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GM 47388 GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

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Page 2: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Robert Oswald, R

GEOLOGICAL REPORT

EXPLORATION CAMPAIGN(1987)

LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORATION

Ministère de rtnergie et des Ressources Service de la Géoinformation

Oats 2 ! - T 1488 No G.M.:

ÉNERGIE ET RESSOURCES SECTEUR MINES

0 8 JUtL. 1988

Bureau régional Val d'Or.

February 1988 RO/1g

Page 3: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

CONTENT

PAGE

SUMMARY

INTRODUCTION 1

DESCRIPTION OF THE PROPERTY 2

Location and access 2

Claim description 4

PREVIOUS WORK 6

REGIONAL GEOLOGY R

GEOLOGY OF THE PROPERTY 10

Lithostratigraphy 10

Mineralization and alteration 1?

RESULTS OF THE CAMPAIGN 14

Economic aspect 14

Geological aspect 17

PRESENT WORK 19

CONCLUSION 20

RECOMENDAT I ONS 21

BIBLIOGRAPHY

Page 4: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LIST OF FIGURES

Figure 1 Location map of Launay-Trecesson property

Figure 2 Details of claims numbers of Launay - Trecesson property

Figure 3 Geological map of the Dumont intrusion

Figure 4 Cross section 36+00 W of Launay-Trecesson property

Figure 5 Campaign 1987 Location of DL-87-1 to DL-87-11 including E-7

Figure 6 Location of diamond drill holes DL-87-12 to DL-87-14 and the others campaigns

LIST OF APPENDICES

APPENDIX A: Parameters of D.D.H.

APPENDIX B: Chemical analyses of whole rocks

APPENDIX C: Best assays

Page 5: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

SUMMARY

The Launay-Trecesson property of Dumont Nickel

Corporation consists of 63 contiguous claims for a total of

1 492,4 hectares (3 688 acres). It is located at

approximately 22 kilometers (13.7 miles) west of Amos, north

western Quebec.

The Dumont Sill is a komatiitic differentiated

intrusion of Archean age. The sill intrudes subaqueous,

iron-rich tholeiitic lavas which are approximately 2,7 Ga

old. It is composed of a lower ultramafic zone and an upper

mafic zone.

The property was acquired in 1969 by Dumont Nickel

Corporation which discovered a weak nickel sulphide

mineralization in the lower ultramafic zone (dunite).

The 1987 campaign focussed on the exploration of the

basal contact, with the possibility of locating Pt, Pd in

the mineralized extension rich in Ni-Cu discovered in the

1970 campaign.

According to holes 87-1 to 11, this mineralization

forms a heap of two or three hundreds feet of dimension,

appears open north-west of the hole E7 and south east of

hole 87-11. The best values obtained in platinum and

palladium are respectively 0,75 gr/t (0.022 oz/t) over 0,6

Page 6: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

meters (2.0 feet) and 2,26 gr/t (0.066 oz/t) over 0,6 meters

(2.2 feet).

It is suggested that we continue our diamond drilling

campaign, and to extend the fields of investigation by

exploring the basal contact of the sill by using a bore hole

geophysical program (pulse EM).

Page 7: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1

INTRODUCTION

The 1987 exploration campaign was conducted on the

Launay-Trecesson property owned by Dumont Nickel Corporation

with the intention of exploring the basal contact, around

hole E-7, in search of platinum, palladium and nickel. At

the volcanic contact, this hole showed a 1,8 meter (6 feet)

intersection grading 1,39% Ni and 0,49% Cu mineralized with

pentlandite, pyrrhotite and chalcopyrite.

This report gives an account of the previous work and

the available knowledge of the property and describes the

work done during the 1987 campaign. The results obtained are

exposed, and the opportunity of doing further work on

the property is recommended.

Page 8: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DESCRIPTION OF THE PROPERTY

Location and access

The Dumont Nickel Corp. property, is situated 22

kilometers (13.7 miles) west of Amos. The property is

accessible by highway III (Figure 1), range lines and small

internal roads. The south part of the property is

intersected by the Canadian National railway. Water is

easily accessible to proceed through the diamond drilling.

Unfortunately, travelling through the property is sometimes

difficult for the equipment during the warmer season

(summer).

The area is rather flat, the elevation ranges of 300

meters (985 feet) to 365 meters (1 200 feet) above sea

level, and the maximum relief over the intrusion is about 30

meters (100 feet). Less than 2% of the bedrock surface of

the intrusion outcrops, and most of the exposure occurs at

the extreme ends of the body. The remainder is covered by

overburden which ranged in thickness from 12 to 45 meters

(40 to 148 feet) in the parts where drilling was carried

out.

2

Page 9: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

SUPERIOR

LAKE SUDBURY ~ONTREAL

CA/Olt •.~ •~S p.

••s R. VIII OTTAWA

\JAMES

AY

• MATAGAMI

LASARRE •AM 0

NORANDA• • •VAL D'OR

ON TAR I O

DUMONT NICKEL CORP.

S

QUEBEC

QUEBEC

ST - LAURENCE RIVER

CIO MS boundOry

R. V I I

, R. VI

Central mineralized dunlf• layer

R. V

To AMOS ~

HIGHWAY 111 LAUN AY

DUMONT NICKEL corp.

LAUNAY-TRECESSON PROPERTY

FIGURE 1

Scale Mips: O I 2

) I I i )

Page 10: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

4

Claim description

The property consists of 63 contiguous claims located

in range V to VIII totalling approximately 1 492,4 hectares

(3 688 acres). 54 claims are located in the Launay

Townships and 9 claims are located in the Trecesson

Township. The Figure 2 shows the list and location of the

claims.

Page 11: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

RANGE VIII

I 4392

27

-I

43

92

31- 2

~ 43

92

27-2

N N 0) M a 4

39227

-4 _

in0 M N a) 0) a) M a

N M

M a

If)

M

l a)ON M a

In

RANGE VII 4

39

23 1

- I

43

92

31-

3 a

N a) â _ N

M

— we

N

V M

..a N â co O M

N â m O M

30

214

9-I

I

30

84

13

„) - a

O M

30

2 L48-I

308

414

a — a O in

_ to a CO p

a

M N m M a

Kf

to M

a

30

21

48

-2

~

N

302147 -

I M

N

CO

V' CO O M

28

17

84-2

:W

- \*-N

N 2

81687

- 1

46

42

79-1

281

784-1

, 2

816

02-4

30

84

15

-3

3084

90

-I

1 ~

2

81783-4

12

81

60

2-3

308

41

5-4

308490- 2

RANGE VI é N O M)

~ m N

N

r CO W CO N

N — N ~

O O M )p CO O ~-y

N N N

M"-; ro M M m m co n r n mis m N N

RANGE V

M

ca W CO

^ N

a Q co T... w N

N

O )D

N

w) a a) r m N N

~/,,

01 M N N

"?M

w

N

CO

N --_

M O c m N

N

~ CO N

fY M O c co N

M0 M m a N

N sr

0

co N

Zr)M

st 0

a m

N

(y .

DUMONT N I CKEL corp.

LAUNAY-TRECESSON PROPERTY DETAILS OF CLAIMS NUMBERS

FIGURE 2 Seale

0 I 2km

1:60 000

Page 12: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

6

PREVIOUS WORK

The intrusion discovery on the property was first

reported by James and Mawdsley in 1925. Thereafter, many

unsuccessful exploration works were carried out over this

area for asbestos, base and precious metals. In 1969, when

the property was acquired by Dumont Nickel Corp., a weak

nickel sulphide mineralization in the Dunite (lower

ultramafic zone) was discovered.

Further to the results of a magnetometer survey in

1969, a bore hole campaign was completed in 1970 with 57

holes for a total of 21 053 meters (69 071 feet).

A comprehensive mineralurgical test work program (1971)

was conducted for the account of Dumont Nickel by the

Mineral Research Center of the Quebec Government, followed

up by a pilot plant test conducted on an 85 ton bulk sample

blasted from an outcrop at the eastern end of the

mineralized sill. The description and results of work

carried out during this period were covered in a feasibility

report prepared by Caron, Dufour, Séguin & Associates

for 4 500 tons per day mining and milling operation on the

property.

r.

With the agreement of Dumont Nickel Corp. (1974), the

Timiskaming Nickel Ltd. conducted laboratory and pilot test

work on samples from the mineralized sill which confirmed

the amenability of the nickel mineralization to the patented

Timiskaming process.

Page 13: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

lk

Four (4) 15,2 centimeters (6 inches) diameter holes

were drilled (1982) by percussion equipment to produce 35

tons sample which were sent for metallurgical testings.

In 1985, the Quebec Mineral Research Center and the

Société Nationale de l Amiante carried out for the account

of Magnitec Mining Exploration Inc., test work which

confirmed that the nickel mineralization was amenable to the

magnesium recovery process developed by the SNA.

In 1987, the Consultants Protect Inc. produced for

Dumont Nickel Corp. a geological report recommending to

carry out a program divided in two (2) phases, both focussed

on the basal contact of the Dumont ultramafic zone, in

search of economic sulphide enrichment deposits mineralized

in base metals and/or PGM.

Two drill core samples from the 1969-70 drilling

program were assayed for PGM and returned traces.

7

~

Page 14: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

8

REGIONAL GEOLOGY

The Dumont Sill is located within the central part of

the Abitibi greenstone belt in the Superior Province of the

Canadian Shield. The sill is hosted by lavas and volcani-

elastic rocks that have been assigned to the Kinojevis Group

by Latulippe (1972) and more recently, to the Amos Group by

Imreh (1980).

Three cycles of mafic to felsic volcanism are

recognized and the Dumont intrusion is one of at least five

ultramafic - mafic complexes in the Amos area which occurs

approximately at the same stratigraphie level within the

mafic lavas of the middle cycle.

Three main directions of faulting were recognized in

the Amos area by Weber and Latulippe (1964). The earliest

is the east-trending set of bedding plane faults which they

believed developed during the major period of folding. The

intrusion of the granitic rocks was accompanied by the

development of steeply dipping faults that strike north to

north-west. The most prominent faults strike north-east and

probably post date the granitic plutonism. The Dumont Sill 7

is cut by a number of these north-east trending faults

(Figure 3).

IONIA

Page 15: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

r r

r . r\

\ rr t \

\. i\ rr \.\ t \

4 •

r ~`.5 '\_. \ \ 3 \•\ NA, t N. '\ ▪ 1

\ ::::-c''''.,; ,, `~ 4 1`

\ \

\Zrr \3,

• , N \,...• .: ♦ • 'N r i \ 2 ` +` ,

• r • • •\'\

0 400 800

I l l mures

Mefic Zona

Upper PendObts Subsoils

Duntte Subsist*

Lower Pendotite Subzone

Basaltic lavas

Range VI

IR VI N60 I Range V

r •.

t• r ' '\ N

i 4••

♦ •\ ,\ \

*\ , 3 \ \ \ •\

2 ,\ \` N \\

5 •\ •

5

\

rr ~ , • rr ••

' • .••<

•\

• ~ 5

4

3

2

1

Aran of outcrop

Geotog cai contact. observed (in outcrop or drat cote?,

location inferred. location very approximate -----•—

Sch.sros.ty 1'

Faun. observed. inferred --

Dnande. collet location

Nicks, ennChed layer

Isolated sulphide occurs/xis t

\ -..

,._. ' 1 2

_ ~ ~ . { •• 4~t'~' . --"' 1 ..,... -

3 .

,

I .....

I GSC

DUMONT NICKEL corp.

LAUNAY-TRECESSON PROPERTY Geological map of the Dumont intrusion

FIGURE 3

Page 16: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

GEOLOGY OF THE PROPERTY

Lithostratigraphy

The Dumont Sill is a komatiitic synvolcanic intrusion

of Archean age. The sill intrudes subaqueous iron-rich

tholeiite lavas which are approximately 2,7 Ga old. The

sill is poorly exposed over a strike length of 6,5

kilometers (4.1 miles) and comprises a lower ultramafic zone

which averages 450 meters (1 500 feet) in true thickness and

an upper mafic zone about 250 meters (820 feet) thick

(Figure 4).

The ultramafic zone is subdivided into three subzoned:

1) lower peridotite,

2) dunite

3) upper peridotite

The mafic zone is subdivided into three subzones which

are from the base upwards

1) clinopyroxenite

2) gabbro

3) quartz gabbro

10

Page 17: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

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' i•il;„~~1`J •~ •• ••:: I- • =•• f NiCkMMndl•d gprl .. , •• I

. _ ; ~' Diunono•aie eel* snowlr+g /) :t =: ~,• : _ \ ; interwove .•0.35 % Ni.........

~,~ -' !~• ;-~Y.- ti•

':~I`

,.)..F:-....-2.:-' ---

-• ;;' ., GSC

CROSS SECTION 36+00 W

DUMONT NICKEL corp.

LAUNAY-TRECESSON PROPERTY

FIGURE 4

Page 18: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

SIM

MIN NA

MOND

Mineralization and alteration

Pentlandite <(Ni, Fe)9 S8>, heazlewoodite (Ni3 S2) and

awaruite (Ni2 Fe) are the principal nickel minerals with

lesser amounts of millerite (NiS). This mineralization

occurs as small, pinhead size, rounded blebs disseminated in

the serpentinized dunite and can be grouped into two size

ranges, one the coarser aggregats of composite grains which

vary from fifty to several hundred microns in diameter, and

the second group is represented by finely dispersed

particles of which most are less than 10 microns in size.

Magmatic sulphides are restricted to the lower

peridotite and dunite subzone. Three olivine sulphide

cumulate layers occur within the dunite subzone (Figure 4).

The middle layer has the highest average nickel grade 0,5%

and is the most laterally extensive persisting over a strike

length of 2 400 meters (7 900 feet) with an average true

thickness of 24 meters (80 feet). A higher grade zone

within the middle layer averages 0,71% Ni over a strike

length of 730 meters (2 400 feet) and has a true thickness

of 14 meters (46 feet).

Olivine, chromite and calcic clinopyroxene are the

essential magmatic minerals throughout the ultramafic zone.

Serpentinization is overprinted by talc-carbonate alteration

in places along the basal contact of the sill. The

predominant secondary assemblages is lizardite + magnetite

brucite + chlorite + diopside + chrvsotile + antigorite

pentlandite + awaruite + heazlewoodite + millerite.

12

r

Page 19: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

In 1970, native copper was found in a few bore holes.

The essential secondary minerals in the mafic zone include

actinolite, epidote and minor chlorite, quartz, pyrite,

calcite and leucoxene are accessories.

Page 20: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

RESULTS OF THE CAMPAIGN

Economic aspect

Two types of mineralization are observed in the lower

peridotite:

1) finely scattered sulphide (omnipresent in variable

quantities) sometimes obliterate by the alteration; or

2) a weak enrichment formed by heap or a lens to the basal

contact. This mineralization is caracterized by small

veinlets, heap or more disseminated sulphides.

The first type shows a weak enrichment in palladium.

