: other l ] hole no, footage date1987 for carlson mines ltd, and black gregor explorations ltd,...

42D16SE8a25 18 LORNA LAKE

DIAMOND DRILLING010

Area: Lorna Lake Report No: 10

WORK PERFORMED FOR: carlson Mines Ltd

RECORDED HOLDER: SAME As ABOVE [ x ]

: OTHER l ]

CLAIM No,668310668310688310668301668333668331668110827335

HOLE No,C-87-1 C-87-2 C-87-3 C-87-4 C-87-5 C-87-6 C-87-7 C-87-8

FOOTAGE

124m 99m99m99m 121m99m 172m98m

DATE

Feb/87 Mar/87Mar/87 Mar/87 Mar/87 Mar/87 Mar/87 Mar/87

NOTE

ft) (D (D d) (D (D (D

NOTES: ( 1) #249-252 (filed in August/87)

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ONTARIO GEOLOG.CAL SURVEY

J UN l 7 'l987

RECEIVED

DIAMOND DRILL REPORT

WIRE LAKE GOLD PROSPECT

MARATHON AREA, ONTARIO

1987

FOR

CARLSON MINES LTD,

AND

BLACK GREGOR EXPLORATIONS LTD,

Toronto, Ontario

April, 1987

J.P. Rollinson, B.Se.

D.T. Hillier, B.Se.

MPH Consulting Limited

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SUMMARY

A gold exploration program Involving 915.5 meters of diamond drilling in

8 holes has been completed on a 16,000 acre property in the Marathon

Area of north-central Ontario for Carlson Mines Ltd. and Black Gregor

Explorations Ltd.

The 1987 drilling was carried out in two adjoining areas on the property.

Holes l through 7 were drilled in the general vicinity of Wire Lake and

tested surface gold showings, geophysical conductors and geochemical

anomalies located during previous exploration programs. Drill hole 8,

located approximately 2 km to the southeast of Wire Lake, tested a strong

airborne EM conductor that was precisely located during follow-up ground

geophysical surveys.

Anomalous gold intersections are summarized as follows:

Hole No.

C87-1

Collar (m)

L2+50S, 1+48E

C87-2 L2+50S, 0+80W

C87-5 L1+70S, 1+70E

C87-6 L2+75S, 2+40E

From(m)

4.885.30

11.9513.0159.74

65.64

47.9949.3753.0753.9054.4064.9479.59

21.9024.9027.0031.6335.2138.1742.18

To(m)

5.306.53

12.1913.9560.11

66.87

49.3750.1653.9054.4054.9366.1080.09

22.6625.1827.8332.6535.8838.8043.15

Interval(m)

0.421.230.240.940.37

1.23

1.380.790.830.500.531.160.50

0.760.280.831.020.670.630.97

Au ppb oz/ton

125917781331190239

4350

722181

1483168516262219

924189168163404

1133450

.047

.052

.047

.140

.021

.047

.022

.027


Hole No.

C87-7

Collar(m)

Ll+COS, 2+50E

From(m)

44.8745.6949.13

86.0089.7391.3893.6094.1796.47102.70103.66108.45109.85

To(m)

45.6947.1249.55

86.7090.5091.6394.1795.4696.93103.56104.32109.38110.64

Interval(m)

0.821.430.42

0.700.770.330.571,290.460.860.660.930.79

Au ppb

13582995844

1063615264694534182182154153413

oz/ton

.033

.092

.028

.031

Although no ore-grade intersections were obtained, it is concluded that

results from this first round of drilling are encouraging and more work

is clearly warranted.

Hole C87-2 which tested a geophysical conductor with a strike length in

excess of 400 meters, returned a value of 0.14 oz/ton Au over a core

length of 1.23 m in sheared altered pyritic interflow sediments. This

zone represents a priority target for future drilling. Several distinct

ly anomalous gold zones were intersected in holes l, 5, 6 and 7 in part

associated with a zone of strong shearing and alteration and surface soil

geochemical anomalies. Further drilling is also recommended for this

area.

The drilling failed to encounter gold values as high as those in surface

showings (1.2 oz/ton in quartz veins, 0.45 oz/ton in sheared interflow

sediments) and further work, primarily in the form of surface stripping,

is required in these areas.

A program of further linecutting, geophysical surveys, geochemical sur

veys, geological mapping and prospecting and additional diamond drilling

totalling 3,000 m is recommended to further evaluate the economic poten

tial of the Carlson-Black Gregor property. This work is budgeted at

$1,000,000.

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42D16SE8825 le LORNA LAKE

TABLE OF CONTENTS

l .0 INTRODUCTION

2.0 LOCATION, ACCESS AND INFRASTRUCTURE

3.0 PROPERTY

4.0 HISTORY AND PREVIOUS WORK

5.0 REGIONAL GEOLOGY AND MINERALIZATION

5.1 Regional Geology

5.2 Mineralization

6.0 PROPERTY GEOLOGY AND MINERALIZATION

6.1 Property Geology

6.2 Mineralization

7.0 DIAMOND DRILLING PROGRAM - 1987

7.1 Drilling

7.2 Assaying

8.0 DRILL RESULTS - 1987

8.1 Summary

8.2 Detailed Discussion, Drill Holes C87-1 to C87-8

9.0 CONCLUSIONS AND RECOMMENDATIONS

References

APPENDIX A Assay Results

APPENDIX B Drill Logs

APPENDIX C Drill Sections

010C

17

17

19

23

23

25

26

26

26

28

28

30

33


1.0 INTRODUCTION

This report presents a summary of the results of a diamond drilling

program on the Wire Lake gold prospect in the Marathon area of north-

central Ontario carried out during February and March, 1987 on behalf of

Carlson Mines Ltd. and Black Gregor Explorations Ltd.

Seven of the eight holes were concentrated on the so-called "discovery

zone" located just south of Wire Lake. An additional hole was drilled

approximately 2 km to the southwest of Wire Lake to test a strong MaxMin

II EM anomaly.

Surface gold showings in the Wire Lake area indicate that gold occurs In

quartz-sulphide veins and also in sheared and silicified Interflow sedi

ments, both within mafic volcanics.

Results of exploration work previously carried out on the Carlson-Black

Gregor property are summarized in this report. The geophysical survey

results, on which the present drilling was largely based, are being pre

sented to Carlson-Black Gregor under separate cover.

This report describes the drilling program carried out, outlines explora

tion results to date and presents recommendations for further exploration

in the property area.


- 2 -

2.0 LOCATION. ACCESS AND INFRASTRUCTURE

As seen in Figure l, the overall property is centered approximately 20 km

northeast of the town of Marathon on the north shore of Lake Superior in

the Thunder Bay district of north-central Ontario.

The Wire Lake area, site of the present drilling, is located in the

southeast portion of the property.

The Hemlo gold deposits are centred some 20 km to the southeast of the

Carlson claims, while the Manitouwadge base metals mining camp is located

30 km northeast of the present property.

The property area is generally rugged with a high proportion of rock out

crop. Some ridges are in excess of 1,800 ft above mean sea-level.

The numerous lakes on the property such ae Cirrus and Goodchild provide

convenient landing sites for float aircraft from bases at White River,

Pays Plat, etc. The creeks on the property are indicated to be variably

negotiable by canoe. Helicopters are available for charter at Marathon.

The Trans-Canada Highway, No. 17, passes to the south of the property,

through Hemlo and just north of Marathon, as does the main line of the

Canadian Pacific Railway. There is now direct air service between Mara

thon and Toronto, Ontario.

The Terrace Bay-Man!touwadge hydroelectric power transmission line cros

ses the north portion of the Carlson property.

A gravel road extends from Highway 17 at Marathon to Mile 16 on the Pic

River. Tractor roads from there provide access to the property and

extend along Goodchild Creek past Goodchild Lake as far north as Cirrus

Creek. A number of variably overgrown logging roads are also present in

the area.

PROPERTY LOCATION

REGIONAL LOCATION MAPSCALE

10 IS 10 is

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PROPERTY LOCATION

DETAILED LOCATION MAP

CARLSON MINES LIMITEDMARATHON PROJECT

LOCATIONI NO: C -665

No: FiflUf*

W.E.Br*r*tonMPH

Ftbfuory, (90

MPH) MPH Consulting Limited


- 3 -

The main local centre of service and supply Is the town of Marathon. The

population here has recently increased from 2,500 to 4,000 reflecting

developments at Hemlo and is expected to double again by the next decade.

Generally all manner of exploration services such as food, fuel,

supplies, aircraft, etc. are available locally.

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- 4 -

3.0 PROPERTY

The property totals 407 contiguous unpatented mining claims aggregating

approximately 16,208 acres in the areas of Cirrus Lake, Seeley Lake and

Lorna Lake in the Terrace Bay administrative district, Thunder Bay Mining

Division, Ontario. The claims are more properly described as:

Claim No. Recorded

TB 663801-663804 TB 653716-653717 TB 689162-689176 TB 689205-689207 TB 689216-689219

TB 668096-668103 TB 668108-668111 TB 668119-668121 TB 668134-668136 TB 668138-668139 TB 683728-683729 TB 683733-683734 TB 683736-683739

TB 708146-708148 TB 708151-708153 TB 708164-708169 TB 708175-708177 TB 708098-708101 TB 708110-708113 TB 708122-708125 TB 708134-708135

TB 708852-708901 TB 709691-709703 TB 708136-708145 TB 708178-708195 TB 709391-709400 TB 709601-709610 TB 709649-709661

November 15, 1982 January 24, 1983 January 26, 1983 January 26, 1983 January 26, 1983

28 claims

February 11, 1983 February 11, 1983 February 11, 1983 February 11, 1983 February 11, 1983 February 11, 1983 February 11, 1983 February 11, 1983

33 claims

February 25, 1983 February 25, 1983 February 25, 1983 February 25, 1983 February 25, 1983 February 25, 1983 February 25, 1983 February 25, 1983

29 claims

March 30, 1983 March 30, 1983 March 30, 1983 March 30, 1983 March 30, 1983 March 30, 1983 March 30, 1983

124 claims

Due

November 15, 1987 January 26, 1987 January 26, 1987 January 26, 1987 January 24, 1987

February February February February February February February February

February February February February February February February February

11, 198711, 198711, 198711, 198711, 198711, 198711, 198711, 1987

25, 198725, 198725, 198725, 198725, 198725, 198725, 198725, 1987

March 30, 1987March 30, 1987March 30, 1987March 30, 1987March 30, 1987March 30, 1987March 30, 1987

Days Due

(40) (40) (40) (40) (40)

(40) (40) (40) (40) (40) (40) (40) (40)

(40) (40) (40) (40) (40) (40) (40) (40)

(40) (40) (40) (40) (40) (40) (40)

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5

Claim No.

