X true width (ft.)

Schistosity




HOLE 81-4M* C-4O9

Safe, -' 5OO

1d

W.E.BreretonGCS Ltd

DM. Aug. I98I


metres 0+25 S Baseline 0+25N 0 + 50N 0 + 75IM 1+OON

m etr e s

8I-5, -500 5+OOE,0+25S

.O creek

—— -25

56.1m

— -5O

——75

Looking west

——loo

0.196 / 3 75 ft. intense greenish sericitization

10

LEGEND

PRECAMBRIAN


Quartz it Feldspar Porphyry

Chemical and Tuffaceous Interflow Metasediments 4a: chert, siliceous sediments 4b: i ron formation

sericitic-chloritic tuffaceous sediments


Intermediate Metavolcanics-"Skead Pyroclastics" 2o! massive and porphyritic lava

f2!c : l chloritic tuff, dacite tuff |.233-| feldspar porphyritic crystal tuff\ 9 l andesitic to dacitic, often feldspar porphyritic K8'! lapilli and block tuff|2f; | cherty tuff, chert; pyritic


M Vein Zone: qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.O oz. Au per ton / t rue width (ft.)

Schistosity


YVANEX-WINDJAMMER JY


HOLE 81 -5 At H. C-409 WE Brereton

GCS Ltd| DM* Aug. I98I


metres 2 + 25S 2 + OOS 75S H-5OS 1+25S

me t r es Outcrop - 2

— O

81-6,-50*2 + 50W, 2+15S

/

—— -25 Otz-carb veining 1-2"Xo py

—— -50

Outcrop - 2

2cThin py veinlets

2d

2c

2d

2e99.4m.

LEGEND

PRECAMBRIAN



Chemical and Tuffaceous Interflow Metasediments 4a: c hert, siliceous sediments 41^ i ron formation 4C' sericitic-chloritic tuffaceous sediments

Ultramafic Metavolcanics

Intermediate Metavolcanics -"Skead Pyroclastics'2.Q' massive and porphyritic lava

[chloritic tuff, dacite tuff (feldspar porphyritic crystal tuff landesitic to dacitic, often feldspar porphyritic

*~ lapilli and block tuff12f: | cherty tuff, chert; pyritic


O Vein Zone: qtz-carb±py, cpy, Au^ sp, chl, hem, ser

o.eo/2.0 oz. Au per ton X t rue width (ft.)

Schistosity


———75

Looking west

——IOO



HOLE 81-6K* C-409

l -- 500W.E.BrerefonGCS Ltd

On A ug. I98I


metres 31-75N 4 + OON 4f 25N 4 + 5ON 4 + 75N

re s

2 outcrop 81-9,-5O0 O 5-f-OOW, 3-fSON

— -25

Skead Pyroclastics

-50

——75

Interflow Metasediments

98.8m.

l

Catherine Basalts

IO-25% py as 1 -3cm. bands

LEGEND

PRECAMBRIAN



Chemical and Tuffaceous Interflow Metasediments' 4a: c hert, siliceous sediments 45s i ron formation 4C! sericitic-chloritic tuffaceous sediments

Ultramafic Metavolcanics*

Intermediate Metavolcanics -"Skead Pyroclastics"JSSjffi massive and porphyritic lava2c: chloritic tuff, dacite tuff2d: feldspar porphyritic crystal tuff

rr—n andesitic to dacitic, often feldspar porphyriticl lapilli and block tuff

|2f: |cherty tuff, chert; pyritic


O Vein Zone: qtz-carb±py, cpy, Au, sp, cbl, hem, ser

O.8O/2.O oz. Au per ton X true width (ft.)