The platinum was found only in the second type and the

nickel is omnipresent in variable quantities. The best

assays came from the second type. With this campaign, we

have better knowledge of the mineralization around the hole

E-7 at the basal contact. The heap was intersected (Figure

5) by the holes 87-1, 7, 11 and E-7. We believe this heap

has a small dimension, a few hundred feet in diameter. The

analysis showed no economic enrichment in base metals or PGM

in the heap. The following describes the best assays:

Two holes showing platinum: the highest value (87-1)

being 0,75 gr/t (0.022 oz/t) over 0,6 meters (2 feet). 87-7

with 0,21 gr/t (0,006 oz/t) over 5,9 meters (19.2 feet).

14

AIM •

Page 21: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

0+00 E 4.90E 8 + 00 E 12+ 00 E

- 38+00 N

-r

07-2 • • 87 -3

L-7

TR

EC

ES

SO

N

35+00 N

• •7-

• 07-7 • 07-11

17 • 17-10 •

17-4 • • 87-8

- 32+00 N

• •7-•

1

1

• Holes intersected heap

HOLES DL-87- I TO DL-87 --ta— including E-7

c 2g ig/2 -

DUMONT NICKEL Corp.

LAUNAY- TRECESSON Property CAMPAIGN 1987

FIGURE 5

SCALE FEET

0 100 200 300

Page 22: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Generally palladium was found in small quantities.

Three holes showed more palladium then others; 87-1 with

•••

0,89 gr/t (0,026 oz/t) over 3,0 meters (9.7 feet), 87-7 with

1,10 gr/t (0,032 oz/t) over 6,5 meters (21.2 feet) and 87-11

with 0,38 gr/t (0.011 oz/t) over 2,7 meters (9 feet). The

highest values (87-7) being 2,26 gr/t (0.066 oz/t) over 0,6

meters (2.2 feet).

Nickel is omnipresent in variable quantity 87-1 with

0,614% over 3,0 meters (9.7 feet), 87-4 with 0,415% over 6,1

meters (20 feet) and 87-7 with 0,611% over 6,5 meters (21.2

feet). The highest values (87-7) being 1,07% over 0,4 MN"

meters (1.4 feet).

Analysis for gold was done several times:

1) in heap, we found a small quantity (87-1 with 0,17 gr/t

(0.005 oz/t) over 1.2 meters (4 feet)).

2) in volcanics, returned traces, and ••••

3) granodiorite dyke returned traces.

We indicate in Appendix C the best assays and logs

reported in "other studies".

16

Page 23: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Geological aspect

In order to establish the nature of the different type

of lithologies met in our campaign, we carried out three

whole rocks analysis on a gabbro, a rhyolite and a granite

dyke. The results demonstrated (Appendix R) that instead we

had a peridotite a andesite and a granodiorite dyke.

The three last holes (87-12, 13 et 14), situated at the

west side of the property (lot 57, range V) aborted in

respect with a fault area, unfortunately couldn't get across

(Figure 6).

17

Page 24: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Microfilm

PAGE DE DIMENSION HORS STANDARD

MICROFILMÉE SUR 35 MM ET

POSITIONNÉE À LA SUITE DES

PRÉSENTES PAGES STANDARDS

Numérique

PAGE DE DIMENSION HORS STANDARD

NUMÉRISÉE ET POSITIONNÉE À LA

SUITE DES PRÉSENTES PAGES STANDARDS

Page 25: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

PRESENT WORK

The 1987 campaign consisted of several steps which are

described below.

- 14 diamond drill holes on targets (contact basal) for

a total of 3 812 meters (12 507 feet) (see Appendix A for

parameters of D.D.H.) carried out by Les Forages J.P.

Bérubé.

- Logging, sampling and analysis of the core for a

total of 127 samples over 101,1 meters (331.8 feet) the

analysis were made at Laboratoire Bourlamaque Inc. (see Best

assays in Appendix C).

19

Page 26: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

CONCLUSION

The 1987 exploration campaign over the Launay-Trecesson

property, prone that the Dumont Sill was rich in

significants values of platinum and palladium. The target

aimed was situated at the basis of the sill where we have

intersect a rich mineralization in Ni-Cu (hole E-7).

The work permitted us to partially identify the

mineralization. This mineralization, intercepted in holes

87-1, 7, 11 and E-7, appears open on the north-west side of

the ancient hole E-7 and south-east of the hole 87-11. The

values found in Ni, Pt and Pd are not economicaly reason.

The few analysis in gold research showed that this element

was associated in small portion to the highest values in Pt

and Pd.

We believe there is a good possibility of finding a

zone rich in Ni, Pt and Pd, because very few investigations

were made near the inferior contact of the sill.

20

Page 27: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

RECOMMENDATIONS

Following the results of the 1987 campaign, we

recommend another diamond drilling campaign;

1- to drill a few holes in the north-west direction of the

E-7 holes and south-east direction of 87-11 hole, to verify

if the mineralization stays open in those direction.

2- to carry on the exploration of the basal contact of the

sill especially where it is thickest.

3- jointly use a geophysical program (pulse Em) inside the

boreholes to increase the investigation of those holes. The

program should provide as much information as possible,

permitting us to minimize the drilling of holes containing

insufficiant datas in several area.

21

Page 28: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

RIBLIOGRAPHY

CARON, JEAN-CLAUDE 1987

Report on the Dumont Nickel property Launay-Trecesson Township; Les consultants Protec Inc., 9 p.

DUKE, J.M. 1986

Petrology and economic geology of the Dumont sill: An archean intrusion of komatiitic affinity in Northwestern Quebec; G.S.C., Economic Geology Report 35, 56p.

IMREH, L. 1980

Variations morphologiques des coulées méta-ultramafiques komatiitiques du sillon Archéen de La Motte-Vassan, Abitibi-est, Québec; Precambrian Research, Vo 12, p.3-30.

JAMES, N.F. AND MAWDSLEY, J.B. 1925

Mineral deposits in Desmeloizes and Trécesson Townships, Quebec; G.S.C., Summary Report, Part C., p. 78-81.

LATULIPPE, M. 1972

Val d'Or - Malartic Area; XXIV International geological congess Guide hook, Excursion A41-C41, p. 33-41.

WEBER, W.W. AND LATULIPPE, M. 1964

Amos-Barraute Area, Abitibi-East country; Quebec Department of Natural Resources, Geological Report 109, 69 p.

Page 29: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

APPENDIX A

PARAMETERS OF D.D.H. (1987)

LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORATION

Page 30: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

PARAMETERS OF D.D.H. (1987) LAUNAY-TRECESSON PROPERTY DUMONT NICKEL CORPORATION

.••••

No: Date Coord. Azimut Lenght DIP Meters (deg.) (feet)

Numb e r Lenght of sampled Samples Meters

(feet)

DL-87-1 30/09-4/10 4+00E 180° 304,8 5 3,0 34+00N 60° (1000) (9.7)

DL-87-2 4/10-8/10 4+00E 180° 411,5 4 1,8 36+00N 60° (1350) (6.0)

DL-87-3 12/10-16/10 6+00E 180° 404,2 27 15,7 36+OON 60° (1326) (51.5)

DL-87-4 16/10-21/10 6+00E 180° 304,8 23 20,2 34+OON 60° (1000) (66.2)

DL-87-5 21/10-28/10 8+00E 180° 305,4 10 5,3 34+OON 60° (1002) (17.4)

DL-87-6 3/11-6/11 2+00E 180° 304,8 10 11,0 34+00N 60° (1000) (36.1)

~ DL-87-7 28/10-2/11 4+00E 180° 267,3 19 16,6 33+00N 60° (877) (54.3)

... DL-87-8 6/11-9/11 2+00E 180° 289,6 7 6,0 33+10N 60° (950) (19.6)

DL-87-9 9/11-11/11 3+00E 180° 251.2 4 1,8 32+00N 60° (824) (6.0)

DL-87-10 11/11-13/11 4+00E 180° 224,6 2 2,4 — 32+OON 60° (737) (8.0)

DL-87-11 13/11-18/11 5+00E 180° 258,2 12 12,8 ... 33+00N 60° (847) (42.0)

DL-87-12 20/11-22/11 44+50W 220° 91,1 4 4,6 50+00N 70° (299) (15.0)

DL-87-13 22/11-24/11 44+50W 220° 78,6 0 0 50+00N 89° (258) (0)

DL-87-14 24/11-3/12 45+00W 220° 316,1 0 0 49+50N 70 ° (1037) (0)

Total 3812,1 127 101,1 (12507) (331.8)

Page 31: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

APPENDIX B

CHEMICAL ANALYSES OF WHOLE ROCKS (1987)

LAUNAY - TRECESSON PROPERTY

DUMONT NICKEL CORPORATION

Page 32: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

CHEMICAL ANALYSES OF WHOLE ROCKS (1987) LAUNAY - TRECESSON PROPERTY DUMONT NICKEL CORPORATION

OXYDE . ANDESITE PERIDOTITE GRANODIORITE DYKE CONSTITUENTS DL-87-1, DL-87-1, DL-87-1,

968,5-973,5 902,0-907,0 838,3-841,9

SiO2

60,30 39,30 63,80

TiO2 0,61 0,13 0,25

A1203 15,20 2,82 17,80

Fe203 6,53 10,70 1,98

Mn0 0,10 0,14 0,04

Mg0 2,76 33,70 2,30

Ca0 5,16 1,00 2,62

Na20 6,66 0,02 9,20

K2O 0,91 0,17 0,86

P205 0,44 0,40 0,30

LOI* 0,60 11,20 0,80

Total 99,27 99,58 99,95

Analytical Method

The concentrations of all constituents are tabulated as weighted percentages. All constituent are determined by plasma - emission except *LOI were determined by gravimetry.

*LOI = lost of fire

Page 33: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

APPENDIX C

BEST ASSAYS (1987)

LAUNAY - TRECESSON PROPERTY

DUMONT NICKEL CORPORATION

Page 34: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

)

NO: PT Pd (oz/t)(oz/t)

BEST ASSAYS (1987) LAUNAY-TRECES SON PROPERTY DUMONT NICKEL CORPORATION

Ni Au L From To Pt Pd Au L (%)(oz/t) (Feet)(Feet)(Feet)(gr/t)(gr/t)(gr/t)(m)

From (m)

To (m)

DL-87-1 N.D. 0.015 0.380 N.D. 2.0 937.9 939.9 N.D. 0,514 N.D. 0,6 285,9 286,5 N.D. 0.040 0.850 0.006 2.0 939.9 941.9 N.D. 1,371 0,206 0,6 286,5 287,1 0.022 0.047 0.990 0.004 2.0 941.9 943.9 0,754 1,611 0,137 0,6 287,1 287,7 N.D. 0.020 0.520 N.D. 2.0 943.9 945.9 N.D. 0,686 N.D. 0,6 287,7 288,3 N.D. 0.006 0.280 N.D. 1.7 945.9 947.6 N.D. 0,206 N.D. 0,5 288,3 288,8

DL-87-4 N.D. N.D. 0.310 2.0 437.0 439.0 N.D. N.D. 0,6 133,2 133,8 N.D. N.D. 0.410 2.0 439.0 441.0 N.D. N.D. 0,6 133,8 134,4 N.D. N.D. 0.330 2.0 441.0 443.0 N.D. N.D. 0,6 134,4 135,0 N.D. N.D. 0.333 2.0 443.0 445.0 N.D. N.D. 0,6 135,0 135,6 N.D. N.D. 0.339 2.0 445.0 447.0 N.D. N.D. 0,6 135,6 136,2 N.D. N.D. 0.470 2.0 447.0 449.0 N.D. N.D. 0,6 136,2 136,8 N.D. N.n. 0.420 2.0 449.0 451.0 N.D. N.D. 0,6 136,8 137,4 N.D. N.D. 0.580 2.0 451.0 451.0 N.D. N.D. 0,6 137,4 138,0 N.D. N.D. 0.540 2.0 453.0 455.0 N.D. N.D. 0,6 138,0 138,6 N.D. N.D. 0.420 2.0 455.0 457.0 N.D. N.D. 0,6 138,6 139,2

DL-87-7 N.D. 0.015 0.390 2.0 833.6 835.6 N.D. 0,514 0,6 254,1 254,7 0.004 0.020 0.430 2.0 835.6 837.6 0,137 0,686 0,6 254,7 255,3 0.016 0.039 0.820 2.0 837.6 839.6 0,549 1,337 0,6 255,3 255,9 0.013 0.035 0.790 2.0 839.6 841.6 0,446 1,200 0,6 255,9 256,5 0.006 0.023 0.500 2.0 841.6 843.6 0,206 0,789 0,6 256,5 257,1 0.006 0.020 0.495 2.0 843.6 845.6 0,206 0,686 0,6 257,1 257,7 0.003 0.066 0.650 2.2 845.6 847.8 0,103 2,263 0,7 257,7 258,4 N.D. 0.015 0.500 2.3 847.8 850.1 N.D. 0,514 0,7 258,4 259,1 N.D. 0.016 0.480 2.2 850.1 852.3 N.D. 0,549 0,7 259,1 259,8 0.009 0.034 1.070 1.4 852.3 853.7 0,309 1,166 0,4 259,8 260,2 0.009 0.019 0.880 1.1 853.7 854.8 0,309 0.651 0,3 260,2 260,5

DL-87-11 N.D. 0.004 0.157 5.0 814.5 819.5 N.D. 0.137 1,5 248,3 249,8 N.D. 0.026 0.910 2.0 819.5 821.5 N.D. 0,891 0,6 249,8 250,4 N.D. 0.012 0.350 2.0 821.5 823.5 N.D. 0,411 0,6 250,4 251,0

N.D. = Means (less than 0.002 oz/t or 0,069 gr/t).

Page 35: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORATION

DIAMOND DRILL LOG

Property : LAUNAY-IRECESSON

noie t _,-i ;r,!onsnip fRELE:,ûLJi9

Lot , .,, Fange: '_laiE; 4 .2:8:8:2--i

Date si-.Nr't:ei; C0:..'t0 "*, IY8I

Date cGmpl's'rr'L'.0:.108Ei; l'6)

Level Section 00L

L711ar Loorot?tiate Line . Ljtl t i.iü ': AiŸ-..!:!i N Azimuth: i89' 9:

Station.: 34+00 (A

;iGartUrP: 409.00 E Dip . -t"' j'

Eja..'dt:nrt; :Ï,iiIJ i enat h . 1090.0 :t

Deviation tests Death Dip Azimuth

CO MN 200.0 Ft; -62'0'

atMD ~ 400.9~.Ü 'Et : -b;'- 0'

C ® (/I 0 800,0 kt i -8;i' fl:

-% 00 n rT7 800,0 Ft; i -Ltz" (.!' Qh 04 L- I? ~ 1000,9 }}; -1O6' 0' 6 = C

~ f-- Au Au .,.~ ~ m

c.®

Remarks :Calii"nt} pulled out, 8.11. size

Laboratoire voi.rt?alaaltN Ltee

Samples t 2901 to 1005 incl.