TB 724394-724417 TB 724424-724425 TB 724444-724453 TB 730289-730327

Recorded

June 23, 1983 June 23, 1983 June 23, 1983

_ June 23, 198375 claims

TB 827280-827317 TB 827318-827329 TB 827330-827339

December 14, 1984 December 14, 1984

__ December 14, 1984 60 claims

TB 798778-798795 TB 798710-798713 TB 798796-798800

March 26, 1985 March 26, 1985

__ March 26, 198527 claims

TB 838182-838192 TB 838194-838213

March 26, 1985 ^ March 26, 1985 31 claims

Due

June 23, 1987June 23, 1987June 23, 1987June 23, 1987

December 14, 1986December 14, 1986December 14, 1986

March 26, 1987March 26, 1987March 26, 1987

March 26, 1987 March 26, 1987

Days Due

(40) (40) (40) (40)

(40) (20) (20)

(20) (20) (20)

(20) (20)

The 8 diamond drill holes are located on the following claims:

C87-1, 2, 3

C87-4

C87-5.7

C87-6

C87-8

claim 668110

claim 668101

claim 668111

claim 668100

claim 827335

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6

4.0 HISTORY AND PREVIOUS WORK

Gold was first discovered in the Heron Bay greenstone belt as early as

1869, making it one of the earliest gold finds in Ontario. That year,

Indian prospector Moses Peekongay had found a gold showing near the Pic

River, not far south of what was to become the main CPR line.

A company that was already producing silver from a mine west of Lake

Superior, Silver Islet Mines, financed a shaft on the Peekongay prospect

in 1873, and while work was in progress a number of high grade samples of

both gold and silver was reportedly brought out. Not much in the way of

production was ever recorded and little more was done in the area until

the early 1920's.

At that time the manager of the CPR stop at Hemlo found a gold showing

just south of the main line on a property now owned by Bel-Air Resources.

The initial assay ran $67 per ton or about 2.57 oz gold. A crew was

assembled and a number of trenches dug, but the work was shortlived.

Although it is impossible to say for sure who first found the gold show

ing that eventually led to the discovery of the Hemlo deposits, this is

generally credited to an Indian prospector from Heron Bay, Peter Moses.

Moses showed the property to prospector Harry Oilman, who teamed up with

American L .G. Williams and staked the 11 claims that now host the Lac

Minerals portion of the deposit. In 1945, Oilman and Williams financed

and conducted what was the first serious work done in the area of the

discoveries, although they got back little in the way of assay results.

Work recorded that year included a limited program of trenching and

stripping with one of the trenches apparently missing the main zone by no

more than a few feet.

Various efforts over the intervening years by Lake Superior Gold Mines,

Teck-Hughes Gold Mines and others yielded only modest encouragement.

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This was the case until Hole C-76, collared on May 6, 1981, by Corona

Resources Ltd, cut a 10.5 ft section grading 0.209 oz gold per ton. This

turned out to be the Corona East Zone and its discovery ultimately

touched off one of the largest staking rushes in Canadian history.

The general area east of the Pic River encompassing the present Carlson

property has been prospected since at least the early 1920's. This work

was directed largely towards copper, copper-nickel and gold.

There has been a surprisingly small amount of assessment work recorded on

the Carlson-Black Gregor property. Some work in the immediate area

however is very relevant to the present claims.

Probably the most critical in this regard is work by Kerr Addison Mines

Limited in 1971 on a zone approximately | mile west of the No. 4 post of

present claim 663804 along the southwest boundary of the Carlson property

(Toronto Ministry of Natural Resources (TMNR drill report 33 - Seeley

Lake area.) The occurrence is located 2 miles due east of the 19 mile

post on the Pic River.

Kerr drilled 9 holes here totalling 1,013.2 ft on EM targets in the

extreme northeast corner of old claim 302250. The holes intersected

rhyolite, graphite tuff, greywacke, mafic agglomerates and andesite.

Of particular interest were their holes 4, 5, 6 and 7 which were all

drilled to the north on the same section under an old surface base metals

- gold showing ("Knut Kuhner Occurrence").

1i*1iiiiiliiiiiiiiit

- 8 -

Drill logs from Kerr Addison include the following assays:

Drill Hole Gore Length (m) AuCg/t) Zn(5S)

KP-71-4 11.9 .4 0.85Including 6.1 Trace 1.15KP-71-5 5.5 2.7 1.16Including 2.5 *5 .6 KP-71-6 3.2 2.2 1.12Including 1.5 4.1

* 0.16 oz per ton

The mineralization occurs as pyrrhotite, sphalerite and pyrite hosted in

"felsic volcanics".

The mineralized section in hole 4 is from 6-60.6 ft and is described as

"rhyolite, graphite"; 11-44 ft has 40% po, 10? py, 5% sp and tr cpy.

That in hole 6 is from 20.1 to 54.8 ft with variable po, py and cpy in

rhyolite.

Shell Canada Limited in 1975 filed the results of airborne magnetic and

electromagnetic (Aerodat) surveys which covered the area east of the Port

Coldwell complex extending across the Pic River and including a small,

west-central portion of the present Carlson property (TMNR file 2.2011).

The edge of the Port Coldwell alkaline complex shows up very clearly as a

broadly arcuate area of greatly increased magnetic activity. A north

west-striking diabase dike in the north portion of the survey area is

clearly reflected in the magnetic data. Some more localized magnetic

anomalies may represent pyrrhotite C+ magnetite) concentrations in the

volcanics .

There is no detailed EM interpretation but a large .number of anomalous

intercepts are indicated. A particularly large concentration of these is

present in the area of the old Kerr Addison zone and to the north of

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- 9 -

this. Shell apparently carried out further drilling in this area (5

holes ??) although no details are reported.

The geophysical trends tend to support the presence of an anticlinal fold

nose as mapped by the ODM in this area in that trends swing from north-

south in the south to more east-west in the north.

Teeshin Resources Ltd. in June, 1984 drilled 5 holes on present claims

469439, 469440 and 656714 (Figure 2) on the property immediately adjoin

ing to the south of the Kerr-Shell zone, although did not report any

assays (T-84 series; 1,165 ft, TMNR drill report 47 - Seeley Lake area).

The holes are summarized as follows:

Hole T84-1;

0-16

16 - 31

31 - 73.6

73.6 - 90

90 - 319.6

319.6 - 353

Hole T84-2;

0-8

8 - 249

Hole T84-3;

0-5

5-78

78 - 85.2

85.2 - 157

353 ft @ -45" W

Casing

Rhy tuff

Mainly sulphide-chert iron formation; to 90/S po with

chalco and pyrite

Mainly rhy tuff-sediment

Mainly basalt

Mudstone, mafic tuff, rhy tuff

249 ft @ -50 0 W

Casing

Basalt with some fsp por dykes

157 ft @ -50 0 W

Casing

Gabbro with some rhy tuff - sed

Sulphide-chert IF; mainly massive po ;f chert, pyrite

Rhy tuff-sed bx; some py

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- 10 -

Hole T84-4: 273 ft @ -50 0 W

0-21 Casing

14 - 64.5 Rhy tuff-sed

64.5 - 73 Sulphide-chert IF as above; to massive po ;f py,

tuff

73 - 273 Rhyolite tuff, sandstone, lamp dykes

Hole T84-5: 133 ft @ -50 0 W

0-7 Casing

7 - 72.6 Tuffaceous siltstone

72.6 - 77 Sulphide IF, massive po * chert, py, sed

77 - 133 Tuff, siltstone, mudstone

Homestake Mineral Development Company currently hold the old Kerr

chert ,

Addison

zone via an option from Gowganda Resources Inc. Homestake carried out a

mapping and sampling program and magnetometer survey in the summer of

1984 (TMNR file 2.7364).

The Homestake claims are indicated to be "situated in the nose of a

northeasterly plunging anticline whose core consists of felsic volcan-

iclastic rocks. Successively overlying these are graphitic argillites

and wackes, carbonatized graphitic mafic fragmentals and finally a thick

succession of variably carbonatized mafic to ultramafic volcanics with

minor intercalations of banded ironstone and argillitic sediments. A

unit including occasionally quartz porphyrite intermediate to felsic

flows and pyroclastics with minor intercalations of banded ironstone and

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sediments is present in the eastern portion of the property".

The banded iron formations are reported to be primarily of oxide

with some disseminations of pyrite and pyrrhotite.

facies

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- 11 -

Homestake view the Au-Zn-Cu zone drilled by Shell and Kerr Addison in the

southern portion of the property as "a small lens of silicified argillite

with nodular sulphides occurring within an argillite horizon in the

mafic-ultramafic sequence".

Examination of airborne geochemical surveys utilizing the SURTRACE tech

nique reveals a prominent airborne copper anomaly over the general Kerr

Addison zone area (Ontario Geological Survey, Study 25, MNR, 1983).

Also, there is reportedly a large lake bottom sediment geochemical

anomaly, indicated to be similar to that at Manitouwadge, in copper,

lead, zinc and mercury in Page Lake (G.S.C. Open File 746) immediately to

the east of the above showing. Carlson claim 663801 covers the southeast

extremity of Page Lake.

Westam Oil Ltd, in 1983-84 carried out a linecutting, Induced Polariza

tion surveying and diamond drilling program on the property immediately

to the southwest of the old Kerr Addison property. They drilled 3 holes

in February of 1984 on present claims 661861 and 661865 (Figure 2) to

test IP targets (TMNR drill report 46 - Seeley Lake area) . The holes are

summarized as follows:

Hole 1: 191 m @ -55" W

- mainly intermediate tuffaceous rocks with some rhyolite, lapilli

tuffs, garnetiferous mafic tuffs and lamp dykes.

- no apprec. sulphides, no assays.

Hole 2: 122 m @ -45 0 W

- tuffaceous sequence as above - mainly intermediate tuffs trending to

both rhyolite and mafic types.

- very little sulphides, no assays.

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Hole 3; 119 m @ -50" W

- virtually entirely rhyolitic tuff with narrow lamp dykes.

- locally to 5% sulphide, no assays.

With reference to the Kerr Addison-Teeshin drilling approximately l mile

to the northeast, it is interesting that there is an apparent transition

from a more volcanic-dominated environment on the Westam claims to more

of a sedimentary regime in the latter area.