Schistosity

S f Bedding, indicating tops

Looking west

—— IOO


8RISCOE-BRYCE PROPERTYDIAMOND DRILL SECTION

HOLE 81-9RK C-4O9

Scab: l 5OO1 i

'r W.E.Breretoni: GCS Ltd

0*n Aug. I98I


metres 1+5OS + OOS O-r5OS Baseline O + 50N OON

m et re s

— O

8I-IO,-5O0 Q4i-5OE,H-5OS

— -5O

— -IOO

———I5O

Looking west

Otz-carb ± py, cpy veins

— 200

LEGEND

PRECAMBRIAN



Chemical and Tuffaceous Interflow Metasediments 4fl: c hert, siliceous sediments

iron formation sericitic-chloritic tuffaceous sediments


Intermediate Metavolcanics -"Skead Pyroclastics' 2o: massive and porphyritic lava

\2G'\ chloritic tuff, dacite tuff ^Era feldspar porphyritic crystal tuff l~ l andesitic to dacitic, often feldspar porphyritic

l lapilli and block tuff cherty tuff, chert; pyritic

Mafic Metavolcanics-"Catherine Basalts'

O Vein Zone: qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.80/2.O oz. Au per ton X true width (ft.)

Schistosity

f S Bedding, indicating tops



HOLE 81-10C-4O9l-' IOOO1,

WE Brtrttoni. GCS Ltd

DM., Aug. I98I


me t re s

— O

metres O * 75 S

8I-II.-500 6 + OOE , 0 + 80S

.Q.

O*50 S 0+25S Baseline 0 + 25N

VLF Conductor

— -25

--5O

——75

—— IOO

2d

1-2 cm q tz- py veins-

Looking west

136.0m

LEGEND

PRECAMBRIAN


Quartz i: Feldspar Porphyry

Chemical and Tuffaceous Interflow Metasediments 4a: chert, siliceous sediments 4lX iron formation 4c* sericitic-chloritic tuffaceous sediments

Ultramafic Metavolcanics4

Intermediate Metavolcanics-"Skead Pyroclastics' 2a: massive and porphyritic lava

chloritic tuff, dacite tuff feldspar porphyritic crystal tuffandesitic to dacitic, often feldspar porphyritic lapilli and block tuffcherty tuff, chert; pyritic


m Vein Zone; qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.O oz. Au per ton f true width (ft.)

Schistosity




HOLE 81-11C-4O9l: 500

* 1k

W.E.Br.r.tonGCS Ltd

Bm. Aug. I98I


metres 0+75 S O* 50 S 0 + 25S Baseline

me t r e s

81-12,12a,- 500 7+OOE,0*40S

— -25

—— -50

———75

Hole 81 -12 (abandoned in overburden at 46.6m.)

qtz - py - ser * fuschite (

0.055/1,0 ft.

87.5m.

Looking west i

—IOO

LEGEND

PRECAMBRIAN


Quartz it Feldspar Porphyry

Chemical and Tuffaceous Interflow Metasediments4a: c hert, siliceous sediments

iron formation

4c: sericitic -chloritic tuffaceous sediments

Ultramafic Metavolcanicsm

Intermediate Metavolcanics -"Skead Pyroclastics 2a: massive and porphyritic lava jg^ chloritic tuff, dacite tuff [2dj feldspar porphyritic crystal tuffrL i andesitic to docitic, often feldspar porphyritic LZe*| iniiii and block tuff

m| cherty tuff, chert; pyritic

Mafic Metavolcanics -"Catherine Basalts"

M Vein Zone: qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.O oz. Au per ton / true width (ft.)

Schistosity

f f Bedding, indicating tops


BRISCOE-BRYCE PROPERTYDUMOND DRILL SECTION

HOLE 81-12,12aC-4O91 = 500

1 l

W.E.BrtrttpnGCS Ltd

Orti Aug. I98I


metres O*75S O* 50 S 0*258 Baseline 0+25N O-i-SON

me tr e s

—25

-5O

—75

81 - 13 - 5O0 8 + OOE , 0+40S

J3

Looking west99.0m.