Lopped oy . h.HER J AI D

Ministère de l'Energle e1 des iRestources Service de !a Géoinfotmation

Datt 2 7 0 CT 1988

No G.Iw_ 47388

~ ~

E. 00 '11 ô _. Ln C:

cz ~ ~j C7

1'"7

Page 36: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

--------• - ------- DLSLRIFTION FROM : 10

(Fti

:------

:Saabie: fEUM (ti L I Ft ; P0 NI Mu

(ft):ozit ozit Juzit

1 1 I 1 I 1 I 1 I I j 1

LPILINf211- -IREuESSuN LOW N1CKEi. LORPOOFION Hole : B1-1 PAGE:

0.0: 43.01 CASING

43.01 310.41 Massive medium-grained, dark olive green, altered dunite. Much magnetite

between and around (fltvine crystais. Scattered sulfides.

43.0- 44.0

Lightly ROUa aitereo, grey-oreenist.

44.0- 142.6

Dunita with saail aagnetite yetnlets. Serbentinized fractures (20'-

40/C.A.), Scattered dzvet-,Lut threads,

142.6- 152.0

•ounite more altered. Serpentinized fractures (1 -fLiY,,,f_;.Ai

asbestos threads.

152.0- 268.8

Some as 44„0 to, 142.6,

268.8- 272.1

Very serbentlnized, sereentinized fractures LJ with

asePstos. threads.

272.1- 310.4 Sue as 44.Q ta i'z..

1 310.41 692.11 some as 43 to 310.4 but more serbentinized. Fine grained and more asbestos

threads In fractures,

311.0- 322.6

Serpentinized fractures t4u --1(')L,A.) with asbestos threads.

394.4- 402.9

Very serpentinizeo fractures w,-40/u.A.) with asbestos threads.

Page 37: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAONAY-IRECESSON DOM NICKEL COE,PBAIION Hole # 3

: [-ROM Ui;

(Fti ;,EtI

;---

DESLRIFfION

lbamplei EhON Ui L Ft ; Fa . Ni ; Mu

iEt).ozit iozit

414.5- 417.2

'Eame as 34.L. to 4v2..,.

422.0- 452.0

Small mineralization of disseminated suifides.

447.0- 460.0

Serpentinizee fractures U0'-S5'/U.A.I with asbestos threads.

510.0- 518.0 Serdentinized fractures Ci-S5C.A.I.

533.0- 536.0

Serpentinizea fractures (0-851C.A.).

611.0- 692.1 Mun sereentinIzed fractures :35'-8:5'/L.A.).

1 692.11 834.01 Massive, fine grained, grey-greenish, altered peridotite. Serpentinized and 1

carbanatized +flied fractures t.S0''-85'/U.ili.). MatInetic disseminated fine

cirai ne suifices.

692.1- 692.5

In sereentinizea fractures.

794.0- 795.0

Sereentinized and carbonatized fractures

1 834.01 947.61 Massif, fine grained to medium drained, black peridotite magnetic. ; Uisseminated fine drained suifides. Linntiv serpentinized and carbonatizea

; fractures.

;

Page 38: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CURPORAT N Hole 87-1 .PAGE: 4

1 FROM 1 TO 1

I (Ft) 1 (Ft) 1

DESCRIPTION

838.2- 842.0 Light grey coarse-grained porphyritic granodiorite dyke. Massive 55/C.A. contacts.

!Sample! FROM 1 TO 1 L 1 Pt 1 Pd 1 Ni 1 Au 1 ! : (Ft lozit ozit 1 )i 10z/t 1

: 1 1 1 1 1 1 1 1

1 842.0- 845.4

Oabbro with anastomoged veinlets of feldspar and serpentine.

854.6- 855.1

Velniets and small heap of sulfides,

1 868.0- 870.0

1

CardonatIzed velniets and veinlets and snail neap of sulfides,

877.0- 914.0 1 Disseminated sulfides and sometimes in veinlets of heap.

Disseminated and veinlet of sulfide 2-31.

, DisseminaLed and veiniet of sulfide 5X, 1

1

Disseminated and velniet of sulfide 57.. 1

Disseminated and veiniet of sulfide 5Z. '

1

Disseminated and veiniet of sulfide -11%.

Sulfide= (Pentlandite + pyrrhotite and chalcopyrite ttrace)1

20011

I

2002;

1

2003: . .

20041

20051 .

..

1 .

1

1

937.91

! 939.91

1

941.91

1

943.91

945.9; 1.71

939.91

I

941.91 .

943.91

1

945.91 .

947.6;

2.01

, 2.01

. .

2.01 , .

2.01 . .

. ,

1

N.D.1 0.015: 0.3801

. . .

. ,

N.D.1 0.0401 0.8501

. ,

. .

0.0221 0.0471 0.9901

. . •1 . .

M.D.) 0.0201 0.5201

. . 1

M.D.; 0.0061 0.2801

M.D.) .

0.006;

0.0041

:

M.D.)

NA.;

:

,

1

1 947.61 1000.01 Light grey, andesite, non-magnetic, disseminated sulfides, carhonatized and

1 silicified filled fractures (54-80,/C.A.).

1

: 1000.01 Ind of hole

1

Page 39: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I 1 I I I I 1 1 I I I 1 I I I I i I

L j}%JNP-iRËi.ESSON ;_ . C NICKEL _r r_NH OJ „a ie Lr_. °_,; o- E:

}R'it1 , TO rFtJ , rttl

:.IEjL^..k I :'.:f$ ,Sa:iiplei FJ*Cii? , IiJ ; L N% i FC C11 Jiu

(Ft) :oz-t ;o.it ; Y. -I i -- - --- I -•_-,_ .._ , , _.---_.`- , f i j

Total amount e} samples=

iota' ieillyth sampled - ;'.;'Ft

Page 40: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

UNIONI NICKEL CaPRAIIUN

OIAMUND DRILL LO6

Property : LAUNAY-1RECESSUN

Hol; $ ; iownsflip: NEL.Es8UN Lot : ih

L2Vel

hanqe: V Lfaim 4 :26161'2-1

Section: 4 LIO;

Date starteri :OLfOBE8 196) Bate cpm5leted:UOJBE8 1981

Lollar cnordenate 4+00 E

Latitude: ;3600.U9 N

Hzimutri; 160' D

6tat3on: ,QE+60 N

Departure: 400,00 E

Dip 0' Eievatifin: 0.0f•J f

ite on tests Depth Oip

kzimutn

I

;

Remarks fUasinp sulled out. 8.0. size Laboratoire Douriafflaque Ltd. Smples # 2006 to 20Ui

Lopped by : ROBERT OSWALD

Page 41: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

) I I I I 1 I I )

t

LAUNAY-TH BSA OUMOW NiaEL t.ORRO ALION Hole it

FROM ;

(Ftt tEt)

DESCRIHILON

;Samie hu: IN L Pt Pd NI ; Au

kfrtl;lizit :ozit ;Uzit

0.01 22,0: CASING

22.01 487.0: Massive, medium grained, dark olive green, altered dunite (peridotite).

; Oucn osonetite between and around oilvine crystals, Aiso Aagnetite

veinlets. scattered sulfides.

22.0- 32.0

Litiit1v serpentinized dunite lperidotiteh

32.0- 80.0

Coarse-orained, altered dunite ,beridotite with serpentinized

fractures (30'-5::?)

154.6- 156.3

Serpentiftized fractures il(?i .N.i with asbestos threads f,dunItei.

188.4- 191.6

Fractured IfPIC.A.) and a.erpentini7ed witn asbestos tnreads.

260.0- 218.6

Altered serdentinuen fractures -55'if:,A.) witn asbestos threads:

303.5- 301.0

Altered serpentiniLed fractures C,.15,C.11.) witn asbestos threads and :

Aadnetite yeiniets

324.5- 328.0

highly serpentinized and fractured dunite with asbestos threads.

394.5- 396.3

hitered, sernentInized fractures 10'.iL.A.) with asbestos threads.

402.6- 407.0

Altered serpentinized tractures 110 and 5tL.uu. I with asbestos

threads.

Page 42: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

)

LALINe-fRECESSON DUMONF NICKEL COPPORATIUN Hole

-------- - - -

; ERUN 10

ihti ! (Ft)

DESCRIPTION

h'OM ! ID L Pt ! Pd i Ni ! Au

! iFt)!OzIt ioz/t % 10zit

;

418.7- 420.4

Aitered, serpentinized and carbonatized fractures (20-7P'1C.A.) with !

asbestos threads.

426.5- 430.0

Hitered seroentinizen and carbonatized ractures iiv and 4Gui'.

with asbestos threads.

459.9- 462.6

Hiteren seroentinized and cartonatizen fractures (0-10,L.Aj with

asbestos threads.

476.4- 477.0

Coarse-drained olivines with madneti,e,

1 487.01 553.01 Some as above (dunite) but more altered and coexistence coarse-medium

; brained. OissemInated serpentinized asbestos threads and sernentinized

; fractures i10-41.PlU.A.).

527.0- 528.8

serpentinized fracturP= N.,0/L,A.1 w,tn asbestos tnraon

538.6- 540.3

Serpentinized fractures, (40C.A.) with asbestos threads and mabneti- !

te veinlets (30-40/C.A.)

1 553.01 842.61 Some as above (487-5531 but few altered with magnetite veinlets (20-85/C.A.)

599.9- 600.5

Coarse-drained duni e.

Page 43: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 I I I I I I 1 1 I I 1 I 1 I I I l i

LA!?tdeiv fHFCEÿ5O _ ~'UMilydl 411,K EL i.l.h.l-lïF.F;! IÜtd Hole 4 r'ïi:it.: 4

; FROM . i4

ifti r' iFt) .

Ot S' 8 i!"' 4 i0

i'ic.:;tG'ei FF';,iK i i; L ;!-'t i8o , Ni : Au

+.f•L)i8Cit ;lii`t i .. itl:it

616.0- 617.6

H1=e-etl [email protected]:za fracture (2(.0/L.A.) with ashnct.s threads,

659.0- 667.0 Riterei: s:'roentinizLd fracture '.!'.'°;Î_.H.) W.:tn asbestos tr!'edC5.

686.6- 687.3 `eril?nti'11;:ed fracture ii?''?L,H,. wit?? =.seesfos t`rea3=.

1 842.61 938.01 Massive, fine grained, grey-greenish, altered peridotite. Serpentinized

and carbonatized tl11Cc fractures ,20-8 /L.H,1.Magnetic- disseminated

; fine grained sulfides.

842.6- 852.0

àeroEn!tlnizcd fracfures f10'-4(P/L.A.

1 859.0- 863.5

borrcnLi:n.lzed ana carC'onatl'ed fil el fractures ,:i''"'!`:L,ti...

865.5- 865.7

verÇeiat.nlzed and car, oniatized filled fracture (A"

1 938.01 1103.91 Some as above with numerous serpentinized and carbonatized stringers.

989.2- 989.4

1 1ï2" mud seam,

989.2- 1111.0

1 172° mud seam.

1 1103.91 1221.61 Massive, fine grained, black peridotite. Magnetic disseminated fine grained

1 sulfides. Llgntiy seroentinizen and carbonatized fractures witd small vein-

let of magnetite.

Page 44: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

2. •

LAPNAY-TRECESSDN 1)UMON1 NICKEL LUHPUNAI10N

Hole : 87-2 t-14HEI

FFUM 10 i DESCRIPTIO :Sample; HON : 10 L! Ft 1 Fd ; Ni

(1.t)107.it 1ozit %

1111.0- 1111.6

Very silicified ann caroonatizmi white dranddlorlte nyle aItered).

1111.0- 1118.1

Light grey coarse-grained silicified. branoatorite d:ke,

massif 45'/L.1. contact.

1

1118.1- 1213.3

Numerous carbonatized fractures l30-91P/C.A.) and sometimes hiled

with magnetite or serpentine. Disseminated sulfides.

Disseminated su;il'Ides lpentiangite: 2:1

1213.3- 1214.4

Etrecclated filled witn carbonate.

!

"2009: 121.1/.0! 1208.5; 1,D; N.D.; N.D.

1

0.330; —1

Disseminated and velniet of sulfide 1%. Aii.)6: 121 1,1; 121Y.1; 0.14ki;

Disseminated and vein et of sulfide :t1%. l'21Y.1; iU.5 I N.U,; N.0 N.O.;

Disseminated and velniet of sulfide 2%.

1 1221.61 1350.01 light grey andesite, non-magnetic.

1 1223.2- 1226.0

few neaps of strinner ovrrhotite 160'iC.A.

,-!E:D; N.D.;

1322.5- 1335.8

Massive, medium grained, dark grey diorite. Pyrite disseminated and

heaps in veiniet (quartz and carbonate) bOiC.A. contact-

! 1350.0; ;End of hole

Page 45: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

EAW. %-%waew ym% %awLUFeb@wN Hole #:£e we;

Ra: TO 1 (F!) ; (Ft) ;

Sv6Rgw

%aGy FHOM; G ; L ;R :R @ ;% ~ ~ : :+b:e» %£t :: ;eJ

Totalae4 of e¥Ds 4 Total SRRsampled = s»!

Page 46: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Date started :OCTOBER 1987

Date coepleted:OCTOBER lŸ87

Latitude: 3600.00 N Azimuth: 180"

Departure: 600.00 E Dip : -60e 0'

Elevation: 0,00 Length . 1,326.0 Ft

Level

Hole # . 87-3

Township: TRECESEON

Lot . lA Fange: V

Section:

Collar coordonate : Line : 6+00 E

Station: 36+00 N

Claie # :28181'-1

1 I I I I I 1 I I I I I 1 I I I I I 1

DUMONT NICKEL CORPORATION LTD

DIAMOND DRILL LO6

Property : LAUNAY-TRECESSON

Deviation tests

Depth Dip ; Azimuth

200.0 Ft; -63" 0' 0u

400.0 Ft; -6i" 0' ù" 600.0 Ft; -62" 0' 0'

800.0 Ft; -61" it' 0'

1000.0 Ft; -60' 0' 0"

1200.0 F t;-;;6" 0' Ù"

1326.0 Ft1 -57° 0' 0' ;

Remarks :Casing pulled out, B.O. size

Laboratoire d'Analyse Souriaeapue Ltee

Samples * 2010 to 2036 incl.

Lopped by : RUBERI OSWALD

Page 47: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

e

LAUMAY-TRECESSON DUMONT NICKEL CORPORATION LTD

Hole It : 57-3 PAGE: 2

FROM ; TO 1

DESCRIPTION

:Sample; FROM ; fO ; L ; Pt ; ea ; Ni i Au :

(Ft) (Ft) ;

4t);Ozit ;Gzit

;

0.01 47.01 CASINO

1

47.01 162.01 Massive coarse-grained, dark olive green altered dunite. Much magnetite

; between and around olivine crystals. Scattered sulfides.

47.0- 98.0

Well serbentinized fractured, asbestos threads and erythrite.

74-1 1/2 mud seam.

100.0- 103.6

Altered and serpentinized fractured (30/C.A.).

102.7- 103.6

Seroentinized fracture with magnetite veinlets.

103.6- 137.0

Well serbentinized ana fractured.

137.0- 162.0

More altered and serpentinized fractures (45') often filled with

asbestos threads.

162.01 566.01 Massive medium grained, dark olive green, altered dunite. Much magnetite

between and around olivine crystals. Also magnetite yeiniets. Scattered

: sulfides.