Pelangio Larder Mines Limited carried out linecutting and magnetic sur

veys and geological mapping on a 19 claim property in the west-central

portion of the present property in 1983 (TMNR file 2.6060). The property

was indicated to be underlain mainly by intermediate to mafic volcanics

with some dacitic tuffs, cherty metasediments, banded iron formation,

agglomerate and brecciated rocks. The area appears to be structurally

complex in that both north-south and east-west strikes were recorded in a

relatively small area.

Pyrite-pyrrhotite was observed in the dacitic tuffs and cherty sediments

in amounts of up to 5%. The banded iron formation was indicated to be

primarily of oxide facies with only minor sulphides. Mafic C+ ultramafic

??) units on the property exhibit variable carbonate alteration and pos

sibly sericitization is indicated in the more felsic units.

Programs of detailed prospecting and sampling along with IP/resistivity

surveys were recommended to further evaluate the property.

Pennant Resources Limited in 1984 carried out airborne EM, magnetic and

VLF surveys on a 24 claim property in the Seeley Lake area surrounded on

three sides by the west-central portion of the present claims (TMNR file

2.7096). Line spacing was 1/16 mile with a north-south flight direction.

Ten to 14 conductors of 'bedrock -potential" were identified. It was

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- 13 -

further noted that "...,. the apparently non-fortnational short strike and

magnetic association characteristics of all the selected bedrock zones

points more favourably to massive sulphides. Conversely, the low calcu

lated conductances of the area are more discouraging to the prospects of

an economic massive sulphide deposit than that of gold".

Note that there is virtually no assessment work recorded on the main or

Lorna Lake portion of the Carlson property. There does not appear to

have been any drilling at all in the area.

Some copper-nickel exploration has been carried out immediately to the

west of the northern (Cirrus Lake) portion of the Carlson property. Much

of this was directed towards an old copper-nickel showing at a metavol-

canic-serpentinite contact 3 miles west of the property.

Pic Nickel Mines Limited in 1953-55 worked the above showing (TMNR drill

report 10 - Cirrus Lake area).

Fourteen holes were drilled with a total footage of 2,863 ft. Eleven of

these holes were concentrated in the immediate vicinity of the showing

with the remaining three spaced about 400 ft to the north and south of

the showing. Intersections of 100 ft and more of altered metavolcanis

rock were cut in the drillholes containing stringers and disseminations

of pyrrhotite, pyrite and chalcopyrite. In the drill logs the altered

metavolcanic rock is referred to as "rhyolitic rock". No assays are

available for these sections.

In 1954, Pic Nickel Mines Limited drilled another hole directed eastward

about 1,600 feet north and 200 feet west of the main showing and again

intersected altered mafic metavolcanic rock that contained stringers and

disseminations of pyrrhotite, pyrite and chalcopyrite. One section,

between 221.0 and 235 ft in the hole, contained sections that assayed

between 0.05 and 0.21 percent copper and 0.03 and 0.09 percent nickel.

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- 14 -

MacLeod Cockshutt Gold Mines Limited in 1954-55 carried out exploration

work in the above area (TMNR drill report 12, 13 - Cirrus Lake area).

Three holes were drilled in 1954 on eighteen claims straddling Cirrus

Creek about 2 i miles south of the Pic River. The holes were drilled

entirely in serpentinite and did not intersect the contact with the meta-

volcanics. No mineralization other than minor magnetite was encounter

ed.

Also in 1954, 4 holes with a total footage of about 1,000 ft were drilled

on 10 claims enclosing Louis Lake. The best section encountered was a

10-foot length of 0.8 percent copper.

In 1955, MacLeod-Cockshutt drilled an additional 5 holes with a total

length of about 1,124 ft on the Pic Nickel Mines property. An earlier

hole was deepened, l hole was spotted 100 ft east, 3 holes placed 800 ft

north and l hole put down 2,400 ft north of the main showing. None of

these holes intersected the metavolcanicserpentinite contact, but traces

of pyrrhotite and chalcopyrite were found in almost all the holes.

Inco Limited in 1963 again worked showings at the Louis Lake area serpen-

tinite-volcanic contact (TMNR drill report 14 - Cirrus Lake area).

Seven holes were drilled by them with a total length of about 3,000 ft.

Two holes were drilled near the main showing i mile northeast of Louis

Lake. The remaining 5 were located between 4,400 ft and 7,200 ft north

of the showing and 3 of these were completely within the serpentinite.

Of the remaining two holes, one intersected the metavolcanic-serpentinite

contact and cut about 20 ft of altered metavolcanic rock with sparsely

disseminated pyrite and pyrrhotite, and occasional stringers of sulphides

directly adjacent to the serpentinite contact. Values obtained in these

holes are unknown.

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Another occurrence of disseminated to massive sulphide mineralization at

the contact of the above serpentinite complex with surrounding volcanics

is to be found immediately west of Goodchild Lake. This area was worked

by Violamac Mines Limited in 1954 (TMNR drill report 11).

Mineralization consists of pyrrhotite, pyrite, and chalcopyrite as thin

seams and disseminations in silicified amphibolite in contact with the

serpentinite intrusion.

The highest values were registered in samples from the west end of the

zone where it becomes narrower. Values up to 2 percent copper, 0.5 per

cent nickel, and 2 ounces of silver per ton across widths of 8 feet have

been reported.

Five diamond drill holes, totalling about 2,000 ft in length, have been

drilled at various points along the silicified zone. Silicified raetavol-

canic rock, containing sparsely disseminated mineralization over narrow

widths, was intersected in all the holes.

Mexico Explorations Ltd, in 1969 held a property at the serpentinite-

volcanic contact area extending south from Louis Lake. They drilled 11

holes on various targets (TMNR drill report 15 - Cirrus Lake area). Some

holes cut pyrrhotite with graphite in the serpentinite-volcanic contact

zone. Others were entirely in ultramafics. No values are reported.

Descriptions of "obsidian" in drill logs probably refers to altered (sil

icified) volcanic contact zone material.

Since acquiring the present property, Carlson Mines Ltd, has carried out

an ongoing exploration program including airborne geophysical surveys,

ground geophysical surveys, geological mapping and prospecting and

geochemical surveys. Gold values in excess of l oz per ton were recorded

from narrow quartz veins and up to 0.45 oz per ton from sheared, silici

fied interflow sediments in the Wire Lake area in the course of this

l I l l l l l l l l l li l l i l i i

- 16 -

work. A prominent gold soil geochemical anomaly was encountered in the

showing area .

It was concluded that results of the above exploration were sufficiently

encouraging to warrant a first phase diamond drill evaluation of the

property. A program of 3,000 ft of B-size diamond drilling in 8 holes

was therefore recommended with drilling to commence in early February of

1987. The above drilling was completed and is the subject of this

report.

l I l l l l l l ll l l l l l l i i i

- 17 -

5.0 REGIONAL GEOLOGY AND MINERALIZATION

5 .1 Regional Geology

The Carlson property lies within a metavolcanic-metasedimentary seg

ment of the Wawa Subprovince of the Superior Structural Province of

the Canadian Shield. This portion of the Western Subprovince is

noteable for hosting the Heralo gold deposits.

Stratigraphically the volcanics and sediments in the Hemlo area are

tentatively subdivided into two groups; the southern, Piayter

Harbour group, and the northern, Heron Bay group. The division,

best distinguished in the west part of the area, is based on limited

chemical analyses and is apparently not as clearly defined in the

eastern half of the area (Muir, 1983). Muir (1984) describes the

rocks as follows:

"The Piayter Harbour Group consists largely of massive and vario

litic varieties of high iron tholeiitic basalt flows and pillowed

flows. Feeder dykes have locally been identified. A number of

relatively thin, intercalated, discontinuous units of intermediate

to felsic tuff and lapilli-tuff as well as siltstone were locally

found. Minor amounts of poorly banded chert, amphibolite, and

magnetite ironstone also occur in the west. Isolated lens-shaped

bodies (sills?) of pyroxenite and lherzolite are found within the

mafic flows in the Pulpwood Harbour area there are several very

thin units of altered graphitic mudstone which contain various

amounts and combinations of pyrrhotite, chalcopyrite, and pyrite.

The bulk of the Heron Bay Group comprised dacitic and rhyolitic

calc-alkalic pyroclastic breccia, tuff-breccia, lapilli-tuff, and

tuff; rocks of rhyolitic composition are minor and restricted to

the vicinity of Heron Bay. The remainder of the group consists of

calc-alkalic basalts as pyroclastic rocks, pillow breccia and some

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

- 18 -

tuff; rocks of rhyolitic composition are minor and restricted to

the vicinity of Heron Bay. The remainder of the group consists of

calc-alkalic basalts as pyroclastic rocks, pillow breccia and some

flows. There are also some tholeitic basalt flows which become

more prevalent than calc-alkalic basalts in the area northwest to

east-northeast of Rous Lake."

Within the Heron Bay Group, there is an eastward facies change from

coarse fragmental volcanic rocks near Heron Bay, to finer-grained

fragmental volcanic rocks, to sedimentary rocks with a considerable

volcanic component (volcaniclastic) in the Hemlo area, to sedimen

tary rocks with an unclear provenance.

Stratigraphic relationships of rocks in the Carlson property area

relative to those at Hemlo have not yet been clearly defined (to the

author's knowledge) but it is very tempting to assign the Carlson

mafic volcanics as equivalent to the Playter Harbour Group and the

more felsic volcanic-sedimentary units to the west as part of the

Heron Bay Group.

A number of granodioritic to quartz monzonite plutons, also of

Archean age, invade the supracrustal rocks. One of these, the Gowan

Lake complex, forms much of the east boundary to the Carlson prop

erty. Numerous middle to late Precambrian subalkalic diabase dykes

cut all of the Archean rocks as do Proterozoic alkalic and lampro

phyre dykes. The latter are probably related to the Coldwell alka

line intrusive complex which is centred to the west of the present

property.

Multiple periods of deformation have taken place. Metamorphic grade

in the area of the Carlson property is indicated to be generally of

greenschist-amphibolite facies.

PROPERTY LOCATION

LEGENDPROTEROZOIC

Coldwell Complex Alkoline Intrusive

Granitic Rocks

Felsic Metavolconics, Tuffs lo Breccias

Mafic Metavolconics, Massive to Pillowed Lavas

Metasedimenfs, Pelite, Siltstone, Cole-silicatef, Argillite

SCALE

KILOMETRES

10 l i

CARLSON MINES LIMITEDMARATHON PROJECT

GEOLOGYNo. C-665

NO: Figart 3

WE.Br.rtlon•MPH

MPH Consulting Limited


- 19 -

5.2 Mineralization

A great deal of attention has been focused on the Terrace Bay-

Marathon-Hemlo-White River area of north central Ontario following

the discovery of world class gold deposits near Hemlo station in

1981 and 1982 by Corona Resources, Lac Minerals and Goliath/Golden

Sceptre. Teck Corporation subsequently farmed into the initial

(Corona) find and Noranda Inc. has earned a 50? share in the

Goliath/Golden Sceptre discovery.