— IOO

LEGEND

PRECAMBRIAN



Chemical and Tuffaceous Interflow Metasediments 4a: chert, siliceous sediments 4b* i ron formation 4C: sericitic-chloritic tuffaceous sediments


Intermediate Metavolcanics -"Skead Pyroclastics'2.Q- massive and porphyritic lava

(chloritic tuff, dacite tuff

[feldspar porphyritic crystal tufflandesitic to dacitic, often feldspar porphyritic l lapilli and block tuffj Cherty tuff, Chert, pyritic

quo--*? crystal tuff

m Vein Zone; qtz-carb±py, cpy, Au, sp, chl, hem, ser

O.8O/2.0 oz. Au per ton / true width (ft.)

Schistosity




HOLE 81-13C- 4091:500

Drawn* ib 1 m

W.E.BrtretonGCS LtdAug. 1981


APPENDIX D

PHOTOMICROGRAPHS

lUpper Left; Hole 81-2, No. l Vein, 340.8 ft. '

Subhedral to massive pyrite (light grey) with chalcopyrite (light l

yellow-grey) and siliceous gangue (black). Butter-yellow, angular

grain in centre of photo is gold. This mode of occurrence as dis- |

crete grains within chalcopyrite is characteristic of all of the mm

gold grains observed in hole 2. Gold grain measures approximately

100 microns by 50 microns (l micron ** 0 .001 millimeter). l

l

l

Upper Right and Bottom

Enlargements of above gold grain. In bottom photoi note how chal

copyrite penetrates fissure in pyrite while the gold grain ter

minates at the beginning of the fracture. Gold grain measures 100 l

microns by 50 microns in both cases.

l

l

l

l

l

l

l

l

l

"X

. mmm-

, illl

ll ^^Upper^J..eft1: Hole 81-2, No. l Vein Zone, 340.8 ft^

H Another, more rounded gold grain (butter-yellow) associated with

~ chalcopyrite (yellowish-grey) filling interstice between pyrite

B grain (grey). Grain measures approximately 18 microns by 8

microns.

lm Upper Right; Hole 81-9, Contact Zone, 148 ft.

Sub-rounded gold grain (butter-yellow) in sphalerite (medium grey)

l with subhedral to anhedral pyrite (grey-white) and siliceous

gangue (grey-black). Gold grain measures approximately 30 microns

J| by 20 microns.

l

l

l

l

l

l

l

l

l

l

l

Cam

pbel

l Fa

ult

Fela

spar

Por

phyr

y

quar

tz c

ryst

al a

sh t

uff,

carb

oniti

zed,

chl

oriti

tized

l

poss

ible

X ve

in of

fset

?

NO. 2

VEI

N Z

ON

EBR

ISCO

E-BR

YCE

NO. l

VEIN

ZO

NE

['[Co

ntac

t Zo

ne-5

5" 2

95 F

T—

9

5792

15

l \

l [5

7921

8^,.

•^ J

^578263,

-\

iaBR

YCE

TWP

2ft

qua

rtz-s

ulph

ide

in zo

ne

Au

Cont

act

Zone

Cath

erin

e G

roup

Bas

alt

Con.

IV

LE

GE

ND

VLF

-EM

D

ER

IVA

TIV

E

MA

P

Instr

urt

enf:

G

EO

NlC

S

EM

- 16

Sta

tion

:

SE

AT

TLE

W

AS

HIN

GT

ON

, F

RE

QU

EN

CY

le

-6

KH

z

366

FT

.0.1

0 to

0.1

8 oz

. ^

r\A

uXto

n.

I070

Cu\

\ (

^^

^ '

in na

rrow

q.

v.

Skea

d G

roup

Pyr

ocla

stic

s

410

VL

F-E

M

FIR

ST

D

ER

IVA

TIV

E

(Frc

r.