191.0- 199.4

Serpentinized fractures W-3041C.A.). Filled with asbestos threads

and erythrite.

210.6- 217.0

Low angle serpentinized fractures (10/L.A.!, scattered asbestos

threads.

Page 48: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORPORATIUN LTD Hole # : 87-3

FROM I TO ! DESCRIPTION ;Sample; FROM ; TO I : f't ; ea :Ni ; Au

(Ft( I (Ftl I ; : : (Ft);Ozit :Oz/t 1-4 ;Ozit ;

265.4- 268.0

Serpentinized fractures QV/C.A.), filled with asoes os threads

and magnetite velniets.

268.0- 296.0

Seroentinized fractures (50-70/C.A.), filled wIth asbestos threads

ana erythrite. ;

371.0- 380.3

Altered and seroentinized fractures (low angle) with asbestos threads.;

392.0- 396.0

Seroentinized fractures (low angle) with asbestos threads.

426.0- 438.0

Seroentinized fractures (20/C.A.).

447.3- 468.0

Highly altered and seroentinized fractures low angle.

486.0- 493.0

Coarse grained aunite.

502.0- 536.0

Altered and seroentinizet fractures (20/L.A.). filled with asbestos

threads and magnetite velniets.

I 566.01 818.01 Same as above but more altered and coarse-grained to medium grained.

; Scattered suifloes.

582.0- 593.0

Altered and seroentinized fractures (20-70/C.A.)

Page 49: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I I I I I I I I I I I I

LA?INAY-TF:EL:ESSON DJMiiNT NICKEL CORPORATION LTD Hole #. 87-3 PAGE: 4

FROM 1 TO

(Ft) . (Ft) ;

t t

:,}ESCF:IPTI)N ;Sample; FROM . 10 . L .t ; f'd ; f:i ; Au

; , ; (Ft) ;1171t ;Üz,'t ; : ;11zlt ;

~~_----.t ~ . , . t ------ , s .~ ~ , i t

, . .

596.0- 615.0

Ditto.

617.0- 620.0

Hiohjy altered, serpentinized fracture with asbestos threads.

644.0- 657,0

Altered serpentinized fracture (30ù L.A.), with asbestos threads.

668.0- 670.0

Altered serpentinized fracture (10j' and 60'/C.A.) with asbestos

thread.

707.5- 711.0

Altered sereentinized fractures (low angle) with magnetite vein)et.

726.6- 729.0

Serpentinized fracture !.low angle).

761.0- 775.5

Altered serpentinized fractures 125-70'/L.A.), with asbestos threads.

1 818.01 1124.51 Massive medium grained, serpentinized peridotite, magnetic, disseminated fine 1

t grained sulfides sometime eruthrite In fractures.

818.0- 902.0

Serpentinized carvonatized fractures (51J'10°/I.e.'rl.I and magnetite rich i

veinlets (45-85a/C.A.1.

907.0- 954.0

Altered ceridotite with carbonatized serpentinized fractures

(25-85YiL.A.) and asbestos threads.

;

;

Page 50: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1

LA AY-TRECESSON DUMONT NICKEL CORPORATION LTD

Mole m : 87-3 PA6E: 5

FROM i TO : DESCRIFI1UN ;Sample; FROM i Tu . L ; Pt ; Pd ; NI ; Au (Ft) ; ;Ft; ; , (Ft?;u2/t ;Oit 1% ;Dzit

954.0- 986.0 Ditto.

986.0- 1089.7 Altered peridotite, seroentinized caroonatized fractures (45-651C.A.). Sometime filled with magnetite veiniets.

Talcose.

1089.7- 1099.2 Altered pendante, talcose.

1099.2- 1124.5 1 2011; 1099.2: ii01.2 , 2.0; N.D.; Nd.; 0.148; ;

Peridatite with fine-grained sulfides. ; !

Disseminated sulfides. 2012; 1101.2: 1103.2. 2.0: N.b.; N.D.i 0.116!

Disseminated sun:Ides. 2013; 110).2, 1105.2: 2.0; N.D.; N.O.; 0.140;

Disseminated sulfides. 2014; 1105.2; 110.2; 2.0; N.U.: M.D. 0.185;

Dissem natea sulfides. 2015; 1101.2; 1109.2. 2.0. N.D.; N.D. 0.1621

Disseminated sulfides. 2016; 1109.2, 2.0; N.D.; N.D.: 0.18.51

Disseminated sulfides. 2017. 1111.2, 1113.; M.D.; N.D.' U.228.

Disseminated sulfides. 2018: 1113.2; 1115.2; 2.u: N.D.; N.V.;

Disseminated sulfides. . 20191 1115.2 1111.2: 2.0; M.D.! N.U.; 0.220;

Disseminated suifides. 2020; 1117.1; 111,, 2; 2.0; M.D.; M.D.; 0.1/1:

Page 51: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION LTD Hole II : 87-3 PAGE: 6

: FROM TO

DESCRIPTION

:Sample; FROM 1 TO 1 L Pt Pd Ni ! AD

(Ft; (Fti

(Ft?;02/t 0zit

Disseminated sulfides.

Disseminated sulfides.

Disseminated sulfides.

;

1 1124.51 1236.31 Altered serpentinized peridotite in talc. Disseminated sulfides.

1124.5- 1151.0

Lightly altered per dotlte in talc.

1151.0- 1236.3

Very altered per dotite in talc.

1156.3- 1157.2

White talc and carbonate stringers.

20211 1119.2: 1121.2; ,!....). N.b.; v.092: 9.249: 1

2022, 1121.2: 112.2; .2.9; N.u., N.u.: 9.166:

2023; 1123.2; 1124.5: 1.3' N.D.: N.D.; u.255;

1193.0- 1194.2

Darkv grey coarse grained, porpnytic granollori e dyke massive.

45'/C.A. Contacts no-magnetic.

1 Disseminated and seau i neap of sulfides H.

1223.5- 1227.0

Scattered white talc and carbonate stringers.

1 1236.31 1326.01 Light grey andesite, non-magnetic. Disseminated sulfides and veinlet or

heap sulfides (1252-12121.

Disseeinated sulfide.

2010; 1215.6: 1216.4; 0.8; N.D.; M.D.; 0.132;

2024; 1252.0; 1254.0; 2.0; N.D.;

1

Disseminatea sulfide with small veiniet sulfide. 2025: 1254.0; 1256,0; 2.0; N.D.;

;

Page 52: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I i I i I 1 I 1 1 1 1 I I I ! 1 1 f I

LAI;Nf({-TRE1'ESSGN D1:MGNT NICKEL CORPORATION LTD Hole #. 87-3 PAGE:

1 FROM 1 TCl

(Ft) ; (Ft) 1

DESCRIPTION ;Sample; FRC't? , Ti? . L; Pt , Pd ; Ni . 4u

; , . (Ft);ilz!t 111z1t ;'l. ilztt

, . . i ; 1 i , 1

Disseminated sulfide with small veiniet sulfide. 2026i 1256,0; 1258.1 ; 2.('t; N.D.; N.il.; N.D.;

~ .

Disseminatedsulfides and small hf criateû 1/2; 2027; 1258.0; I26. .0' ..û ; N.r., N.J., i.4. ,

filled sulfide,

Disseminated sulfide.

Ditto.

Ditto,

Ditto,

Ditto and fracture 112° filled sulfide (35'IC.;.1.

Ditto and small veiniet.

Ditto.

ureccia.

1311.3- 1315.4

treccia with carbonate ciment.

Srec.ci a.

1323.1- 1326.0

Massive, medium grained, dark grey, porphyritic diorite.

Disseminated sulfides in fractures. 301C.A. Contacts.

1326.01 ;End of hole

2028; 1250.0: 1..82.0i d.'.i; N.D. i N.I'.. N.:...

2029; 1252.0; 1264.0; 2.0; N.Q. i N.D.. N.U.;

, 20301 1264.0; 115:.0 2.0i N.D.; N.D.;1Ÿ.D. ï

2031: 1266.0; 1168.0; 2,0; N.D.; N.D.: N.D.;

1 1 .

2032; 1268.0; 1270.o;2.0; N.0.1 N.D.i N.D.;

2033; 1270.0; 1212.0; 2.0; N.D.; N.D., N.D.;

24341 1272.01 127 3.01 1.0; N.D.; N.D.; N.D.;

103"i }: 1313.0; 2.01 fR;

2036; 1313.01 1315.41 2.4; ; TRI

Page 53: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

)

LAIMAY-TRECESSON DUMONT NICKEL CORPORATION LTD

Hole il : 87-3 PAGE: 8

; FROM TO

DESCRIPTION

;Sample; FROM ; TO L 1 Pt ; Pd Ni ; Au

(Fti

(Ft);Ozit Ozit i% ;Ozit

Total amount of sample = 27 Total length sampled = 51.5Ft

;

;

1

Page 54: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 I 1 I I I I 1 1 1 I 1 1

DUMONT NICKEL CORPORATION LTD

DIAMOND DRILL LOS

Property : LAUNAY-TRECESSON

Hole # : 87-4

Date started :OCTOBER 1987 Township: TRECESSON

Date coepieted:UC(U8ER 1987 Let . 14

Range: V Claim # :281812-1

Level Section: 6 + 00E

Collar coordonate : Line : 6+00 E

Latitude: 3400.00 N Azimuth: 180' 0'

Station: 34+00 N

Departure: 600.00 E Dip : -6`i?' Ù'

Elevation: 0.00 Length : 1000.0 Ft

Deviation tests Depth Dip t Azimuth

i:ut!.".i Ft; -63' 0' 0" ;

400.0 Ft; -60' 0' 0' 600.0 Ft; -63' 0' Ù' g(}.!,i! Ft -63' 0: 0"

995.0 t-t; -594 ;,: +1" t 18/' +„y' 0"

Remarks :CASING PULLED OUT, i;0 SIZE LABORATOIRE D'ANALYSE SOUI?LAPiADUE LTD SAMPLES # 2037 TO 2059 INCL.

Legged by . ROBERT OSiALD

Page 55: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 I 1 1 1 1 1 1 1 1 1 1 1 1 I I I 1

ïAtiNAv-1RECE:BFtN OtIMüNT NICKEL CORPORATION LTG

Hole ; . 87-4 PAGE: 2

FROM 1 ?0

(Ft) ; (Ft)

DESCRIPTION ;Sample; fsiOf? , ÏO , .. . Pt , Pd Ni G ;

4t)lUz?t ;O;z+t

0.01 20.0 CAS1N8

20.01 257.0 Massive, coarse grained, dark olive green, altered dunite. Much magnetite

between and around olivine crystals. Scattered sulfides.

23.2- 33.5

Highly altered and serpentinized fractures (15'/C.A.).

71.5- 76.0

Seroentinlzed fractures (10-454 tC.A.;).

77.0- 93.2

Highly altered and serpent raze, fractures i?;-25°i{L.M.i with

asbestos threads.

107.5- 119.0

Serpentin.zed fractures (159-25Ù/C.AJ with sometimes magnetite

veinlet.

138.0- 148.0

Serpentin zed fractures (154-204ic.A.

157.0- 179.0

Altered and serpentinized fractures (10$ and 854 î:.A.) with

asbestos tnreads and magnetic veinlets.

226.4- 227.0

Seroentinized fractures (354)C.A.I.

241.8- 255.0

Highly serpentinized and altered fractures (15-454 /C.A.).

257.01 347.01 Same as above but sore altered and disseminated asbestos threads.

} ; .

Page 56: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 ! I 1 1 1 1 1 I I 1 I 1 I 1 I 1 1 I

LAUNAY-TREt .FLN DUMONT NICKEL CORPORATION LTD Hole iE : 87-4 PAGE: 3

; FROM ; TO

(Ft) ; (Ft)

DESCRIPTION ;Sample; FROM , TO . L , Pt . Pd , Ni 'L ; . . , i['.,,O,i. ;Ozlt i ,

284.0- 290.0

Serpentinized fractures (40-60'ic.A.) kith asbestos threads.

347.0; 693.5; Massive, eediva grained, dark alive green. Altered peridotite. Magnetic.

Scattered sulfides.

407.0- 412.0

Mitered and serpentinized fractures (low angles).

437.0- 457.0

More disseminated visible sulfide.

Disseminated sulfide. 203?; 431.v; 431.01 2.0; N.D.; N.D.; 0.31v;

Disseminated sulfide. 2038; 439.0; 441.0; 2.0; N.D.; N.D.. 0.410;

Disseminated sulfide. 2039; 441.0; 443,L; 2.701 N.O.; N.D.; U.350; 1 i !

Disseminated sulfide. 204v; 443.0; 445.0; 2.0; N.i).; N.D.; 0.333

Disseminated sulfide. 2041; 445.0; 447.0; 2.03 1 N.D.; N.D.; 0.3391

Disseminated sulfide. 214~; 447.v; 449.0: :.v' N.D.; N.D.; 0.47v;

Disseminated sulfide. 2043; 449.0; 451.0; 2.o; N.D., N.D.; 0.4211;

Disseminated sulfide. 2044i 451.0. 45.3.E/i 2.1; N.D.; N.D.; 0.580i

Disseminated sulfide. 2045; 453.0; 455.0; 2.0; N.D.; N.D.; 11.540;

Disseminated sulfide. ; 2046. 455.0; 45/.v; ..ü; N.Q., N.D.. 0.4'20;

Page 57: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUMAY-TRECESSON DUMONT NICKEL CORPORATION LTD Hole # : 87-4 PAGE: 4

; FROM 1 TO

; (Ft) ; (Ft) DESCRIPTION !Sample; FROM ; TO L ; Pt Pd Ni XI

(Ft)!Ozit ;Ozit

503.0- 548.0

Altered serbentinized fractures (10-25'iC.A.) with magnetite

veinlets and or asbestos threads.

548.0- 607.0

Numerous serpentinized, carbonatized ractures (30-80/A.C.) with asbestos threads and erythrite.

607.0- 667.0

Ditto.

670.0- 671.0

Fracture (Itiv/C.A.) filled with carbonate, serpentine and magnetite.

1 693.51 887.01 Massive fine grained, yellowish green altered peridotite, magnetic, ; disseminated fine grained sulfides.

697.0- 702.0

Righlv altered and serbentInized fractures (low angle).

702.0- 722.0

Serpentinized, carbonatized fractures

722.0- 737.0

Seroentinized, carbonatisen fractures (30-60'/C.A.).

737.0- 762.0

Ditto.

762.0- 768.0

Seroentinized, carbonatised fractures (low angle) and magnetite

veinlet.

Page 58: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LHuNAY-TRECESSON DUMONT NICKEL CORPORATION LTD Hole It : 87-4 PAGE: 5

FROM ; TO ; DESCRIPTION ;Sample: FROM ; TO . L: Pt . Pd + Ni X.

(Ft) !Ft! ; (Ft);Lz,t ;fJztt . ,

, , __._

, , ; ~ , • ~ ~

768.0- 808.0

aereentinized. carbanatized fracture E30-604!r.4.1.

808.0- 809.0

Seroeritinizea, cartonatized fractures I354,C.A.i.