The Hemlo deposits are geologically part of one large semi-

continuous zone which must rank as one of the greatest gold discov

eries of the century.

Pre-production reserve and capital cost figures are quoted as

follows:

Tonnes Grade Tonnes* Capital Cost

(million) (oz/tonne) per day ^Cdn. million)

Lac Minerals 47

(Williams Deposit)

Noranda et al 20

(Golden Giant)

Teck-Noranda 2.1

(Quarter Claim)

Teck-Corona 8.4

0.20 3,000

(6,000)

0.20 1,000

(3,000)

250

270

0.33 milled by Noranda

0.36 1,150 90

* Initial production with full-scale figure in brackets.

The combined output of the three operations will reach a staggering 2,400

ounces of gold per day when full production is achieved towards the end

of this decade.

l l l l l l l l l l lll l l l l l l

- 20 -

Gold mineralization at Hemlo appears to be spatially related to the

facies change between volcaniclastic sedimentary rocks to the west

and southwest and clastic sedimentary rocks to the east and north

east. It is localized at a volcanic-sedimentary contact and occurs

in the second volcanic cycle in the region which corresponds to the

Heron Bay Group.

The lack of raafic-ultramafle volcanic sequences in the Hemlo area

plus the presence of unusual mineralogical components (pyrite- moly-

bdenite-stibnite-arsenopyrite-barite) combine to differentiate this

ore zone from all significant lode gold deposits of the Canadian

Archean, such as the Timmins camp.

The ore consists mainly of pyrite, gold and molybdenite, with numer

ous minor minerals, in sheared volcaniclastic metasediments which

are sericitic and locally contain green mica. The volcaniclastic

units have been intruded by feldspar and quartz-feldspar porphyry

bodies and by diabase dikes. Of particular interest are the dis^

tinctive associated hydrothermal alteration assemblages tourmaline,

sericite, green mica and other aluminous minerals. Exhalative

volcanogenic models are intimated as to its genesis.

Recent workers such as Hugon (1984) consider the sericite schists

which host the Hemlo ores to be mylonites within a major dextral

shear zone. In this view, structural control of ore deposition is

considered significant and the exact or original lithologies are of

little interest. In this case hydrothermal epigenetic replacement

deposition may be invoked and, in fact, the alteration/accessory ore

mineralogy is precisely that of world-wide volcanic epithermal

deposits, for example in New Zealand.

Noranda's Geco massive sulphide deposit (Cu-Zn-Ag) at Manitouwadge

also occurs at an Archean volcanic-sedimentary interface, a similar

relationship observed for gold-pyritic ores at Hemlo.

I l l l l l l l l l l i i i i i i i i

- 21 -

Lytton Minerals Limited has reported what appears to be a signifi

cant gold discovery some 18 miles to the west of the main Heralo

deposits but located on the same general trend. Their drilling has

outlined a "low grade" silicified structure which extends for a

strike length of l mile and to a depth of 1,500 ft. (the "Main

Zone"). This zone is in the area of the first reported gold discov

ery in Hemlo area made by Moses Peekongay in 1869. Lytton, in late

1984, subsequently discovered two new zones some 1,300 ft. north of

the Main Zone, called the "C" and " Porphyry" Zones.

Gold mineralization in the "C" zone is reported as occurring in a

strongly siliceous sedimentary unit which contains barite and moly

bdenum and is bounded by dacltic pyroclastics. Values of up to 0 .23

oz Au/ton over 13.5 ft. core length have been reported (Northern

Miner, January 24, 1985).

Other gold showings and occurrences in the region occur at

Schreiber-Terrace Bay and Big Duck Lake, adjacent to Winston Lake.

These occurrences are hosted, for the most part, by silicate and/or

sulphide-facies iron formation and interflow sediments (graphitic to

cherty argillite, laminated tuff, chert) often with appreciable

associated base metal values. The encompassing mafic volcanics are

frequently carbonatized and silicified which is reminiscent of the

associations found at the presently producing gold mines of the Red

Lake district.

The Schreiber-Big Duck Lake area produced only minor gold in the

1930's. Deposit examples include the Schreiber Pyramid, Harkness-

Hayes, Empress Mines and Otisse, McKenna-McCann prospects.

This segment of the Wawa subprovince also contains a number of base

metal occurrences of volcanogenic affiliation. Of these, the

Winston Lake deposit, located 20 km north of Schreiber and 70 km

l l l l l l l l I l l l l l l l l l l

- 22 -

west of the Carlson property, is the most important. It is a

classic volcanogenic massive sulphide deposit which occurs near the

top of a mafic to felsic calc-alkaline volcanic sequence of the

lower Winston Lake cycle. Alumina-rich alteration assemblages simi

lar to that at Geco are recognized.

Reserves at Winston Lake, now undergoing development, stand at

2,675,000 tonnes grading 17.8% Zn, Q.94% Cu, 25 g Ag per tonne and

0.85 g gold per tonne (1985).


- 23 -

6.0 PROPERTY GEOLOGY AND MINERALIZATION

6 .1 Property Geology

The majority of the Carlson-Black Gregor property is underlain by

mafic to intermediate metavolcanic rocks (basalts and andesites).

Fine-to-medium grained, dark green to grey-green mafic to inter

mediate metavolcanics are especially abundant. The rocks are both

massive and well foliated, occasionally gneissic and, in places, may

be described as amphibolites. The metavolcanics reach amphibolite

grade of metamorphism near the contact with the granitic rocks found

on the eastern edge of the property.

Medium-to-coarse grained mafic metavolcanics are sporadically noted

across the property. The unit exhibits gabbroic to dioritic texture

and may represent either sills or coarse-grained flows.

Pillowed metavolcanics are found throughout the area. Generally,

original pillow structures have been destroyed. For the most part,

only selvages of pillows and pillow rims are recognized. Partially

complete pillow structures, although stretched parallel to folia

tion, indicate apparent stratigraphic tops to the east.

Scattered exposures of vessicular flow-top breccia are found

throughout the area of mafic metavolcanics. The breccia is composed

of grey-green subangular to rounded clasts of moderately chloritized

metavolcanics.

Fine-grained, banded, mafic to intermediate tuffaceous rocks outcrop

on the property. These rocks display narrow bands of light and dark

tuffaceous material. Outcrops of lapilli tuff have also been

recognized. The lapilli generally average 1-2 cm in size and are

stretched parallel to foliation. Garnetiferous chlorite schist,

mica schist and minor greywacke also occur.

I l l l l l l l l l l l l l l l l l l

- 24 -

Narrow (generally less than 5 m wide) beds of interflow and chemical

sediments are mapped throughout the claims, principally represented

by siliceous argillite, graphitic argillite, cherty tuff and/or

oxide-to-silicate facies iron formations* These units are generally

less resistant to erosion and are found in gullies between more

resistant ridges of metavolcanic rocks.

A large U-shaped serpentinite body intrudes the volcanics on the

northernmost portion of the property. This is of some interest in

that disseminated to massive sulphide mineralization in altered

rocks is known at various places along the contact.

The Gowan Lake complex which is a granodiorite to quartz monzonite

intrusive is found on the eastern edge of the property.

Numerous diabase dykes, which generally trend northeast-southwest

have been seen over most of the property area. These dikes range in

width from 15 to 75 meters.

Narrow lamprophyre dikes are ubiquitous within the property area.

Structurally, the volcanic units trend generally north-south with

moderate to steep dips. The rocks appear to young eastwards.

Numerous small scale drag folds and abrupt strike variations attest

to the relatively complex, multi-phase deformational history these

rocks have undergone.

There are 2 prominent directions of faulting on the property, these

at N70 8W and N55 0W. These are clearly visible on topographic and

airborne geophysical maps with some of the more prominent examples

including the Runnalls Lake Fault, Fallen Lake Fault and Veronica

Lake Fault.


- 25 -

6.2 Mineralization

Three distinct types of sulphide mineralization are recognized on

the property:

(a) Pryitic quartz veins hosted by mafic metavolcanics.

(b) Sulphide-bearing (pyrite-pyrrhotite, * chalcopyrite) graphitic

to cherty, argillitic, laminated tuff and oxide-to-silicate

facies iron formation.

(c) Disseminated pyrite within mafic metavolcanics.

Types (a) and (b) would seem to have the most potential in terms of

gold exploration.

Surface grab samples taken from a narrow (l foot wide) pyritic

quartz vein near L2+OOS at 2+25E on the Wire Lake grid returned an

assay of 1.21 oz/ton Au. Another narrow pyritic quartz stringer in

the same vicinity returned a value of 0.52 oz/ton Au.

Several samples taken near 1+OOE on L2+50S from a sheared siliceous

interflow sedimentary zone, with up to 15X pyrite and pyrrhotite,

returned significant gold values with the highest being 0.45 oz/ton

Au, 0.16 oz/ton Au and 0.13 oz/ton Au. Another grab sample taken

from an iron formation located l .5 km north of this area returned a

value of 0.095 oz/ton Au. It would appear, based on airborne geo

physical data, that this latter occurrence is along the same stra

tigraphic trend as the Wire Lake mineralization.

l l l l lB A total of 915.5 meters of BQ drilling was completed in 8 holes. No

major problems were encountered and all 8 holes were completed to

l their desired depths.

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

isolated instances where the rocks were heavily fractured and

B sheared although core loss was minimal.

l

l

- 26 -

7.0 DIAMOND DRILLING PROGRAM -1987

7.1 Drilling

Drilling operations were carried out by N. Morissette Canada Inc. of

Haileybury, Ontario.

All drilling was carried out with a Longyear 38 machine supported by

a Hughes 500D helicopter.

Drilling operations were completed in the period February 26 to

March 20, 1987.

Drill core is presently being stored in core racks in a building at

H the Marathon airport.

B The drilling program was managed by MPH Consulting Limited of

' Toronto on behalf of Carlson Mines and Black Gregor Explorations.