Inph

ase

Val

ues)

-10

CO

NTO

UR

IN

TE

RV

AL

(IO

QXo)

10C

ON

DU

CTO

R

AX

IS

WIT

H

DE

PT

H

(met

res)

TO

WN

SH

IP

BO

UN

DA

RY

CO

NC

ES

SIO

N

BO

UN

DA

RY

.—

LOT

LI

NE

__

. C

LA

IM

LIN

E

LA

KE

CR

EE

K

(Arr

ow

Indi

cate

s F

low

)

\AA

/ FA

ULT

AN

OM

ALO

US

IN

DU

CE

D

PO

LAR

IZA

TIO

N

ZON

E

UJ

^^P

- R

EP

OR

TE

D

QU

AR

TZ

-SU

LP

HID

E ±

GO

LD

OC

CU

RR

EN

CE

GE

OLO

GIC

AL

CO

NTA

CT

0.15

to

0.30

oz.

in

6 in

ch q

.v.81

-8

314

FT

DIA

MO

ND

D

RIL

L H

OLE

, 19

81;

com

plet

ed,

prop

osed

YVAN

EX -

WIN

DJAM

MER

J.V

BR

ISC

OE

- B

RY

CE

P

RO

PE

RT

Y

VLF-

EM

FIRS

T DE

RIVA

TIVE

AND

EX

PLOR

ATIO

N CO

MPILA

TION

Not

e U

pdat

ed

Nov.

81

Jan.

82

By

D. J

ON

ES

/W.B

RE

RE

TO

NPr

ojec

t No

: C

40

9

Date

: JA

NU

AR

Y, 1

981

MPH

C

onsu

lting

Lim

ited

O M

eP

8/-

41P89NE0046

63.3987

BRYCE

MA

P A

RE

AC

LAIM

A

RE

A

5792

I6|2

5696

i 25

^94

1256

.9,3

;.

25

i95

|feg

^ 5792

I5\"

J57

42'8

1578

265

J578

E66

I \

TRENCH # 6

CLAIM MAP

TRENCH

Bed

rock

no

t ex

pose

d

072

oz

Au, 0

.30

oz

Ag,

I56

o7c,

Cu

O 0

02

oz

Au

0.0

02

oz

A

uB

edro

ck

not

-exp

osed

N0.

2 SH

AFT

0.0

802

Au-—

—^.

^^

0.0

4/O

7m

——

04/O

.Sm

Nil

Au

TO 0

05/0

.45 m

0.6

3 o

z A

u. 0

.36

oz

Ag

Bed

rock

no

t ex

pose

d

0.2

6 o

z A

u,O

.I2oz

Ag,0

.52

0XoC

u

O 0

05

oz

Au

0.0

2 o

z A

u.0

.52

% C

uB

edro

ck

not

exp

ose

d

Sca

le

—

l- 10

02

3 4

5 6"

89

'0

Qua

rtz

vein

ing

Qua

rtz

bre

ccia

, m

inor

su

lphi

des

Mas

sive

py

rite

band

Bas

ic

volc

an

ics

Fol

iatio

n

Sel

ecte

d gr

ab

sam

ple

(oz

Au

,t o

z A

g,i

0XoC

u)

Chi

p sa

mpl

e (o

z. A

u/m

)

DETAILED SAMPLING

NO.

2 SHAFT

ZONE

OU

TC

RO

P

AR

EA

INT

ER

ME

DIA

TE

^

ME

TA

VO

LC

AN

ICS

L-

E

GM

P-7

B40

", 1

69'

TR

EN

CH

4

TR

EN

CH

(

5M

T

RE

NC

H7o

z A

uX2.

6m l

C

f

^^

v

QM

P-9

\l

45",

I2

6\

\ \T

RE

NC

H

TR

EN

CH

\ \

2 l

BA

SE

LIN

E

O

MP

-7A

550,

abon

.311

MP

-6

450,

156

MP

-450

0, 21

0'

450,

166

5910

0N

-345

", 2

O2.