809.0- 827.0

Serpe;itinized, carh[lnatized fractures i4Y!L.4.i.

827.0- 848.0

More altered (talc and serpentine), carbonatized fractures (10* and

601/C.A.) with magnetite veinlet.

847.0- 849.2

Carbonatized and sereentinized fractures 1O"tC.iT.) with magnetite

vs in let.

849.2- 869.0

Seroentinized and carbonatized fractures (0-85°IC.t;.).

869.0- 883.0

Ditto but more fractured.

883.0 951.01 Massive fine grained, black altered peridotite, weakly magnetic, disseminated

sulfides.

Disseminated sulfides 3:. 2047; 883.0; 884.!); 1.0; N.D., 0.010î 0.890)

885.3- 890.2

Lign grey, coarse grained silicified. 8ranoaiorite ayke, massive

40°!C.F., contact non-magnetic.

Page 59: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION LTD Hole 4 : 87-4 PUE:

: FROM ! TO ;

; (Ft) 1 (Ft) 1

DESCRIPTION ;Sample; fROM 1 TU ; L ; Pt ; Pu ; N I. ;

(Ffl:ezit 10z/t

;- -;

890.2- 930.6 1 Cartonatized fractures (25-45'IC.A.).

More disseminated sulfides.

More disseminated sulfides.

More disseminated sulfides (chalcopyrite trace).

More disseminated sulf des.

More disseminated sulfides.

More disseminated suifides.

More disseminated sulfides.

more disseminated su'fides,

930.6- 934.5 Ditto (985.3-890.2, dyke...) 501C. - Contact.

;

2048; 991.3; 896.1! 4.8; N.U.; N.U.; 0.1961

: 2049: 296.1; 900.6: 4.7: N.0.: N.D.; 0.210;

2050: 900.8; 9O:J.61 4.b. N.D.' N.u.. 0.120;

L01; 905.6: 910.4. 4.5 M.D.; N.U. 0.148

.102. 910.4: 9111.1, 4.7. N. M.D.; 0.142:

205o, -715.11 919. 4.8; N.0.; M.D., :.).2101

2054: 924.61 4 M.D.; 0.220:

2055: 924.8 4.7: N.J., N.D.! 0.171:

934.5- 948.0 Breccia filled ca dilate ana angulars fragments Ideridetite).

1 951.01 1000.01 Light grey andesite, non-magnetic. Disseminated sulfides. 30'/C.A. Contacts. 1

Disseminated sulfides (contact peridotitetandesite). ; 2056; 951.0; 952.0; 1.0;

Veinlet and email neap su fides. 2057; 957. ' 959.8; 2.2;

Veinlet and soaii Mean sulfides. 2058t 959.8; 961.5: 2.0:

0.006:

--; --; 0.022:

0.006:

Page 60: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I I I i I I I I I I I I

LAJ!dAY-irtEl.EShON DOW NICKEL CORPORATION LTD

Hole 4 . b1-4 PAGE: 1

, FROM ; TO ,

Ft! : tFtf

:ieiniet and small heap sulfides.

1000.0; ;End of hole

Total amount of sample = 23

Total ienottt saaoied = 66.2Ft

;Sample; FROM . TO ; L; Pt , Pd ; Ni Z; ;

, , (Ft);ilzlt ;tlzrt , ; ~

, ; ; ! : ~ ~ ; . i

2059; 96i.8; w63.01 ..U; --. --. 0.0051

DESCRIPTION

1 i i ;

Page 61: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORATION

DIAMOND DRILL LOS

Property : LAUNAY-TRECESSON

Hole # : 87-5

Date started :OCTOBER 1987 Township: TRECESSON

Date completed:OCTOBER 1987 Lot : IA

Range: V Claim # :281812-1

Level : Section: 8 + 00E

Collar coordinate : Line : 8+00 E

Latitude: 3400.00 N

Azimuth: 180" 0'

Station: 34+00 N

Departure: 800.00 E

Dip : -60' 0'

Elevation: 0.00

Length : 1002.0 Ft

Deviation tests Depth Dip Azimuth

200.0 Ft 1 -62' 0' 0"

400.0 Ft: -61' 0' 0"

600.0 Ft l -61' 0' 0"

800.0 Ft! -61' 0' 0°

1000.0 Ft! -59' 0' 0"

Remarks :CASING PULLED OUT, B.G., SIZE

LABORATOIRE D'ANALYSE BOURLAMAGUE LTEE SAMPLES # 2060 TO 2069 INCL.

Logged by : ROBERT OSWALD

Page 62: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION

Hole 4 : 87-5 PAGE: 2

1 1 1 FROM 1 TO I DESCRIPTION :Sample! FROM : TO I L I Pt I Pd 1 Ni% 1

: (Ft) I (Ft) I . . ' . : (Ft)10z/t 10z/t I ' , I : : 1 : ; : ; 1 1 1 ; 1 1 0.01 3.01 CASING :

I .

. I 3.01 581.01 Massive Actium grained, dirk olive green to yellowish green altered dunite.

1 Much magnetite between and around olivine crystals. Scattered sulphides.

1 19.2- 20.1

1 Highly altered.

38.6- 40.0 Altered serpentinized fractures 1.351/C.A.) with magnetite veinlet

and asbestos threads.

49.2- 58.0 Altered serpentinized fractures (30 and 751/C.A.) with asbestos threads.

66.0- 105.0 Altered serpentinized fractures (0-85/C.A.) with asbestos threads

or/and magnetite veinlet.

1 1 1 105.0- 159.0 Altered serpentinized fractures (15 and 501/C.A.) with asbestos threads.

1 174.0- 188.0 Highly altered, serpentinized fractures (201/C.A.).

1 193.0- 199.0 Altered, serpentinized fractures (10 and 301/C.A.).

220.0- 224.0 Altered serpentinized fractures (301/C.A.) with asbestos threads

and magnetite veinlet.

Page 63: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 I I I I I I I I i I i I I I I i I I

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION Hole 4 : 87-5 PAGE: 3

1 FROM : TO

(Ft) : (Ft) : DESCRIPTION

:Sample: FROM : TO 1 L Pt 1 Pd 1 NiX 1

(Ft)10z/t 1Qzlt :

1 ! , i i , 1 1 , , 1 i

242.0- 291.0

Highly altered serpentinized fractures (0' and 30'/C.A.) with

asbestos threads and/or magnetite veinlets.

332.0- 337.0

Altered serpentinized fractures (30' and 45'/C.A.)

371.0- 375.0

Highly altered, serpentinized fractures (10' and 85'/C.A.) with

asbestos threads.

i 427.6- 432.0

Highly altered serpentinized fractures (30'/C.A.) with asbestos

threads.

480.0- 511.0

Numerous serpentinized fractures (40' and 60'/C.A.) with asbestos threads.

: 1

1 535.0- 550.0

Altered, serpentinized fractures (0', 15' and 30'/C.A.) with magnetite:

veinlet or/and asbestos threads.

557.6- 581.0

Highly altered, serpentinized fractures (25' and 50'/C.A.) with

asbestos threads.

1 581.01 827.01 Massive, fine grained, green dark altered peridotite. Magnetic. Scattered 1 sulphides.

581.0- 696.0 Altered, carbonatized, serpentinized fractures (20', 40' and 75'/C.A.):

with asbestos threads.

Page 64: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I 1 I 1 I I I I I I I I

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION Hole il : 87-5 PAGE: 4

1 FROM 1 TO 1 DESCRIPTION ;Sample; FROM 1 TO 1 L 1 Pt 1 Pd 1 Ni% 1 1 (Ft) 1 (Ft) 1

1 1 1 1

(Ft)10z/t 10z/t

, 1 i

708.0- 735.0 1 ; Altered, carbonatized, serpentinized fractures (30 and 60/C.A.) 1 1

with asbestos threads.

735.0- 741.0 Disseminated sulphides. 1

1

1

Disseminated sulphide. 1 20601 735.01 738.01 3.01 N.D.1 N.D.1 0.1891

Disseminated sulphide. 1 20611 738.01 741.01 3.01 N.D.1 N.D.; 0.1651

i

741.0- 787.0 1

Altered, carbonatized, serpentinized fractures (45 and 60°/C.A.)

with asbestos threads.

787.0- 797.7 Disseminated sulphide, carbonatized and serpentinized fractures

(10 and 60/C.A.). 1

797.7- 827.0 ; Carbonatized and serpentinized fractures (30 and 60/C.A.). 1 1

1 827.01 989.21 Massive, fine grained, hard black altered peridotite, magnetic, disseminated 1 sulphide.

827.0- 849.2 More disseminated sulphide, carbonatized fractures (20-70/C.A.)

More disseminated sulphide 51X. 1 20621 834.01 835.01 1.01 N.D.1 4.D.; 0.2651

1 1 1 ; 1 1 1

More disseminated sulphide !1X. 1 20631 844.51 845.51 1.01 N.D.1 N.D.1 0.1771 . , 1 , , i , ,

:

Page 65: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION Hole : 87-5 PAGE: 5

1

1 FROM 1 TO 1 DESCRIPTION :Sample: FROM 1 TO 1 L 1 Pt 1 Pd 1 Ni% 1 : (Ft) : (Ft) :

(Ft)10z/t 10z/t 1

1 1 1 1 854.0- 859.5

White carbonate-talc. ;

872.0- 876.0 Ditto.

876.0- 989.2 Altered peridotite in disseminated talc with numerous fracture (30 and 6(0/C.A.).

Disseminated and small veinlet sulphide.

Disseminated and all velniet sulphide.

Disseminated sulphide.

1 989.21 1002.31 Light grey andesite non-magnetic, disseminated sulphides.

Disseminated sulphide.

Disseminated sulphide.

Disseminated sulphide. 1 1002.01 1End of hole

1

!

1

1

;

t

11.

2064:

20651 1

20661

;

20671

2068;

20691

1 .

974.61

. 975.81

1

9E17.31

989.21

991.2;

;

993.21

975.81 1.21

977.01 1.21

. a

, .

4E18.31 1.01

991.21 2.01 ",

993.2; 2.0;

; , .

995.21 2.01 , ,

N.D.1 N.D. 0.124:

N.D. N.D. 0.1751

. , .

. . ,

N.D.1 0.0031 0.0951 „ I

--' ; 1

--1 0.0061

1 .

. , .

--1 --1 0.0071

; ;

--1 --; 0.0081

Total amount of sample = 10 Total length sampled = 17.4Ft

Page 66: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Hole # : 87-6

Township: TR:ECESSUN

Lot : IA Range: 4' Claim # :281812-:

Latitude: 3400.00 N

Departure: 200.00 E

Elevation: 0.00

Date started :NOVEMBER 1987

Date compieted:NOVEMBER 1987

Azimuth: 180° ;r,

Dip . -60' 0"

Lenott : 100u0.0 Lt

Level . Section: + 00E

Collar coordonate : Line : 2+00 E Station: 34+00 N

i i I I i i I I I I I I I I I I I I I

DUMONT NICKEL CORPORATION LTD

DIAMOND DRILL LO6

Property : LAUNAY-TRECESSON

Deviation tests Depth i Dip i Azimuth

200.0 Ft; -63" 0'

400.0 ft. -64ü v' 0" 600.0 Ft: -63v 0' ,

800.0 Ft i -62a l'' li"

995.0 Ft1 -59` 0' ta' ; 199' 0"

Remarks :CASINB DEVIATED. Br SIZE

LABORATOIRE D'ANALYSE BOURLAMAOUE LiEE

SAMPLES # 2103 TO 2104 INCL. 2089 TO 2096 INCL.

Loqued by : ROBERT OSWALD

Page 67: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I ) I ! ) ! I 1 I I I I I I I I I I 1

LAL+NAY-TF;ECESSC+N DU-ONT NICKEL CORPORATION LTD Hole #: 67-6 PAGE:

FROM . TO '

(Ft) ; (Ft)

{

?ESCkirTICiN ;Sample; FROM f i0 , L f Pt . Pd 1 Ni 'r'. . Au ;

iFt};oz/t ;oz/t sE7z/t .

0.01 55.01 CASING ; .

55.0! 478.4 Massive, coarse to medium grained, dark alive green, altered dunite. Much

magnetite between ana around olivine crystals. Scattered sulfides.

55.7- 57.0

Fracture, (00 and 770'/C.A.), filled with carbonate.

105.0- 108.7

Altered, serpentinized fractures (200 and 4U /C.A.) with magnetite

veinlets.

142.0- 156.6

Few serpentinized fractures (40-500/C.A.) with asbestos threads.

166.8- 170.0

Altered, serpentinized fractures (100-200/C.A.), with asbestos

threads and magnetite veinlets.

;

200.3- 201.4

Altered, serpentinized fractures (25' and 600/C.A.) with asbestos

threads and magnetite veinlets.

230.0- 280.0

Few serpentinized fractures (10-30/C.A.) /C.A.) with asbestos threads and !

magnetite veinlets.

315.0- 340.5

Altered, carbonatized and serpentinized fractures (100, 200, :i50

and 500/C. A.) with asbestos threads and magnetite veinlets.

357.8- 362.5

Altered, carbonatized and serpentinized fractures t10-20 and 600/A.C.);

with asbestos threads and magnetite veinlets.

Page 68: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 I ) ) ) I ) ) I ) I ) ) ) ) ) 1 ) )

LAL;NAV-TRECESSON D?fMONT NICKEL CORPORATION LTD

Hole 4 . 8/-6 FAIL:

i • 1

FROM ; TO .

(Ft) ; (Ft)

DESCRIPTION ;Sample; FROM ; TO ; L ; Ft ; Fa ; Ni ,. ; Au ;

:l't;;oz(t ;oz/t ; :Oz/t v i

365.0- 376.0

Few serpentinized fractures (20u and 6U !C.?.?.

378.5- 383.0

Serpentinizea fractures (04 and 30-404iA.C.) and tilted in soaes

with asbestos threads.

422.0- 432.6

Carbonatized ans serpentinized fractures (10-50/C.A.) with magnetite

veinlets.

434.0- 435.0

Highly serpentinized fractures ±55.1 /C.A.r.

446.3- 451.0

Altered and highly sereentin.zea fractures 1 20-504/C.A.).

478.4; 453.8; Massive, medium to fine grained, yellowish green ta black peridotite. More altered, Magnetic. disseminated fine grained sulfides.

513.5- 551.3

Altered, highly serpentinized fracture 110, 30, 60 and 854/C.A.i

with asbestos threads and / or magnetite veiniets.

568.5- 584.7

Weakly carbonatized. serpentinized fractures t30 and 604/C.A.)

with magnetite veinlet and erythrite?

584.7- 625.0

Disseminated, carbonatized and serpentinized fractures

150 and 854/C.A.).

Page 69: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION LTD

Hole # : 87-6 FAA: 4

FROM ' TO

DESCRIPTION

ISatple FROM IU I L Pt ; Pd I Ni

(Ft) (Ft)

(Ftflozit out

625.0- 626.5 Carbonatized. serpentinized and fragmented peridotite.

626.5- 685.5 Ditto 1584.7-625).