V 7.2 Assaying

All assaying and analytical work was carried out by Assayers

j (Ontario) Limited of Toronto, Ontario.

l Gold, silver, copper, zinc and arsenic determinations were made by

atomic absorption. Anomalous gold values were re-checked by fire

fl assay techniques.

l

l l l

Core sections which appeared to have any Au potential were split and

H assayed.

l

- 27 -

Unused sample material will be collected from Assayers (Ontario) and

stored for possible future use.

l The entire assay results for the 1987 drill program are presented as

Appendix A.

l

l

l

l

l

l

l

l

l

l

l

l

l


- 28 -

8.0 DRILL RESULTS - 1987

8.1 Summary

The 1987 drilling in the showing area south of Wire Lake has estab

lished the presence of at least four distinct gold zones. Zone A is

seen in holes C87-6 and C87-7 and contained the second highest gold

value of the program (0.092 oz/ton over 1.43 m). In hole C87-6,

zone A is found near the contact between an intensely sheared,

silicified, sericitized and carbonatized mafic volcanic and more

massive mafic flows on either side. The gold is found in the more

massive mafic flows and occurs within weakly silicified and serici

tized zones that contain trace to 2% finely disseminated pyrite and

pyrrhotite. In hole C87-7, gold occurs in an intensely sheared,

weakly silicified, sericitized and carbonatized mafic volcanic with

trace to 2 7, disseminated pyrite. This shear zone appears to be the

same zone seen in hole C87-6. Zone A coincides with a very distinct

soil geochemical anomaly.

Zone B encountered in hole C87-1 is a zone of silicified mafic

volcanics that have been intruded by narrow (1-3 cm wide) quartz

veins and quartz stockworks. Gold values occur in the 0.05 oz/ton

range in silicified and weakly sericitized mafic volcanics which

contain up to 7% disseminated pyrite. Zone B also coincides with

the above geochemical anomaly.

Zone C, which is seen in hole C87-5, is within an altered mafic

flow. The zone is locally sheared, silicified and carbonatized.

Gold values to 0.05 oz/ton occur in silicified volcanics which con

tain l-2% finely dissemianted pyrite. This zone appears to be

related to a zone of intense shearing which contains several mica

schist units. Zone C may also coincide with the above mentioned

geochemical anomaly.


- 29 -

Zone D is to the west of the above mentioned drill holes and repre

sents a new discovery in this area. Hole C87-2 was drilled to test

a prominent MaxMin II EM conductor. The highest value of the entire

program, 0.14 oz/ton Au over a core length of 1.23 meters, was

obtained in this hole. The gold occurs in a slightly silicified

tuff which contains 2% disseminated pyrite and/or pyrrhotite. This

'tuff is within an interflow sedimentary unit approximately 15 meters

wide. This interflow unit appears to have a geophysical signature

in excess of 400 m. This zone represents a first priority target

for future work in this area.

Drill hole C87-8, which did not contain any significant gold values,

had distinctly anomalous copper and zinc values. The possibility of

massive sulphide base metal deposits on the Carlson-Black Gregor

property cannot be overlooked.

Anomalous drill results from the holes are summarized as follows:

Hole No. Collar From To Interval Au ppb oz/ton (m) (m) (m) (m)

C87-1 L2+50S, 1+48E 4.88 5.30 0.42 1259 .0475.30 6.53 1.23 1778 .052

11.95 12.19 0.24 1331 .04713.01 13.95 0.94 19059.74 60.11 0.37 239

C87-2 L2+50S, 0+80W 65.64 66.87 1.23 4350 .140

C87-5 L1+70S, 1+70E 47.99 49.37 1.38 722 .02149.37 50.16 0.79 18153.07 53.90 0.83 1483 .04753.90 54.40 0.50 16854.40 54.93 0.53 51664.94 66.10 1.16 26279.59 80.09 0.50 219


- 30 -

Hole No. Collar From(m) (m)

C87-6 L2+75S, 2+40E 21.9024.9027.0031.6335.2138.1742.1844.8745.6949.13

C87-7 LH-(OS, 2+50E 86.0089.7391.3893.6094.1796.47102.70103.66108.45109.85

To(m)

22.6625.1827.8332.6535.8838.8043.1545.6947.1249.55

86.7090.5091.6394.1795.4696.93103.56104.32109.38110.64

Interval(m)

0.760.280.831.020.670.630.970.821.430.42

0.700.770.330.571.290.460.860.660.930.79

Au ppb

924189168163404

1133450

13582995844

1063615264694534182182154153413

oz/toi

.022

.027

.033

.092

.028

.031

Logs and sections for the 1987 drilling are presented as Appendices

B and C respectively. Hole locations are shown on Map 2a.

8.2 Detailed Discussion. Drill Holes C87-1 to C87-8

Hole C87-1, collared on L2+50S at 1+48E, was drilled to test a geo

physical conductor that coincides with a sheared, silicified, seri-

citized, carbonatized, interflow sedimentary unit containing up to

lS-20% pyrrhotite, ;f pyrite mineralization. Grab samples taken from

this unit at surface returned values of up to 0.45 oz/ton. Three

anomalous zones (samples BG-1, 2 and 5) near the top of the hole are

described above as zone A. Semi-massive to massive bands of pyrr

hotite, similar to the surface grab samples, were encountered at a

drill depth of 61.16 to 65.96 meters; however, no gold values were

obtained from this zone.


- 31 -

Hole C87-2. collared on L2+50S at 0+80W, was drilled to test a

strong geophysical conductor with a strike length in excess of 400

meters. This conductive zone is a siliceous, graphitic, argilla

ceous to tuffaceous interflow sedimentary unit with up to 5% dissem

inated pyrite and pyrrhotite mineralization. Sample BG-17 taken

over a core length of 1.23 meters assayed 0.140 oz/ton Au. This

sample of siliceous tuff is described above as zone D.

Hole C87-3 collared on L3+OOS at 1+05E, was drilled to test a

geophysical conductor extending south from the zone tested by hole

C87-1 . The target sheared, silicified interflow sedimentary unit

was intersected at a core depth of 38.45 to 44.44 meters. Sulphide

mineralization was not as well developed as in C87-1 and no gold

values of significance were obtained.

Hole C87-4, collared at 4+05S/0+75E, was drilled to test the south

ern extension of the geophysical conductor and mineralized zone

tested in holes C87-1 and C87-3. The same sheared, silicified,

graphitic argillite zone was intersected at a core depth of 72.40 to

74.63 meters, however, as in C87-3 this mineralized zone was poorly

developed and no gold values were obtained.

Hole C87-5. collared at 1+70S/1+70E, was drilled to test a geochemi-

cally anomalous zone and also the northern extension of the

geophysical conductor tested in holes C87-1, 3 and 4. Two anomalous

zones were intersected at drill core depths of 47.99 to 49.37 meters

and 53.07 to 54.93 meters, respectively. These two zones have been

combined and are described above as zone C.

Hole C87-6 was collared at 2+75S, 2+40E and was drilled to test a

highly anomalous soil geochemical anomaly (1130 ppb Au), centred 25

meters due west of the drill hole collar. Two distinctly anomalous

zones were intersected at core depths of 21.90 to 22.66 and 38.17 to


- 32

49.55 meters, respectively. These zones coincide with the geochemi

cal anomaly and returned a maximum value of 0.092 oz/ton Au over a

core length of 1.43 meters. This zone represents a second priority

target for future work in this area.

Hole C87-7, collared at 1+90S, 2+50E, was drilled to test a surface

pyritic quartz vein zone where grab sample values exceeded l .2

oz/ton Au. This hole also tested the geochemical anomaly extending

south from hole C87-6 at a greater depth. It appears that the sur

face quartz vein zone has been cut off at depth by a granitic intru

sive located slightly to the east of the surface showing. An anoma

lous zone was intersected at a core depth of 86.00 to 86.70 meters

which appears to be the northern extension of zone A intersected in

hole C87-6.

Hole C87-8 was collared approximately 2 km southwest of Wire Lake at

16+35S, 9-4-12.5W. This hole tested a strong airborne and ground

geophysical response. The conductive zone is a 5 meter wide inter

flow sedimentary unit consisting of siliceous, graphitic argillite

and siliceous tuffs. Up to 153! semi-massive to massive bands of

pyrrhotite, pyrite * chalcopyrite mineralization occur at a core

depth of 76.81 to 84.15 meters. No gold values of significance were

obtained, however distinctly anomalous zinc values are present (to

2300 ppm Zn). This is relevant since the possibility for a massive

sulphide base metal deposit on the Carlson-Black Gregor property

cannot be overlooked.


- 33 -

9.0 CONCLUSIONS AND RECOMMENDATIONS

It is apparent that at least four distinct gold zones exist within the

discovery area just south of Wire Lake. Zone A appears to be related to

a sheared, silicified, sericitized and carbonatized zone within mafic

volcanics. Gold occurs within this sheared zone as well as in the less

sheared mafic volcanics on either side. A value of 0.092 oz/ton Au over

a core length of 1.43 m (4.69 ft) was obtained in hole C87-6. Though

not ore-grade, it is significant enough to warrant further work.

Zone D is a sheared, silicified interflow sedimentary unit consisting of

interbedded graphitic argillite and tuffaceous sediments. It appears to

have a strike length in excess of 400 meters. This zone represents a

first priority target for any future drilling in that a value of 0.140

oz/ton Au over a core length of 1.23 meters (4.04 ft) was obtained in

hole C87-2.

Two other anomalous gold zones (Zones B and C) were also identified

during the drilling program. Although values were not as high as above

(generally around 0.05 oz/ton) it is considered that further work is

warranted to properly evaluate these zones.

At least two of the gold zones directly coincide with a soil geochemical

anomaly. This type of survey will make an excellent exploration tool and

should be included in any future work program.

It is concluded that results from this first phase of drilling are suffi

ciently encouraging to warrant a major exploration effort encompassing

the present Wire Lake area and extending for some 6 km to the north along

the geophysically-indicated continuation of the potentially favourable

trend.

The basic geological/geophysical/geochemical reconnaissance on the pro

perty as a whole should continue.

1111111111111111111

t- 34 -

The recommended work program is as follows:

A) Supervising, Management, General Consulting

B) Wire Lake Area

Allowance for stripping, trenching and sampling 50,000

Helicopter, mob/demob 7,500

Completion of soil geochemistry, analytical 10,000

Reporting, drafting, reproduction 2,500

C) Wire Lake North Area

Linecutting, geophysics (mag, VLF, MaxMin II) 50,000

50 miles @ $l,000/mile

Helicopter, mob/demob 20,000

Geochemical sampling over EM anomalous areas 80,000

2,000 samples @ $40/sample

Geological mapping/prospecting 60,000

Allowance for stripping, trenching 20,000

Reporting, drafting, reproduction 15,000

Miscellaneous equipment, supplies, communl- 5,000

cations

D) Continuing Evaluation of Balance of Property

E) Diamond Drill Allowance

10,000 ft @ $60/ft all inclusive

GRAND TOTAL APPROXIMATELY

$ 15,000

70,000

250,000

75,000

600,000

$1,000,000

l l lB

l

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

- 35 -

Further work on the property will be contingent on the results of the

above relative to on exploration models for the property area.