6'6

7-6

59",

37

2(n

o in

form

atio

n av

aila

ble

)

N-4

450,

205

N-6

40",

218

'

75

-740",

198

.5'

N

D

Quart

z -

pyrite

ve

in

zone

(s

urf

ace)

Surf

ace

p

roje

ctio

n

of

shea

r i

vein

zo

neba

sed

on

prev

ious

dr

illin

g(I

5)~

dep

th

to su

rface

of

vert

ica

l pro

ject

ion

Pre

viou

s D

iam

ond

Dril

l H

ole

M N

oran

do

Min

es

Ltd

M

P M

iner

al

Pro

ject

s L

td.

75

Rip

V

on

Win

kel

Syn

dica

te76

T

riho

pe

M

inin

g

Au

valu

e (o

z pe

r to

n /s

am

ple

w

idth

in

m

etre

s re

po

rte

d

by

prev

ious

o

pe

rato

rs)

Sam

plin

g R

esul

t -

1980

VL

F-E

M

con

du

cto

r ax

es

Ano

mal

ous

Induce

d

Po

larizC

tion

Z

one

Mag

netic

co

ntou

r

Infe

rred 'fa

ult

or

shea

r zo

ne

Pro

pose

d D

iam

ond

Drill

Hol

e -

1981

"A"

/\

Sur

face

or

esho

ot

indi

cate

d by

pr

evio

us

sam

plin

g

tIC

ON

SON

/^

Bed

rock

no

t ex

pose

d

0.2

6 o

z A

u,0.

12oz

Ag

,0.5

20X

oCu

O 0

05

oz

Au

0.0

2 o

z A

u.0

.52%

Cu

Bed

rock

no

t ex

pose

d

Scale

—

h

100

l 23

45

6 7

a 9

' C

Qua

rtz

vem

mg

Qua

rtz

bre

ccia

, m

inor

su

lphi

des

Mas

sive

pyr

ite

band

Bas

ic

volc

an

ics

Folia

tion

Sele

cted

grab

sa

mpl

e (o

z A

u,i o

z A

g,i*y

0 C

u)

Chi

p sa

mpl

e (o

z, A

u/m

)

DETAILED SAMPLING

NO.

2 SHAFT

ZONE

OU

TC

RO

P

AR

EA

INT

ER

ME

DIA

TE

^ M

ET

AV

OL

CA

NIC

S

MP

-345

s, 1

96M

P-7

B40

", 1

69'

75-4

-45

", 1

43'

N-5

35

0,

219

TR

EN

CH

4

TR

EN

CH

f

TR

EN

CH

II

7oi

Au

/Zfim

.V

6M

P-8

40

0,

M7

NO

. l

SH

AF

T

BA

SE

LIN

E

'O7

5-5

-48

",9

6.8

MP

-7A

550,

abo

n.Jl

'M

P-6

45",

156

MP

-450

", 2

10'

N-2

450,

209

IMP

-245

", 16

6 59

10

0N

-345

0, 20

2.6

67

-65

9",

37

2(n

o in

form

atio

n ava

ilable

)

N-4

45",

205

75

-740

". 1

98.5

'

L-

0.8

0.27

oi

Au/?

6m

l l l

S94

00-

\

81-1

200S

N

Qua

rtz -

py

rite

vein

zo

ne

(sur

face

)

Sur

face

pr

ojec

tion

of

shea

r 7

vein

zo

neba

sed

on

prev

ious

dr

illin

g(1

5)-

de

pth

to

surf

ace

of v

ertic

al

proj

ectio

n

Pre

viou

s D

iam

ond

Drill

Hol

e N

Nor

ando

M

ines

L

td.

MP

Min

eral

P

roje

cts

Ltd

.75

R

ip

von

Win

kel

Syn

dica

te7

6

Trihope

Min

ing

Au

valu

e (o

z pe

r to

n /s

am

ple

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1

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and windjammer power and gas ltd. - ontario · ling programme completed on the briscoe-bryce gold...

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