685.5- 694.0 Altered, serpentinized fractures (50-804/C.A.) with ervthrite?

694.0- 811.0 Ditto (584.7-625).

811.0- 815.9 Carbonatized, serOentinzed strinoers an fractures (30 and 704/C.A.1.;

815.9- 858.0 Ditto (5E14.7-625).

;

Contacts perinotitein ke. Small sulfide Yeinlets .21%. ; 2103; 857.1); Stid.ti 1.0; N.Q. 0.00I;

858.0- 861.3 2104; b58.1„); 861.6;

Light Ivey coarse grained porphyritic granonlorite dyke.

861.3- 866.0 Liantly silicified peridotite with few carbonatizecl fractures and

magnetite einlets.

866.0- 892.0 Numerous carbonatized fractures 10-601L.A.), sometimes with

magnetite. Lightly talcose.

892.0- 953.8

--I FR;

Page 70: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAJNA•v-TnECEüStIN DiiMONT NICK:EL CORPORATION LTD Hole 4 . 87-6 Pf1DE: 5

DESCRIPTION FROM ; TO ;

(Ft) ; (Ft) , 15amoie; FROM , TO , L 1 Pt , Pd , NI .. F 4u

; (I-tS Czit ;nzit ;Out

Caroonatized, seraentinl_ed fractures (0-85'/A.C.) with magnetite

veinlet. More disseminated sulfides.

Disseminated sulfides. 2089; 923.5; 928.4; 4.9; N.D.; N.D.; 0.165;

Disseminated sulfides.

Disseminated sulfides.

2090;

2091;

926.4;

935.0;

937.0;

937.9:

4.0;

4.9;

N.D.,

N.D.,

,

N.D.; 0,150;

N.D., 0.185:

Disseminated sulfides. 2(z92; 937.9; 942.5; 4.6. N.D.: N.D.; ?i.182;

Disseminated sulfides. 1093; 942.5; 947.3. 4.8; N.D.; N.D.: 0.207;

Disseminated sulfides. 2094; 947.3; 952.0; 4.1; M.D.1 N.D.: 0.260;

Disseminated sulfides and sulfides veiniets. t095: 952. (1; (66.b; 1. 6; N. D. ; N.D., 0.1301

953.8; 1000.0; Light grey andesite, non-eagnetic. Scattered sulfides. Silicified, carhonatlzed and chioritized fractures.

Disseminated sulfides and sulfides veiniets. 2096; 953.8; 955.3; 5 N.,t.4 1.5;M.D. N.U.!li.il.: 1000.0) ;End of hole

Total amount of sample = 10

Total length sampled = 56.1Ft

Page 71: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 I 1 1 ! 1 ! I 1 I I I I I I I I I I

0

DUMONT NICKEL CORP. DIAMOND DRILL LO6

Property : LAUNAY-TRECESSON

Date started :OCTOBER 1987

Date completed:NOVEMBER 1987

Latitude: 3300.00 N Azimuth: 180' 0'

Departure: 400.00 E Dip : -60' 0'

Elevation: 0.00 Length : 877.0 Ft

Hole 4 : 87-7

Township: TRECESSON

Lot : IA

Range: V Claim 4 :281812-1

Level Section:

Collar coordonate : Line : 4+00 E

Station: 33+00 N

Deviation tests Depth Dip Azimuth

200.0 Ft1 -63' 0' 0°

400.0 Ft1 -63' 0' 0"

600.0 Ft: -63' 0' 0"

872.0 Fti -58' 0' 0" i 187' 0' 0"

Remarks :CASING PULLET OUT, BB SIZE

LABORATOIRE D'ANALYSE BOURLAMAQUE LTEE SAMPLES 4 2070 TO 2088 INCL.

Logged by : ROBERT OSWALD

Page 72: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DESCRIPTION

1 1

1 FROM 1 TO 1

1 (Ft) 1 (Ftl 1 i i , 1

1Saeple? FROM 1 TO 1 L 1 Pt 1 Pd 1 Ni Z 1

1 , 1 (FtllOz/t ?Oz/t 1 1 1 1 1 , 1 1 ,_

I I I I I I I I I I I I I I I I I I

LAUNAY-TRECESSON DUMONT NICKEL CORP. Hole # : 87-7 PAGE: 2

,

1 0.01 30.01 CASINO 1

1 30.01 199.81 Massive, sedius and coarse grained, dark olive green, altered dunite. Much ? ? 1 magnetite between and around olivine crystals. Scattered sulfides.

1 50.7- 66.0 1 Serpentinized fractures (25-30'/C.A.) with magnetite veinlets.

Asbestos threads.

( 1 85.4- 86,5 ? 1 Serpentinized fractures (154-20/C.A.I

134.6- 136.5 Highly serpentinized fractures (15'/C.A.I with magnetite veinlet

and asbestos threads.

(

1 1 144.0- 145.0 Ditto.

156.0- 163.0 1

Altered serpentinized fractures (10'/C.A.I with magnetite and asbestos?

threads.

194.6- 197.8 Carbonatized fractures (30'/C.A.I filled with asbestos threads.

197.8- 199.8 Altered, serpentinized fractures.

;

1 199.81 352.01 Sole as 30 to 199,8, but sore serpentinized and sedius fine grained. 1

1 1 210.0- 210.5 ? 1 Magnetite veinlet (25'/C.A.) with carbonate and serpentine.

1

(

(

Page 73: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

! I I I I 1 I 1 1 I I I I I 1

LAUNAY-TRECESSON DUMONT NICKEL CORP. Hole 11 : 87-7 PAGE: 3

: FROM : TO :

(Ft) 1 (Ft) : 1

1 1 ,

DESCRIPTION :Sample: FROM : TO 1 L 1 Pt 1 Pd I Ni X 1

: 1 1 (Ft)IOz/t :Oz/t 1

I 1 1 : 1 I 1 1 1 I

1 231.4- 231.8

I Carbonatized, serpentinized fractures (40'/C.A.) with magnetite : veinlet.

236.0- 245.3

Carbonatized, serpentinized fractures (0, 30' and 60'/C.A.).

262.0- 302.0

More disseminated sulfides.

I 302.0- 312.0 , : Highly altered, carbonatized and serpentinized fractures (15 and 304/ 1 I C.A.? with magnetite veinlets and asbestos threads. 1

1 1 I I I 312.0- 352.0 1 1 : 1 1 Few serpentinized fractures 140-50/C.A.) with carbonate and magnetite: 1

veinlets. I 1 I

: 1 352.01 713.01 PERIDOTITE I : : : : : 1 : I Massive, medium fine grained, grey yellowish altered, peridotite (approximate 1 1 1

: contacts). Magnetic, disseminated fine grained sulfides. : :

352.0- 372.0

Carbonatized and serpentinized fractures (15 and 604/C.A.) with

asbestos threads, magnetite veinlet and erythrite (?)

375.5- 403.5

I : 1 1 More altered and numerous fractures (carbonated and serpentinized).

i I 403.5- 405.0 Serpentinized stringer zone.

~ 1 :

Page 74: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I 1 I 1 I 1 1 I 1 I 1 1 1 I i I I 1 I

LAUNAY-TRECESSON DUMONT NICKEL CORP. Hole (R : 87-7 PAGE: 4

1 FROM 1 TO 1 DESCRIPTION :Sample! ~ Ni~ ~ ,baeple, FROM , TO , L, Pt , Pd , Ni ti, 1(Ft) :(Ft) 1 1 1 1 1(Ft)10z/t 10zlt : , ' ' ' 1 1 1 1 1 1 405.0- 432.0 1 t : Ditto (375.5 to 403.5). 1

432.0- 559.5 Carbonatized, serpentinized fractures (20-60'/C.A.) with asbestos threads.

559.5- 561.7 Serpentinized fractures (60'/C.A.). 561.1-6' Highly altered.

559.5- 598.0 Ditto (432 to 559.5).

598.0- 599.4 Highly serpentinized fractures (40'/C.A.) and carbonatized.

599.4- 627.3 1 1 Numerous carbonatized and serpentinized fractures (40/C.A.)

1 627.3- 637.0 Altered, carbonatized and serpentinized fractures (15 and 60'/C.A.).

637.0- 680.0 Numerous carbonitazed and serpentinized fractures (0', 40' and 60'/

C.A.). Sometimes with magnetite veinlet.

1 1 680.0- 681.0 1 1 Highly serpentinized fractures (10/C.A.).

681.0- 713.0 1 1 1 Numerous carbonatized and serpentinized fractures 10, 20.40,70' and 1 90'IC.A.)

1 ,

1

1 1 1 1 1 1 1

1 ; 1 ; 1 1 1 1 : : I 1

Page 75: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORP. Hole # : 97-7 PAGE: 5

1 1 FROM 1 TO 1 DESCRIPTION :Sample! FROM : TO 1 L 1 Pt 1 Pd 1 Ni % 1 1 (Ft) 1 (Ft) 1 1 : 1 (Ft1102/t 10z/t 1 1 1 : 1 ! 1111 ! ! f 1 713.01 854.81 Massif, fine grained, black peridotite, magnetic disseminated fine grained 1 . . 1 . . . . . . . .. . . . . 1 1 sulfides. Lightly serpentinized and carbonatized fractures. 1 , . . . . a . . . . , . . , , . a a . 713.0- 722.8 . ;

' , Hard peridotite.

722.8- 729.9 Light grey coarse-grained, porphvritic granodiorite dyke. Massif 301/C.A. Contacts.

: , ., , ,

729.9- 736.0 Hard peridotite.

736.0- 805.8 Numerous fractures filled with carbonate and serpentine.

Disseminated sulfide i1/2%.

805.8- 854.8 Ditto and disseminated sulfide. Sometimes with small sulfides veinlets.

Disseminated sulfides.

Disseminated sulfides.

Disseminated sulfides.

Disseminated sulfides.

Disseminated sulfides.

1

1

1 1

1

!

1

!

.

1

.a

20981

2070; 1

20711

a 20721

1

,

20741

,.

796.01

1 905.81

: 810.41

,

815.01 1 I

t .

824.41

20 73 1

779.51

; 810.41

1 815.01

1

819.6; 1

824.4;

827.11

8 19.61

3.51

4.61

1 4.61

1

4.61

4.8; t

4./1

N.D.1 0.0041 0.4301

14.0.1 14.0.1 0.1821

1 1 1

N.D.1 N.D. 0.170:

14.0.1 14.0.1 0.1501

1 1 1

N.D.1 14.0.1 0.1431 .

14.0.1 N.D.; 0.1801

Page 76: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-TRECESSON DUMONT NICKEL CORP.

FROM TO DESCRIPTION

(Ft! (Et)

Disseminated sulfides.

Disseminated sulfides.

Disseminated sulfides.

Disseminated sulfides plus small sulfides veinlet.

Disseminated sulfides plus small sulfides veinlet.

Disseminated sulfides plus small sulfides veinlet.

Disseminated sulfides plus small sulfides veinlet.

Disseminated sulfides plus small sulfides veinlet 11X.

Disseminated sulfides plus small sulfides veinlet 2-3X.

Disseminated sulfides plus small sulfides veinlet 2-3%.

Disseminated sulfides plus small sulfides veinlet 5X.

Disseminated sulfides plus small sulfides veinlet 57..

854.8 877.0 Grey dark andesite (?) Non-magnetic, disseminated sulfides, chloritized,

carlionatized and silicified filled fractures.

Disseminated sulfides.

877.0 End of hole

Hale # : 87-7

:Sample: FROM I

1

2075; 829.11 .

2076; 833.61

1 1

20771 835.61

, 1

2078; 837.61

. 1

2074; 839.61

; I

20801 841.61 ..

, .

20811 843.61

I t

2082: 845.6: ..

. .

2083: 847.81 I

20841 850.11 ..

. .

20851 852.31 .

1 .

20861 853.71

. .

. .

20871 854.81

o . I

PAGE: 6

TO I L I Pt 1 Pd !

I attlOztt 10z/t

-1 :

833.61 4.51 N.D.1 N.D.

. . .

. .

835.61 2.01 N.D. 0.015!

1 1 1 .

837.6; 2.01 0.0041 0.0201

I ,

I 1

839.6: 2.01 0.016! 0.039:

. . :

841.6; . .

2.01 0.0131 0.0351

I , .

, . .

843.61 2.01 0.0061 0.0231

. .

1 , .

845.61 2.01 0.0061 0.020:

I ! . , .

847.6: 2.0! 0.003: 0.0661 .

. 1 ; ,

850.11 2.3: N.D. 0.0151

. .

852.31 2.2; N.D. 0.016; . ,

853.7: 1.41 0.0091 0.0341

. .

. . . . .

854.81 1.11 0.009! 0.019!

856.81 2.01 N.D.: 0.003;

Ni X :

0.1441 :

0.390! , ,

0.4301 .

0.820: , .

0.7901

0.5001 , .

0.4951 . ,

0.650: , ,

0.5001 .

0.480;

1.0701

. .

0.8801

0.1001

Page 77: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

J I J I I I J I 1 I I I I 1

LAUNAY-TRECESSON UMONT NICKEL CORP. Hole # : 87-7 PAGE: 7

: 1 1 FROM 1 TO 1 DESCRIPTION :Sample: FROM I TO : L 1 Pt 1 Pd 1 Ni % 1 : (Ft) 1 (Ft)1 : ,

, , ,

, 1 (Ft):0z/t 10z/t : 1 1 1 1 : 1 1 { : : : 1 1

Total amount of sample = 19 I f : 1 Total length sampled = 54.3Ft

Page 78: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I I I I i 1 I I I 1 I I

DUMONT NICKEL CORPORATION LTD

DIAMOND DRILL LOB

Property : LAUNAY-TRECESSON

Hole t . 87-8

Date started :NOVEMBER 1987 Township: TRECESSON

Date compieted:NOVEMBER 1987 Lot . 1A

Range: V Claim :281812-1

Level Section: 2 + 00E

Collar coordonate . Line . 2+00 E

Latitude: 3310.00 N Azimuth: 180' V'

Station: 33+10 N

Departure: 200.00 E Diu : -68e 0

Elevation: 0.00 Length : 950.0 Ft

Deviation tests Depth ; Dip Azimuth

200.0 Ft; -64' Ù' 0"

400.:3 Ft; -63Ô 01 0' 600.0 ht; -85' Dr 0' 800. 0 Ft; -64' 01 t}"

750.0 Ft; '64ù Lt' vjn

Remarks :CASING PULLED OUT, BO SIZE

LABORATOIRE :l'ANALYSE BrOURLAMADUE LTD

SAMPLES t 2097 TO 2102 INCL. AND 2109.

DL-87-8 BOX 33, (644'-6631 ) MIXTED

Lopped tu : ROBERT OSNALii

Page 79: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAtiNAY-TRECESSON DJNONT NICKEL COKPOTtATiON LTV Hole : B/-B F'A6E: :.

FROM ; TO .

(Ft) . (Ft) ;

~ 1 ~

0.0 43.01 CASINO

( 43.0: 402.31 Massive, coarse grained, dark olive green, altered dunite. Much magnetite

; between and around olivine crystals. Scattered sulfides.