Respectfully submitted,

J. P. Rollinson, B. Se.

D. T. Hillier, B. Se.

l l l

Hugon, H., 1984: The Hemlo Deposit: Gold mineralization within a

fi Dextral Shear Zone, O.G.S. Summary of Field work, 1984.

lll

REFERENCES

Milne, V.G., 1967: Geology of Cirrus Lake-Bamoos Lake Area, District of

Thunder Bay; Ontario Department of Mines, Geological Report 43, 612 p.l^ Accompanied by Map 2099, scale l inch to \ mile.

Milne, V.G., 1972: Manitouwadge-Wawa Sheet, Algoma, Cochrane, Sudbury,

l and Thunder Bay Districts; Ontario Division of Mines, Geological Com

pilation Series, Map 2220, scale l inch to 4 miles.

MPH Consulting Limited, 1985: Report on the Marathon Area Gold Property

tt of Carlson Mines, Ltd., 82 p. (including Appendices).

MPH Consulting Limited, 1986: Report on Geological, Geochemical and Geo

physical Surveys, Marathon Project for Carlson Mines Ltd., 82 p.l(including Appendices).

Muir, T.L., 1982a: Geology of the Heron Bay Area, District of Thunder

l Bay; Ontario Geological Survey report 218, 89 p. Accompanied by Map

2439, scale 1:31,680.

* Muir, T.L., 1982b: Geology of the Hemlo Area, District of Thunder Bay;

I Ontario Geological Survey report 217, 65 p. Accompanied by Map 2452, scale 1:31,680.l Muir, T.L., 1983: Geology of the Hemlo-Heron Bay Area; p 230-239, in CIM

Geology of Gold in Ontario; edited by A. Colvine, Ontario Geological

l Survey, Miscellaneous Paper 110, 278 p.

11I11111111111111ii

*- 2 -

Muir, T. L., 1984: Geology of the Hemlo - Heron Area p Dl-20 in CIM Geo-

logy Division Guidebook, Hemlo-Manitouwadge-Winston Lake, edited by

McMillan and Robinson, Field Trip, October, 1984.

Paterson, G. R., 1984: Exploration History and Field

the Hemlo Area in CIM Geology Division Guidebook,

Stop Description of

Hemlo-Manitouwadge-

Winston Lake, edited by McMillan and Robinson, Field Trip, October,

1984.

Paterson, G. R., 1984: Exploration History and Field Stop Description of

the Hemlo Area in CIM Geology Division Guidebook,

Hemlo-ManitouwadgeWinston Lake, edited by McMillan

Trip, October, 1984.

Quartermain, R. A., Trusler, J. R., Blecha, M. and Fox

liminary Geological Description of the Corona Gold

Ontario; unpublished paper presented at Canadian

and Metallurgy in Winnipeg, 1983.

and Robinson, Field

, J. S., 1983: Pre-

Deposit, Hemlo Area

Institute of Mining

Sheehan, D. G. and Valliant, R. I., 1983: Exploration, Discovery and Des

cription of an Archean, Stratiform, Pyritic Gold Deposit, Abstract,

Canadian Institute of Mining and Metallurgy Bulletin, Volume 76, Number

851, p. 86-87.

Valliant, R. I., Mongeau, C., Doucet, R., 1982: The Bousquet Pyritic Gold

Deposit, Bousquet Region, Quebec: Descriptive Geology and Preliminary

Interpretations on Genesis, in Cimm, sp. V. 24,

Gold Deposits, p. 41-49.

Geology of Canadian

APPENDIX A

l l l I l 1 l l lf Assay Results

l

l

l

l

I

l

l

l

l

111111111111111111

/7T\ ASSAYERS (ONTARIO) LIMITEDLMJL^ 33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z2Z2 - TELEPHONE (416)239-3527

Certificate of Analysis

rpriifirato No MPH-17/6Q43- Date:

Received - 1-6 Samples of -...- D-H-i-LLllCWIVWI ——— —————————————— - ————————————— ————— —— ————————————— * w '

nu M ^ MPH Consulting Ltd. Att.'n

Proj ect : C-951

Sample No. Au ppb oz/ton Ag ppm As ppm

BG-1 1259 .047

ASSAYERS (ONTARIO) LIMITED33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z 2Z2 - TELEPHONE (416) 239-3527


Certificate No. .JIE H^ia/j&iJAi.

Received ___-___________ ————13-

I Submitted by ^.JULH_CjxrLS-ul-tJ-n-a-J-trL._—

Samples of

Date: February

Dr-i-i L.-Cpr-e_____

_A^t-Uw-

| Project: C-951

l

l

Sample No

BG-17

18

19

20

21

22

23

24

25

26

27

28

BG-29

Au ppb oz/ton

4350 .14

1 /7^| ASSAYERS (ONTARIO) LIMITEDY UM 33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z 2Z2 - TELEPHONE (416) 239-3527

l

11 Certificate No.

Received .

1 Submitted by

1 P r o i e c t :

Sample No .

| 6G-30

31

133

135

1 3637•7 o

1 383940

1 'i42

144

1 45461 4 ?1 48

1 "BG-51

1

1

1

Certificate

MPH-1 9/01/6089

___ Mar. 12/87 66 S

C-951

Au ppb oz/ton Ag ppm Pt

0 ^1

ASSAYERS (ONTARIO) LIMITED33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z2Z2 - TELEPHONE (416) 239-3527


1 111111111111111

Certificate No. JEJi^

Qn^AtY/orl MSP fiULfOlvtjvl _________ LU.oJ — *-

Submitted by _ MEii

Proj ect : C-95

Sample No .

BG-52

53

54

55

56

57

58

59

60

61

62

63

64

65

66

67

68

69

70

71

72

BG-73

19/02/6098

1P/87 66

1

Au ppb oz/ton

181

ASSAYERS (ONTARIO) LIMITED33 CHAUNCEY AVENUE TORONTO, ONTARIO M822Z2 - TELEPHONE (416) 239-3527


Received . . .....Mar. 1 2/87

Submitted by ™JlEJtLJCjmsjjJ.:Li

Proj ect : C-951

66 Samples of

ng j-jjnj-t.e.d. .,

Sample No. Au ppb Ag ppm

BG-74

75

76

77

78

79

80

81

82

83

84

85

86

87

88

89

90

91

92

93

9't

BG-95

76 ^1

146 < .']

219 ^1

76 < .^

15 ^1

^

ASSAYERS (ONTARIO) LIMITED33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z2Z2 - TELEPHONE (416) 239-3527


Certificate No. M PH-20/01 /6089 Date:,,,Harch 30 , 1 987

Received Mar.

Submitted by MPH

Pro j ect : C-95

Sample No .

BG-2A

96

97

98

99

100

101

102

103

104

105

106

107

108

109

110

1 11

112

1 13

BG-1 14

17/87 36

Consulting Ltd.

1

Au ppb oz/ton

30

42

16

72

12

924 .022

189

47

168

1 /5\^L ASSAYERS (ONTARIO) LIMITEDV'lBV 33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z2Z2 - TELEPHONE (416) 239-3527

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

^**S'


Certificate No. J4PJHr2D7. 027 6089

Received Jar lZ7Ji7 - —3^ __ Samples of

Submitted by _ M.PJLJlcias-U-Lt i.n.g--L±-d--- - -- -- ——

Project: C-951

Sample No. Au ppb oz/ton Ag ppm

BG-115 1133 .027 < .^

116 450 0.3

117 1358 .033 < . /\

118 2995 .092 ^1

119 844 .028 ^1

120 89

1111111111111111111

f^\ ASSAYERS (ONTARIO) LIMITEDL* ijU 33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z2Z2 - TELEPHONE (416) 239^^•^^^

xs6iilnCcLiO PnO. . -——— . l T .ti. TJ

Rftf*O jyfVfj M ri P

Submitted by MPH

Sample No .

BG-131

132

133

134

135

136

137

138

139

140

141

142

143

144

145

146

147

148

149

1 50

BG-151

?1 /D1M1P1

74/87 -

.Consult i no

Au ppb o

50

39

11111111111111111

/7^ ASSAYERS (ONTARIO) LIMITEDL IMf 33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z 2Z2 - TELEPHONE (416)239-3527


Certificate No. __ tlilE-Zl/JdZj^ALZ-'L.

Receive^ Mar. 74/87 .42 Samples of

Submitted by MP H _ Qxxn-S-u L-t-i-ag -Ltd-. ——————————

Sample No. Au ppb Ag ppm

BG-152 59

J®1

1 Certificate No.

Received

1 Submitted by

1

1

1

1

1

1

1

1

1

1

1

1

1

1

ASSAYERS (ONTARIO) LIMITED33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z 2Z2 - TELEPHONE (416)239-3527

i


MPH-PP/m/6127

___ Ha-r —24.7.8171-

—— Mfi-H _ C-O.rvsJJ-L±J-n-g L±-C

Sample No. Au ppb

BG-173 69

174 37

175 34

176 28

177 17

178 16

179 37

180 ^

181 17

182 36

183 < ^

184 O

185 < 5

186 < 5

187 < '5

1 88 20

189 A3

190 < 5

191

ASSAYERS (ONTARIO) LIMITED33 CHAUNCEY AVENUE TORONTO, ONTARIO M8Z2Z2 - TELEPHONE (416)239-3527


Certificate No.

Received ^M

Submitted by

MPH-22/02/6127

Mar. 24/87 42 Samples of

MPH Consulting L i m rt p ri_

Date: February 27^ 1987

Drill Core

-A.t Jt-Ln : Mr. Ul. Rrprptnn

Sample No.

BG-194

195

196

197

198

199

200

201

202

203

204

205

206

207

208

209

210

211

212

213

B G - 2 1 4

Au ppb

APPENDIX B

l f l l l ll l lg Drill Logs

l

l

l

l

l

l

l

l

l

M P H CONSULTING Ltd DIAMOND DRILL HOLE RECORD Page 11 of

PropertyLocationHole No.BearingDip-Collar

FROM TO

BLACK 6RE50RMARATHON, OUTC87-1290 DEGREES-45 OE6REES

latitude LINE 2 * 50 SDeparture 1 * 4B EElevationNorthingEasting

DESCRIPTION

StartedFinishedLengthCUii No,Tirget

FEBRUARY 14, 19B7FEBRUARY 28, 1987124.10 i HETER546B110

Depth Dip Aziiuth Test Depth Dip Aziiuth Test Drill No.60.0 - 42 124.0 - 3B Logged by 3 .