56.0- 60.0 Altered, serpentinized fractures (40-50/C.A.? with asbestos threads.

78.4- 80.9

Ditto.

138.5- 151.0

Altered, serpentinized fractures (30, C.A.) with magne te veiniets

and asbestos.

158.0- 193.5

Carbonatized, serpentinized fractures (20-30/C.A.) with magnetite

veinlets and asbestos threads.

212.0- 216.0

serpentinized fractures (30/C.A.? filled with asbestos threads.

216.0- 267.0

serpentinized fractures t30-50/C.A.I with magnetite and asbestos

threads.

267.0- 272.5

Altered and serpentinized fracture (10¢/C.A.; with magnetite and

asbestos threads.

303.0- 308.0

Altered and serpentinized fractures (0-30/A.C.t with magnetite and

asbestos threads.

:Sample; FROM : TO : L,Pt ; Pd , Nil ;

~

1 . (Ft);Oz/t ;Oz/t

: 1 ; . , ;

DESCT!IFTION

1

Page 80: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION LTD Hole * : 87-8 PAGE: 3

FROM i TO

(Ft) (Ft)

DESCRIPTION ;Sample; FROM ; ;L s Pt ; Pd ; NO.

(Ftl;l=z/t 10z/t j i f t "1

331.0- 336.0

Serpentinized fracture (104 and 60 C.A.) with magnetite and asbestos

threads.

349.0- 381.0

Seruentinized fractures (30-70°/C.A.) with magnetite and / or asbestos;

threads.

381.0- 383.0

Serpentinized breccia filled with asbestos.

383.0- 399.0

Serpentinized fractures (10-604/C.A.i with magnetite and asbestos

threads.

399.0- 402.0

Asbestos and serpentinized breccia filled with asbestos.

( 402.31 753.7 Grading into medium-grained serpentinized peridotite, massive much disseminated(

fine grained sulfide. Magnetic. Dark olive green to dark grev-green.

402.3- 496.0

Few serpentinized fractures (10-60/C.A.) with magnetite veiniet and i

or asbestos threads.

496.0- 580.0

Serpentinized fractures (10-70°/C.A.) with in some ervthrite?

580.0- 583.0

Altered and serpentinized breccia.

584.5- 586.0

Page 81: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LA11NAv-iRECESSUN DUMMONT NICKEL CORPORATION LTD

Hole 4 : 87-8 PAGE: 4

FROM ; TU ;

(Ft) , 1Fti ! DESCRIPTION

!Sample: Fh;UM T U ; L; Pt . Pd ; Nil ,

, I i . (Ft)L

10:!t ili'L1 L i I i . J i 1 I I , i 1 v 1 1 1

Altered and fractured ;10-90°/f,.A..l

590.0- 591.4

Highly fractured and altered fractures filled with asnestos.

591.4- 644.0 Carbonatized and serpentinizen fractures t10-70ç/C.A.i filled with

asbestos.

644.0- 749.8

Carnonatized and serpentinized fractures f0-704/C.A.i with in some

magnetite velnlet.

749.8- 753.7

Light grey coarse grained porphyritic granodiorite dyke.

Non-magnetic chioritized.

Contact 306/C.A.

753.7; 865.9; Same as above but getting black greenish and more disseminated sulfides. Serpentinized and numerous fractures (0-50/C.A.) filled with carbonate, talc, magnetite or serpentine.

1

i ; ; More disseminated suffices i,LX. 'Lhalcnpvrite trace). . 2109: 817.0! 818.+» 1.0; N.D.; 0.006; 0.6001

1

Disseminated sulfide. 1 09 ..L~i1, 847 .3; 85 , 2.3' 5 ;N.D.;N.D.0.1481 ,,,t.l N...

Disseminated sulfide. ;0ù8; 852.3; 857.0; 4.7; N.D.; N.D. 0.161; ;

Disseminated sulfide. 2099; 857.0; 861.0; 4.0; N.D.! N.D. 0.200;

Disseminated sulfide, 1-2X. ; 21100; 862.0; 1.01 N.D., 0.014; 0.4501

Page 82: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

i I i I I I I I I I I I I I i I I I I

LAUN€;Ÿ-Th)EC ESSON ÜUMONT NICKEL CORPORATION LTD del : 87-8 P+i6E. 5

; FROM ; TO . DESCRIPTION

+ ift) ; ift) t . +

;Sample; FROM Ir, } L ; Pt ; Pd ; Ni%

= tft);ClZit ;Ozit ;

[ i i t i ; _ 5 1 i i

. ; Disseminated suft:de and small veinlets. 2101; 862.0; 883.0; 1.0; N. U.; N.D.; U.204;

i i 1 i . . + I I 1

Sulfiûes, 2302; B63. U; 865.9; 2.9; N.13.; N.D.! 0.082;

865.91 950.0; Dark grey basalt-andesite, fine grained, non-magnetic. Numerous veinlets

; ï30°-60`-'iC.A.i filled with quartZ, carbonate, enidete. Disseminated sulfides.

886.2- 950.0

Same as above but the colour getting light grey. Numerous veiniets

(up to 3 inches) carbonate and in some pyrite and nvrrtiotite. Inc

sulfides is in trace.

440.9- 941.4

Small breccia filled with quartz contacts 20°iC.A.

950.0; ;End of hole

Total amount of sample =

Total length sampled = 19.6ft

Page 83: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

| | 1 | I | | | 1 | | | | | 1 | | 1 |

DaalwaE CORPORATION DIAMOND DRILL LOG

Property ;waR9Eaea

6!e # : 87-9 TmseG awb§a Lot : G Range: V G2■ #:2a25

Setae 2002,§ Departure: :&00E d e#!æ: 0,00

2& started : meRw@ Gte o#4t@:r dÆkaw

RlyA: ee « A „ -w° C

weR: 824.0 Ft

Level Section: ;!§3

aûJEer62w ; Line : 3+00 E Station: 2waN

Deviation tests Depth 2R ; 4im J§

200.0 R: %2 E 490.0 Ft; aJ « 600.0 Ft: ae « 815.0 R! -y° «

Re æ

were :wah 6&b OUT, 80 GPO wB6@64 2k@ÿ± DURLAMAQUE L1EE SAMPLES #2110 G 213IRu & wd mf 24. I,471-490l N3(

Loaned Q:6E9 0S6Q

Page 84: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I 1 I 1 1 I 1 I I I I I I 1 1 I I I

L`illt'dfll tHE/ESSIA :;Oi11!NI NiUEL ;.tiheL'rf4i!1L'+tf Fiole # ° ti7-9 FAA.:

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

Fn'i_tM ; 10 i DESCRIPTION 15amp:e:: FROM , fÜ ; i. , Ft Fd

i lFtt i (Ft) ' , , (Ft)i(3i.'t i(1:lt ~

1^ , . _' _ . , ' . ;__.._-_i . ~_i ~ t ,

1 0.01 39.01 CASINB

1 39.01 142.01 Massive, coarse to medium grained, dark olive green, altered dunite. Much 1

. Magnetite between and around olivine crystals. Scattered sulfides.

39.0- 48.0

More altered, seroentinited and carhonatizei; fractures (50-7Ù`~!±_.N.)

with in some magnetite veinlets.

48.0- 87.5

Fractured dunite :49-70"r'i:.h.).

87.5- 91.5

More altered seroentinized fractured t+;-iü'' and 81"!'„.t?.t with

asbestos or magnetite.

91.5- 121.2

Fractured dunite

121.2- 126.5

More altered weil serpentinized fractures ,t:''?-4S'iC. t.1 with asbestos

and magnetite.

139.2- 142.0

Ditto t1.5`ÎI•.H.1.

1 142.01 490.01 Same as but more altered (serpentinized).

142.0- 206.0

Fractured gunite U5-VO' If.!... with asbestos and magnetite.

206.0- 274.0

Altered, serpentinized fractures t25-8(P/L. filled with asbestos

magnetite and carbonate.

, "ii .. i Ru

1O:,'t .

i i 4

Page 85: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

L.:MAY-IRE-LESSON OUM0Nf NIE LUNI-'0R4IION Hole # 8J- FAUE:

FROM TO

IFt) IFt

DESCRIPTION

;Sample. FROM U L . Pt : PO 1 Ni I Au

qt):Ozit Ut !]zit

274.0- 297.0 nitered, serrientinized and carbonatized fractures i30-60/C.A.1

filled asbestos erythrite and aunaberalte?

297.0- 339.0 More fractured (Q-40'iC,A.) dunite, fractures filled with serpentine, ;

asbestos maonetite and ervtOrite?

339.0- 397.5 Serpentinized fractures 10-40/L..i with carbonate, madnetite.

Drucite and asbestos.

1

397.5- 397.8 Mua seam,

397.8- 437.0 More fractured (10°-6ViC,

Wed with serpentine, carbonate,

magnetite and asbestos.

437.0- 490.0 Numerous small fracture (50-LIT-A.A.? titled with asbestos carbonate,

magnetite and serpentine.

i 490.01 671.51 Massive, medium to fine grained, grey-greenisb peridotite. Altered magnetic,

more disseminated fine drained sulfides.

490.0- 554.2 Numerous serdentinized fractures f ileo wi th asbestos

carbonate and magnetite.

554.2- 558.7 Light grev coarse grainea porohyritic granodiorite chRe. Massive

contacts. Lightiv chloritized, .few biotite.

Page 86: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LOW-IRECESSON DuMONI NICKEL CORPURAIION Hole : 87-Y FRIA: 4

- FROM : TO

(Ft) ; (Ft) :

DESCRIPTION

Sample; FRIA lULPt ; Pd NI Mu

11q);13,11t ;Ult. 10zit ;

; •

558.7- 603.0

Serpentinized and carbonatized fractures (10-60/C.A.1

603.0- 662.0 Seroentinized ana carbonatized fractures UU-/U'iC.A.) filled with

magnetite and in same asbestos, numerous stringers of talc. ;

More disseminated sulfides i1i41.1 and magnetite stringers. 2110; 637.0; 639.0; 2.0; Nb.i 0.006 Q.400;

638.6- 641.1

Stringers of talc

More disseminated sulfides (1/4:41 and magnetite stringers. 2111; b3'1.Q; b41.0; 2.0; 0.151!

More disseminated sulfides and magnetite stringers. 2112i 641.01 642.0; 1.0; N.D. 0.0U2; 0.65;

1 671.51 723.61 Breen to blue-grey basalte andesite, fine grained, non-magnetic, disseminated 1 ! pvrrnotite (trace! In small veinlets near by contact. Lhlorltized, numerous ;

; quartz-carbonate einlets 140-60G/Ca4.).

Utiartz-chlorite-earoonate vein. ; 2113; Y13.9; /14.Y; 1.0; - - TR:

714.2- 714.6

Uuartz-eniorite-carbonate vein 50/.A.

723.61 824.01 Same as above but become green-grey, chloritized, numerous small veinlets

110-?0 C.A.i. Uuartz and carbonate, non-magnetic; pyrrhotite patch in trac-

turc.

746.2- 746.9

Porphyrine diorite dyke, contact 40u-501C.A.

791.1- 795.1

Porohyritic diorite dyke. contact 40-50,iC.A. Iwo porphyrinc

diorite dykes, grey-light. 357. Feldspar porphyry, non-magnetic,

Page 87: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

)

LAUNM-IRECESSON DOW NEKEL CORP RAMA Role 87-'1 PR6E:

; FROM TO :

IFtl !

DESCRIPTION

;Sample; FROM Id L ; Pt ; Po Ni XAu

;..Ffi;Ozit :Ozit ; :0,71t

numernus quartz-caroonate-chlorite yeinlets

i 824.0; :End of hole

Iota' amount of samples= 4

iota: leroith sampied = 6.0Ft

Page 88: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORATION DIAMOND DRILL LOG

Property : LAUNAY-IRECESSON

Hole t : 82-10

township: TRECESBON

tat IA Range: V Llaim :281812-1

Date started :NOVEMBER 1982

Data completed:NOVEMEER 1982

pvel Section: 4 4- 00E

Co lar coardonate : Line : 4+00 E

Latitude: 6204.1.1.111 N wilmata: laus

Station: 32+00 N

iieoirture; 400. E no

Elevation: Lenata 132.0 ht

Deviation tests Depth Dip Azimutn

200.0 Ft; -63' 0'

400.0 Ft: -63' 0'

600.0 Ft; -63 0'

732.0 Pt; -60' O' ; 182' u'

Remarks :CASING PULLED Obi, BO SIZE LABORATOIRE D'ANALYSE BOURLAMAtla LID SANPLES 14 2114 TO 2115 INCL.

Loquea b UEÎ OSWALD

Page 89: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I i I I I I I I I I I I

!_fiilNN, ?HË;.tStiOfV Dîiyn4P,f Ni'v,;ii l.ilRPi!^!:l:Lfi Hole . - -.1 F- ?.,

FROM ; TO i (Ft) . (Ft) ,

ÜLSCR11'i!;.i?`k ,S3tkniët .,:t'3. + Ît'• , L Pt Pd ftil i

iËtliLt2,''t

_. -

1 0.01 21.01 LASING

1

1 21.01 243.01 Massive, coarse to medium grained, dark olive green, altered dunite. Much

i magnetite between and around olivine crystals, bcattered sulfides.

26.5- 33.0 1

Highly altered dunite With magnetite stri?tlers and asbestos threads. i

51.0- 52.0 i Ser?ér±tinizt+d fractures ,i:'.''!'.,,i:. i with magnetite.

71.0- 12.0

werùentinired fractures '_'U'r',.ii.i with magnetite, brucite and

asbestos threads.

1 122.0- 124.0

Hitèred serrentiiiièd rart.te .i_ � i4. with Pd ilEti}e 5trirgers.

150.0- 160.0

Iyiltto.

170.0- 175.0

Hitered serpentini2ee fractures 1.10-20 A) with magnetite stringers:

and asbestos threads.

183.0- 243.0

Much altered and sernentini::e'u- fractures ? 1is-.'ii^-.ri.ié.i with asbestos .

threads and magnetite stringers.

1 243.01 721.51 Massive, medium fine grained, grey-yellowish, altered peridotite (approximate 1

contacts). Magnetic disseminated fine grained sulfides.

243.0- 434.0

Numerous =•ar^ÔPtini«ad small fracture's (l0-/0 l't.ii,} with asbestos

threads, carbonate and magnetite.

Page 90: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I 1 I I I 1 I I I I I 1 I I I I

L rUNHY-TRE; Euvl?r~t DU ONT NICKEL CORPORATION

Hole 4 , 87-i0 Nr;ÙE:

FROM ; TO . DESCRIPTION (Ft) (Ft: ,

15alâüie; FROM , TO L r't ; Pd :Ni i , ;tt; iL(zit il?z!t if

;---

434,0- 434.5 Highly altered dLslte.

434.5- 593.2 Ditto. (143-434..,)

593.2- 597.0 ;

Alteration Increase to {iranodlorite dyke, Ine core decome very hard

like 5llicitication.

597.0- 597.5 black dranooiorite ektreaely altered, Mar 'zed and cartooatizeo

matrix,

597.5- 599.5 Ditto to 593.2 -5',,...

599.5- 665.0 Mack oei idotite with numerous small fractures t25',

filled with carbonate, serpentine and magnetite. e29-63; More

visible disseminated sulfides.

665.0- 712.0 Fractures l.i;-i:I'J tailed wit!? carbonate. talc. serpentine an:;

magnetite.

712.0- 721.5 More altered oeridotite. _arbonatized matrix and fractures

t2 -fj, L.H,Î tailed with carbonate talc and serpentine.

721.5; 737.01 Dark grey andesite, fine grained, non-magnetic, chloritized. Few veinlets i20-60/C.A.) fined with cuarta carbonate and chlorite,

! 737.0, ;End of hole

I ::114; 6L-1.i:i 613.01 4,l'1 t;.il.. 0.0;14i 0.410; ..1i5i 636,01 63:.0i 4.01 N.D.; 0.ii021 0.240i

s , i

Page 91: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

| | | | | | | | 1

EAON Q 9»663&

MOM £ERL QvyQ GN

w»* .gea awa

8a: Q (Et) ; (Eti

3&3Æ8a

%a66 ESN; 3 L ;R ;R ~w @Ù;bJ @2t

Total amount Cr samples : GGl length e#!/ = G R1

Page 92: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORAl ION DIAMOND DRILL LOG

Property : LAUNAY-IRECESSON

Note # S7-11 fownship; IRECESSON Lot : lA kange: V Clal :281812-1

Level Section: 5+00 E

Collar coordonate Line : 5+00 E Station: 3.3+00 N

bate started :NliVEM8ER 198/ bate cofflpleten:NOVEMSER 1587

LatituciP1 ,S3UMQ N Aziffiuth; 180 0'

Departure: IANMO E. Dip -60' 0'

Elevation; Length : 84./.0 Ft

beviation tests bepth Dip AziAutti

600.0 Ft; 642.0 Ft:

R.efearks :CAS1NB POLLED WI, BLi SliE LA8URAWIRE D'ANALYSE NOURLAMA0UE LID SAIPLES: # # 2105 IQ 2108 INCL.

# 2116 10 2123 INCL.

Logged by : ROBEid USWALb

Page 93: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

) J )

LAURAY-IRECESSON DUMONI CC'S!, CORPOkOION Hole : 7-11 PmUE: 2

--------------- FROM ; ID

! (Ft) (-ti ;

--

DESCRIPTION ;hampiei FROM ; IO L

1 (Ftflozit ;ozit

0.01 19.01 CASINO

1 19.01 475.01 Massive, medium and coarse grained dark olive green, altered dunite much magnetite between and around aiivine crystals. '6cattered sulfides.

19.0- 31.0 serdentinized fractures t.CJ witn brucite, magnetite

and aSDBEAOS,

63.0- 70.2

NItered ang serbentinized fractures (10-2b'/A.C.( with Aebestas and

magnetite.

93.0- 135.0 ("41tered

an sergentinized fract,(-es (i0-S0'1A,L, with asbestos

brucite and magnetite.

195.5- 204.2 Highlv altered and serdentinizet fractures with cagne- tite and asbestbs threads.

212.0- 217.2 DittD,

262.5- 270.0 Ditto.

315.0- 322.5 !Met).

322.5- 475.0 Few sergentinized !wail fractures (10-70/W.t.1 with carbonate, asbes- tos threads, erythrite and eri te stringers.

Page 94: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I 1

LAUNAMRECESSON DUMUN NICKEL LORPoRMIION Hon # b?-11

-- ; FROM ; DESCRIFfi6N ;&15plei FROM lU; L Pt ; Pg Ni (Ft) i

tfWozit ;aft i -------:

1 475.01 544.01 Massive, medium to fine grained, grey-yellowish to black, altered peridotite ; a..oproximate contacts, Magnetic disseminated fine grained sulfides,

475.1- 544.0 More serpentinized fractures (0-60/64. witn car nate. magnetite, stringers, asbestos threads and erythrite,

1 544.01 824.51 Same as above but more altered.

544.0- 702.5 Alterea seraentinized and more caraonitized fractures (20--/U'IA.C.).

702.5- 717.8 More aiterea, sergentinized anl carbonatizeg stringers.

717.8- 724.5 AitEfit1011 1PCF2ESE to nranodiorite dyke. the core become very haTd like sillci+ication,

724.5- 727.4 Lignt are, coarse grained, aorphyritic granodiaritg dyke, non-magne- tic, chloritized, massive, 30/C.A., contacts, Small veinlets of quartz and carbonate,

727.4- 729.2 !hi:to (117.8 - ?24,t1).

729.2- 783.5 Numerous small veiniets (20-bOiC.h. tilted witu carbonate, magne te and few serpentines,

783.5- 824.5

;

Page 95: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAUNAY-1HECESSON DOMONf MILK:EL cORPORATION Hole # f 87-11 PAGE: 4

----------- FROM ; TO DESCRIPTION :Sample: FROM TO i L 1 Pt Pc Ni ; (Pt) (Ft) :

-

More visible suifldes. :

Disseminated suifides 2.11b; ib03.1i; 9; 9.00O; 3,6d9;

Disseminated sulfides. .u. 9.U.; N.D.; 0.245;

Disseminated sulfides. Lild; )90.5; N.U.:

Dissemlnated sulfides -4%. 211: v.909; V.DOV:

Disseminated sulfides. 21L0; 0. N.D.; 0.603;

Disseminated sulfides. Z12.1; 609...3; b;.1!-„;.;-J; N. u. N.D.; v.1 ,

DISSefairated 2122; bOO.O; bi '3.9; N.D.: N.D.: b,160;

Disseminated sulfides: 61Q.1*J; blit.b; 4.9; N.D.; N.D.; 0.14U1

Disseminated sDifides.

iil SLU1 itet1 su)+Ideq 10-157..

bissemindtea sulfides

i

210;

614.5;

621.1);

b19,;p; 1-3.D;

2.9;

N.V.; O. 0.151;

N.u. 0.359;

Oteseminated aDifideq. We S2Pfl two pilfides; -'ent1a;v1Ite ria; N.D.; 4,D.; 0.105: 20% and pyrrtotite 807..

I 824.51 847.01 Dark grey andesite, fine grained, non-magnetic, chloritized. Few yeinlets (10 1

H. i-111ed witn quartz, cardonate, chlorlte 8115 spii-icie.

828.5- 835.0

Graduaily with wdata nerphyritic feldspar.

: 847.01 :End of hole

(F.L:oz/t QZt

Page 96: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAONA?-1RELESSON PUMON MILKEL -LIRFOFAilUN Hole : Si-11 PAH:

)

UE'dLP1PTION fbampie; HiUM lU; L ; Ft ; Pd ! N1

fotal amount of samples. 12

fotai le. noitn sape = 42.UFt

PRON

iFtf

; fft);ozit lozit

; • :

Page 97: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DUKE NICKEL 3#a¥!* DIAMOND DRILL LO

Property ;gaA.qkEsa

616 4 : &52 %reR:Lwwf Lot :9@ Geel Ga, ■ :21688-1

Level Section: @»50W

Collar E3de#@ : Line : 44+50 w

Station: Sw§N Latitude: 99344

§ozGR; 1450&9w Elevation: 0M0

Date started Awb3R26 Date :»petNA2R±æaw

Cw«e 2eÆ

29th: 299.0 Ft

Deviation . 2#§ , Did Azimut§

0,0

NUN 2 9,

Remarks :w@# PULLED DO, 6 e3 wBORg26 Eaweae2±¥wJ y§ SAMPLES 2124 TO os !%u

Lodged by ROBERT bled

Page 98: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LALt1N`;-!kEi:EH5i1tx 11'sin!.It'•J1 fliILKEi_ LL 7hAtii Hole ~.,-12 RAS}'

FROM , TO DESCRIPTION ;Sample; FHU% ; .„' i L , Ÿt ; Pd TJi .. , Au

;Pt !-tl i ; !~tffZ;t iIZ{t ;kit

1 0.01 97.01 CASING t

1 97.01 299.01 Massive, medium and fine grained, dark olive green altered dunite. Scattered 1

sulfide=- ann ematin magnetite dettèeen and around olivine crystals.

114.0- 117.0

Altered and crus{'!ed i,; ,mal i fragment.

122.0- 131.0

Weil fractured.

131.0- 164.0

[rushed at few spots.

164.0- 166.0

Altered and :rushed.

166.0- 229.0

Altered and serpentiniZed fractures m- o'lL.h.;.

229.0- 231.0

Well fractured.

231.0- 234.0

Weil fractured.

234.0- 284.0

H:tered and 5erCtentiniZe^ frac t+:res i3t!"?L.H, iwitn asbestos dr:icite

and magnetite.

284.0- 299.0

Weil fractured and =rushed.

Weil fractured and cru=-shed. 1124: 2134.,., LSi . ,i

Page 99: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

LAifNAY-TRECESSCIN

FROM i TO É

1 (Ft) 1 (Ft) 1

i 1 i ! ,

i 299.0i ;End of hole k i

DUMONT NICKEL 1CURPÙRATIUN

DESCRIPTION

Well fractured and crushed.

Well fractured and crushed.

Nell fractured and crushed.

Hole #: 87-12

!Sample! FROM Ë

1 : 1 1 1 / 1 1

1 21251 287.81 1 I , 1 I ; 2126: 291.61

E

I } 71 )~,ry i , 2127i 295. 1

i

PAGE: 3

TO É L1 Pt z Pd 4 Ni %; Au,

É 4Fti :ilzit e0zit : !Ûzit

1 1 1 1 I

I 1 I• 1 /

291.66 3.8; ---; ---1 0.340;

I 1 E i

I i I I

295.4; 3.81 ---1 ---É 0.240;

1 1 1

i i

1 ---1 +5• 1

299.01 3.61 i f}.i~Jl

1 i i

1 1

I i

I !

1 : 1 Î i

1

Total aaount of samples= 4

Total length sampled - 15.0Ft

1

1

Page 100: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

DUMONT NICKEL CORPORATION LTD DIAMOND DRILL LOS

Property : LAUNAY-TRECESSON

Hole tt : 87-13

Township: LAUNAY

Lot : 578 Range: V Claia 4 :281688-1

Level : Section: 44 + 50W

Collar coordonate : Line : 44+50 W

Station: 50+00 N

Date started :NOVEMBER 1987

Date completed:NOVEMBER 1987

Latitude: 5000.0 h Azimuth: 220Y 0'

Departure: 4450.00 w 015 : -89 0

Eievation: 0.4.10 Lencith 208.0 Ft

Deviation tests Depth Dip ; Azimuth

Remarks :CASING PULLED OUT, BD SIZE

LABORATOIRE D'ANALYSE BOURLAMADUE LTD

Lopped by : ROBERT OSWALD

Page 101: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I I I I I I I I 1 I I I I I i I 1 I I

LAt1NAY-TRECESSON D(iMONT NICKEL CORFORATION LTD

Hole # : 81-13 tAiit: 2

FROM TO

(Ft) ! )Ft)

DESCRIPTION ;Sample; FROM : TO i L

(Ft)i

i I

o.o! 98.0 CASING

98.0 258.0 Massive, tediut and fine grained, dark olive green altered dunite. Scattered sulfides and much magnetite between and around olivine crystals. Faulted area.

98.0- 111.0 Altered and sernentiniued fractures (1O-60°1C.A.).

111.0- 114.5 Fractured and crushed.

135.0- 137.0 Well crushed.

137.0- 150.0 Weil fractured.

150.0- 153.0 Well crushed.

153.0- 157.0 Well fractured.

157.0- 161.0 Well crushed.

161.0- 185.0 Well fractured.

185.0- 187.0 Well crushed.

187.0- 207.0 Weil fractured.

207.0- 213.0 Weil crushed.

213.0- 241.0 Well fractured.

241.0- 246.2 Well crushed.

246.6- 253.0 Well fractured.

253.0- 258.0

Page 102: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

1 1 I ) I I I I I I I 1

LAUNAY-TRECESSON DUMONT NICKEL CORPORATION LTD

Hole # 87-13 PAGE: 3

1 FROM : TO

DESCRIPTION

;Sample; FROM TO ! L

; (Ft) iFt1

1,Ft/1

; 258.01

Well crushed.

;End of hole

1

Total amount of sample = 0

1

Total lempth sampled = 0.0St

1

Page 103: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

| | | | i | | | | | | | | | | | | | |

&MONT NICKEL CORPORATION DIAMOND DRILL LU

Property ;UaA@EE@a

6287§

@a # : Sd4 Tae@çE~tu%

219,#:actes

GEG&: 495030B Departure: «w 2,w e RKia: 0.0

0a9 4«tw ;q7y6æ 1987 )2t0 cosrtu1l 1V/

f4ziffutn; 220, 0'

Le«, Ft

gel : Section: 4 + w,

LOI eaQaé : E9 : 4580« «#:e: @!w w

Deviation tests w#, : Dip @ a&4

Zwd Ri «2 « 400.0 -74, æ 6002 «2 « 10005 R «

P:em #G :wgw PULLED QC w w2 wHR QGR Æaï2£a6C¥Q3 Du

Cgg m:bæRukkE

Page 104: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

I i I I I I I I I I I i I I I I I I I

LAUtdAŸ-TRECESSOtf DUMONT NICKEL CORPORATION Hole #. 87-14 -At:~E: 2

FROM ; TO 1

(Ft) , (Ft) ,

k I

DESCRIPTION ;Sample'. FRt;f? , ,O L

: tFtfl

0.01 103.01 CASING

103,01 451.01 Massive, medium and fine grained, dark olive green, altered dunite. Magnetic. Scattered sulfides.

103.0- 210.0 Few serpentinized fractures (60-70/C.A.).

210.0- 213.0 Well crushed.

213.0- 263.0 Seraentinized fractures (50'fC.A.) with few small 1i-2't crushed zone.

263.0- 451.0 Largest (3-5') crushed zones.

451.01 1037.01 Same as above but getting more altered (yellowish).

451.0- 652.0 Few crushed zones, altered and seraentinized fractures t30_?U'iC.A.i

filled with asbestos brucite and magnetite stringers.

652.0- 800.0 Crushed zones t2-7'i. More altered, serpentinized fractures

30-80'!C.A.. filled with asbestos brucite and magnetite stringers.

800.0- 953.0 Crushed zones tl-2'i. Altered, serpentinized fractures t20-5O'uC.A.i

with brucite. magnetite stringers and more asbestos.

930.0- 936.0 Gouge.

953.0- 1037.0 More crushed zone t1-5' altered ans serpentinized fractures

(20-50/C.A.) with asbestos and magnetite stringers.

1004.0- 1005.0 Gouge.

1014.0- 1015.0 Gouge.

1037.01 End of hole

Page 105: GEOLOGICAL REPORT, LAUNAY-TRECESSON PROPERTY

Léw*34ÆSa 2Kv NICKEL CORPORATION %&l=6H# «+e

Ra; 3 : (Et, ; (Et) ;

DESCRIPTION ;Sample; 8a; G ! L ~ ; ~ ; (Ft);

lutai amount of sample = a Total !@#asampled = 0.7t