Checked by ME

Consnts

SAMPLE fm TD HIDTH Au Ag Auppb ppi 0: Ton

Drill Co. N. HORISSETTEP.ROLLINSONBRERETON Core BB

Cu In Asppi ppi ppi

SUMMARY

0.00 3.66 CASING

3.66 7.46 MAFIC FLOH

7.46 14.48 MAFIC TUFF DR COARSE FLOH

14, JB 29.44 MAFIC FLOH

29.44 32,61 LAMPROPHYRE DIKE

32.61 59.74 MASSIVE MAFIC FLOH

59.74 60.11 MAFIC DIKE

60.!! 61.16 INTERMEDIATE OR SILICIFIED VOLCANIC

61.U 65.96 INTERFLOW SEDIMENTS

65,96 127,10 MAFIC FLOH

M P H CONSULTING L td. PROPERTY - BLACK GREGOR HOLE - C87-! PAGE

FRON DESCRIPTION SAMPLE FROM TO HIDTH Ag ppi

Au Oz Ton

Cu ppi

In ppi

As ppi

0.00 3.64 CASING

3,44 7,44 MAFIC FLON- dark to lediui green, very fine-grained- linor carbonitization in nisps throughout- tiny Kin) ilca (biotite) or uphibole flakes, possible indication of letaiorphic grade- trace pyrite/pyrrhotite in very fine disseiinations throughout- linor patches of silicification

4.83 - 6.52 - slightly siliceous Kith trice to IX pyrite disseiinitedthroughout

6.48 - 6.4? - quartz veinlet at approxiiately 55 degrees to the core axis- gradational contact Kith next unit

7.46 14.48 MAFIC TUFF OR COARSE FLOH- dirk to lediui green, fine-grained, but slightly coarser-grained than ibove f l ON- tiny clasts of feldspar and aiphibole present- trace pyrite-pyrrhotite disseiinited throughout

9.81 - 10.05 - linor quart) stockwork, quart! for the lost pirt is birren Kith up totrace pyrite, reinant volcanics ippear slightly epidotized?ftericitizedoith trice very fine pyrite

10.88 - 10.8? - lei Hide pink (fleshy) quirtzo-feldspathic stringer! 11.15 - 11.35 - narroN silicified zone, volcanics appear to be silicified and

sericitiied, IKO barren quartz veins ipproxliitely 2-3ci Hide it 47 to 50degrees to the core axis, trice disseiinited pyrite

11.95 - 12.1? - nirroK pyritic zone, up to 71 pyrite is fine disseiinitions throughoutthis zone

13.01 - 13,95 - tone of silicification/sericitization, barren quartz veins up to 3dKide, (5J cherty light brow) Kispy laiinations, linor (51 pinkquartzo-feldspathic blebs, trace to li pyrite disseiinated throughout,quartz veins have no preferred orientation

14,33 - 14.46 - nirroK zone of silica flooding Kith It pyrite in fine disseiinations- contict nith next unit probably Kithin above zone

14.46 29.44 MAFIC FLOH- dark green to grey, very fine-grained, i issive lafic flow- linor local silicification- trace pyrite disseiinated throughout- linor carbonate in thin hair-like fractures

19.26 - 20.2? - silicified, sericitized, trace pyrite 20.72 - 21.03 - narron silica/sericite zone with II pyrite and trice pyrrhotite

27,6? - carbonate and iron carbonate filling thin hair-like fractures 29,26 - 29,44 - sheared/fractured, carbonate and chlorite filling fractures

- suspect contact Kith next unit nithin sheared zone, at approxiiately 35 degrees to the core axis

29.44 32.61 LBNF'RDPHYRE DIKE- dark grey to black, fine to lediui-grained- phlogopite/biotite rich lafic intrusive

B6-1

B6-2 B6-2A

86-3

iG-4

5,30 0.42

5.304.33

t, S3 6,71

1.230.16

125?

177B 30

0.047

(.1 O.OS2 (.1

9.81 10.05 0.2S 133 U

11.IS 11.35 0.20 106 (.1

206

212 4?

?6

5734

78

?2 U

13 274

410 22 216

B6-5 11.95 12.19 0.24 1331 (.1 0.047 207 24 1(1

86-6 13.01 l J. 95 0,94 190 {.l 11? 10 168

B6-7 1?.26 20.2? 1.03 24 (.1 118 15 201

M P H CONSULTING; Ltd. PROPERTY - BLACK BRE60R HOLE - C87-1 PAGE l 3

FROM TO DESCRIPTION SAHPLE FROM TO V1DTH Au ppb

Ag ppi

Au Oz Ton

Cu PP*

Zn ppi

As. PP"

- cut by linor late stage quartz-carbonate veinlets 30.16 - 31.54 - pyritic, intensely chloritic volcanic nith 5-71 pyrite in

seii-iassive to disseiinated stringers- contact nith next unit at approxiiately 43 degrees to the core am

30.96 31,59 0.63 139 1351 7032.41 59.71 HASSIVE HAF1C FLOtl

-dart; green to grey, very fine-grained tassive lafic flOH- cut by ilnor later stage quartz-carbonate yeinleti nhich do not appear to have any preferred orientation- chloritic- trace pyrite tending to locate Hithin shear-fracture planes

38.5j - 40.23 - phlogopite rich zone, up to 101 phlogopite as very fine lightbronn grains disseiinated throughout

42.62 - 43.0? - thin interband of slightly coarser porphyritic lafic flow 44.BO - 44,81 - lei wide quartz-carbonate veinlet 51.23 - 51.78 - quartz vein cutting volcanics at 52 degrees to the core ixis,

sericitization of volcanics at contact, trace pyrite/pyrrhotltediiseiinated throughout, linor carbonate "lthin quartz

55.55 - 56.40 - biotite flakes Hithin volcanics, possible indication ofletaiorphic grade

58.88 - 58.90 - quartz-carbonate stringer nith trace pyrite- contact nith next unit at 74 degrees to the core axit

B-9 51.23 51.7B 0.55 53 (.1 184 44

59,74 60.11 MAFIC DIKE

60.1!

- dark grey to black, Fine to lediui-gralned lafic intrusive- probably related to Port Coldtiell Coiplex- 2-31 pyrite very fine-grained, often ringed by aiphibole- note saiple B6-42 assayed 380 ppb Pt and 180 ppb ft- a t largin Nith volcanics appears chilled, very fine-grained- around (0.11 core is broken and sheared obscuring contact

61.16 INTERMEDIATE OR SILICIFIED VOLCANIC- light to lediun green, very fine-grained volcanic- trace pyrite disseiinated throughout- cut by linor (1-21) carbonate stringers- gradational contact with next unit

B6-42 59.74 60.11 0.37 139 0.1 124 126

61.16 65.96

41.16

INTERFLOW SEDIMENTS- light green to grey silicified/sericitized sediients/volcanics Nith up to 711 pyrite/pyrrhotite disseninated thioughout- sulphides are within seii-iassive to disseiinated stringers- linor Nispy carbonate stringers

61.76 - Silicified, with 3-57. pyrrhotite and trace pyrite in seii-iassive stringers- contact Kith next unit at 56 degrees to the core axis note - this zone is cut by a laiprophyre dike

63.72 - lediui-grained phlogopite rich lamprophyre, up to 20?. phlogopite in shiny brown flakes- contact Kith nett unit Jt 70 degrees to core axis

86-10

B6-11 BB-12

61,16 61,76 0.60

61.7662.59

62,5963,72

0,831.13

55

2665

740 317

252 94344 70 50

M P H CONSULTING Ltd. PROPERTY - BLACK 6RE60R HOLE - C87-I PAGE l 4

FROM DESCRIPTION SAHFIE fm TO KIOTH Au Ag Au Cu In Asppb ppi Di Ton ppi ppi ppi

43.72 -

64.49 -

65.41 -

64.

65.

45.

49

41

It

- lilicified/seridtized ion: with 5-71 pyrrhotite md tricein seii-iassive bands md disseiinited stringers- silicified zone with up to 101 pyrrhotite in seii-iassivetrace nounts pyrite in finely disseiinited stringersnote - sulphide binds tppeir to be cutting the core axis at- tilicified/sericitlzed, trace pyrite/pyrrhotlte in linelystringers- no distinct contact Kith next unit

to 21 pyrite

binds Kith

30-32 degreesdisieilnated

8G-13

SB-14

BG-15

43.72

44.49

45.41

44.49

45,41

45.96

0.77

0.92

0.55

75 (.1

80 (.1

18 (.1

470 350

880 383

294 74

(1

(1

(1

45.96 127.10 BAF1C FLOH- sue as above tentioned iific HOB

78.53 - 78.98 - silicified, with 31 pyrrhotite in seii-usiive to disseiinited stringers79.95 - 79.96 - quartz-carbonate veinlet cutting the core it tpproKiiitcly 25 degriei68.42 - 90.19 - slightly coarser-grained iific flow91.48 - 91.65 - nuierous thin hair-like unite and pink quartz-cirbonate/feldspathlc

stringers99.44 - 99.46 - pink quartzo-feldspathic veinlet94.60 - 96.70 - sericitic, quartzo-feldspathic veinlet96.80 - 96.85 - sericitic, quartzo-feldspithic veinlet98.70 - 99.30 - abundance of biotite? or hornblende flakes 100.43 - 100,46 - sericitlzed quartt-carbonate veinlet tilth trice pyrrhotite 106.97 - 106.99 - carbonate filled fracture 107.50 - 107.52 - carbonate tilled fracture 115.67 - 115.70 - carbonite veinlet lith trice pyrite

88-16 78.53 78.98 0.45 32 U 733 90

127,10 - END OF HOLE C87-1

M P l-1 CONSULTING Ltd. DIAMOND DRILL HOLE RECORD Page 11 of

PropertyLot ill onHole No.BearingDip-Collar

FROM TO

BLACK ERE60RHARATHON.ONTC87-2290-45 DEGREES

Latitude LINE 2*50 SDeparture 0*80 HElevationNorthingEasting

DESCRIPTION

StartedFinishedLengthCliii No.Target

MARCH 2, 19B7MARCH 3, 196799.7 i HETERS468110

Depth Dip Aziiuth Test Depth Dip Aziiuth Test Drill No. Drill Co. N. NORISSETTE L63,0 - K 99.7 - 43 Logged by J.P.RDU.INSDN

Checked by Core BO

Conenti

SAMPLE FROM TO NIDTH Au Ag Au Cu In Asppb ppi D: Ton ppi ppi ppi

SUMMARY

0.00 1,60 CASING

i.80 15.23 MASSIVE MAFIC FLO*

15.2J 19.50 MAFIC TUFF OR VERY FINE-BRAINED MAFIC INTRUSIVE

19,50 27.15 HASSIVE MAFIC FLOH


28.20 43,98 MASSIVE MAFIC FLOH

43.98 45,65 INTERMEDIATE FLOH OR SILICIFIED FLOK

45.85 47,01 MASSIVE MAFIC FLOH

47.01 48.35 HAFIC TUFF OR COARSE FLOH

48.35 64.91 MASSIVE tIAFIC FLOH

64.91 B4.84 INTERFLOH SEDIMENTS

B4.E4 99,70 MASSIVE MAFIC FLOH

M P r l CONSULTING Ltd. PROPERTY - BLACK 6RE60R HOLE - C87-2 PftSE t 2

FRQH TD DESCRIPTION SAMPLE FROH TD HIDTH Au Ag Au Cu In Asppb ppi Oz Ton ppi ppi ppi

0.00 1,60 CASING

l.BO 15.23 NASSIVE HAF1C FLOK- dark green to dark grey, very fine-grained to aphanitic- loderitley carbonitized, wth carbonate in nitpy itringert md ittoclitid with quartz in veinlets, no preferred orientation to the veinleti- trace pyrite/pyrrhotite disseminated throughout

4,70 - 4.93 quartz-carbonate veinlet at approxiiately 37 degrees to the core axil- gradationat contact Kith next unit

15.2J 17,50 HAF1C TUFF DR VERY FINE-BRAINED NAFIC INTRUSIVE- dark green to dark grey, fine-grained, toderattey serialized and carbonitiied- cut by linor quartz-carbonate veinletf- trace pyrite/pyrrhotite disseiinated throughout- note TBG-3 tent out for thin tectlon analytii- contact nith next unit at approxiiately 24 degreet to the core mil

19,50 27,15 MASSIVE tIAFIC FLOH- dark green, very fine-grained to aphanitic- linor K5H) quartz-carbonate in nitpy itringert and veinleti- trace pyrite and pyrrhotite disseiinated throughout- unit appears to be chloritlzed- linor graphitic interbandi with up to 71 pyrrhotite nithin

22,08 - 22.30 - graphitic interbind Kith up to 71 pyrrhotite in teii-miive bindi,contact at approxiiatley i2 degreet to the core axlt

22.40 - 22.45 - graphitic interband, slightly sheared with carbonate nlthin ihear, up to31 pyrrhotite nithin the graphite

23.90 - 23.93 - slightly sheared, with carbonate filling their 26.80 - 24.94 - tericitized quartz-carbonate shear nith trace pyrite/pyrrhotitc, note

shear is at approxiiately 45 degrees to the core axil- contact nith next unit at 30 degrees to the core axil

27.15 28,20 LAHPROPHYRE HIKE- dark green to dark grey, lediui-grained, tastive- 25 to 301 lica (phlogopite) as shiny brow flakes within the core- contact Kith next unit at approxiiatley 22 degreet to the core axis- note TB6-4 tent out for thin section analysis

26.20 4I.9B HASS1VE HAFIC FLOH- saie a above lentioned lafic f l OK except no graphitic interbandt

40.80 - 40.02 - quartz-carbonate veinlet at 27 degreet to the core axit-contact Kith next unit at 42 degrees to the core axis

43.9E 45,85 INTERMEDIATE FLOH OR SILICIFIED FLON- ilark grey to dark green, very fine-grained Hou- slightly coarser grained and slightly harder than above unit- note TB6-5 sent out for thin section analysis- contact with next unit at approxiiatley 25 degrees to the core axis

45.35 (7,01 NASSIVE HAFIC FLOW- dart green, *ery ^ine-grjined to sptunitic, chloritic iufic (Ion

MPH CONSULTING Ltd PROPERTY - BUCK 6RE60R HOLE - CB7-2 PftGE l

FROH 10 DESCRIPTION SANFLE FRON TO K1DTH Au ppb

fig PPI

Au Oz Ton

Cu ppi

Zn ppi

V

As PP*

- lassive but cut by linor K5i) wispy quarti-cirbonate itringert- trice pyrite/pyrrhotite disseiinated throughout- contact *ith next unit at approxiiatley 52 degrees to the core axis

47,01 4S.35 NAF1C TUFF OR COARSE FLOW- dark green to dark grey, fine-grained, chloritic lafic tuff?- slightly coarser grained than above (Ion- trace pyrite/pyrrhotite disseiinated throughout- contact xith next unit at ipproxiittley 35 degrees to the core mis

(8,35 64.91 NA55IVE NAFIC FLON- sate as above tentioned lafic flow

55.51 - 55.46 - graphitic interband nith 31 pyrrhotite disseiinated nithin i tinycarbonate shear

5j.46 - 56.16 - volcanics appear to be a slightly lighter grey, silicified? 64.74 - 64.91 - slightly silicified tone

- contact Kith next unit it approxiiately 46 degrees to the core axis

64,71 84.64 INTERFLOW SEDIMENTS- thinly bedded tuffs? and siliceous, graphitic argillite- siliceous graphite/argillite unit Is dark black, very fine-grained with up to SI pyrite/pyrrhotite disseiinated throughout lnination planes, ftlnor carbonate within laiination planes- laiination planes are at approxiiately 47 degrees to the core ixis- tuffaceous? unit is light to dark grey, fine-grained, iisiive- both graphitic argillite and tuffs? are locally silicified

65.6466.87

67.65 - 69.33

70.49 -

71,65

72.56 -73.3674.3!

75.59 -

76.3B

66,67 - slightly silicified tuff tilth 31 pyrite/pyrrhotite67,65 - siliceous graphite/argillite ttith 31 pyrrhotite In seil-iaisive to

disseiinated stringers69.33 - slightly siliceous tuff? Kith trace pyrrhotite/pyrite 70,49 - siliceous gnpnite/argillite tilth 5! pyrrhotitl and trice pyrite, note

contact with above tentioned tuff? is at approxiiately 44 degrees to thecore axis

71,65 - siliceous graphite/argillite tilth 31 pyrrhotite and trace pyrite indisseiinated stringers parallel to laiinations, binding is approxiiately47 degrees to the core axis

72,56 - Nell laiinated siliceous graphite/argillite nith 21 pyrrhotite and tricepyrite disseiinated throughout, laiinations are at approxiiately 29 degreesto the core axis

73.36 - silicified tuff? Kith cherty interbands, trace pyrite/pyrrhotite 74.31 - dark green partially altered tuff? Kith trace sulphides 75.59 - siliceous, sericitic tuff with cherty Interbands, trace pyrite/pyrrhotite

disssiiinatei! throughout76,38 - siliceous interlaminated tuff^/argillite nith trace pyrite/pyrrhotite 77.82 - siliceous interlaiinited tuH'-'grachitic argillite nith up to 2!

pyrrhotite and trace pjrite

0,34 - siliceous g'aphite/irgillite tilth 1-27, pyrrhotite and trace pyrite in fine disseminations

B6-41

B6-17 B6-18

BB-19

BB-20

B8-21

64.93 65,64 0.71 14

65.64 66,87 1.23 4350 66.67 67.65 0.78 (5

69.33 70,4? 1,16 (5

70.49 71,65 1.16 (5

71.65 72.54 0,91 (5

0.8 0.4

0.2

(.1

0.14

ISO

329361

6213

232

207

1346

2381992

1350

1100

967

2076

52

72

BG-22 86-23 86-24

86-25 86-26

86-27

BG-29

72.56 73.36 74.31

75.59 76.38

77.82

79.26

73.36 74.31 75.59

76.38 77.82

79.26

80.34

O.BO 0.95 1.28

0.79 1.44

1.44

l. 08

(5 < . (5 ^ (5 ( ,

(5 < . (5 < ,

tt ( .

tt i .

97 119 96

118209

185

582

64 JO 11

326 648

50

67

134 (1

131

150 73

66

\1

MPH CQNSULTINB Ltd PROPERTY - BLACK BREBOR HOU - CB7-2 PftBE l 1

FROH TO DESCRIPTION

B0.34 - 60.80 - silicified lull? Kith83.25 - B3.72 - silicified tuff? Nith

H disseiinated pyrrhotite/pyritethin chloritic stringers, trice pyrrhotite

SAMPLE

B6-40B6-29

FROM

BO. 34B3.25

TO H1DTH

B0.80 0.44B3.72 0.47

Auppb

19(5

Ag Au Cuppi Oz Ton p'pn

U 245U 97

ZnPP"

21012

AsPPI

u147

- contact with next unit it 47 degrees to the core axis

84,B4 99,70 HASSIVE HAF1C FLOK- dark green, very (ine-griined, ussive lau'c flon, trice pyrrhotite/ pyrite disseiinated throughout- cut by linor quartz-cirbonite veinlets K5S)

99.70 - END OF HOLE CB7-2

M r H CONSUL-TIMS Ltd. DIAMOND DRILL HOLE RECORD Fags f i o f

PropertyLocationHole No.BearingDip-Collar

FKOH TO

BLACK EREGORMARATHON ONT.C87-T290 DEGREES-45 DEGREES

Latitude LINE 3 * 00 SDeparture 1 * 05 EElevationNorthingEasting

DESCRIPTION

StartedFinishedLengthCliii No.Tirget

MARCH 4/B7MARCH 7/8799.70 i METERS646110

Depth Dip Aziiuth Tett Depth Dip Aziiuth Test Drill No.40.0 - 45 99.7 - 43 Logged by J. P

Checked by K. E

Conentt

SAMPLE FROM TD WIDTH Au Ag Auppb ppi Dz Ton

Drill Co. N. MORISSETTE L.RDLLINSON, BRERETON Core B9

Cu In Asppi ppi ppi

SUMMARY

0.00 3.64 CASINO


6.64 27,68 BAFIC FLON


35,}9 42,64 MASSIVE NAFIC FLON

42.44 44.44 INTF.RFLDH SEDIMENTS

44.44 97.70 MASSIVE MAFIC FLON

M P H CONSULTING Ltd. PROPERTY - BLACK SRE60R HOLE - C87-3 PABE f 2

FRON TO DESCRIPTION SABPLE FROM TO K1DTH Au fig Au Cu In Asppb op* 0; Ton ppi ppi ppi

0.00 3,66 CASING

3.66 6.64 LAMPROPHYRE DIKE- dark green to dark grey, lediui-grained lafic intrusive- cut by linor carbonate veinlets- characterized by an abun

: other l ] hole no, footage date1987 for carlson mines ltd, and black gregor explorations ltd,...

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