42A06SE0065 OP91-243 ELDORADO010
GEOLOGICAL REPORT
ON
ROUSSEAU PROPERTY
ELDORADO TOWNSHIP
PORCUPINE MINING DIVISION
TiBBins, Ontario August 18, 1989
John R. Boissoneault, B.Se., P.Eng.
Geologist, Engineer
42A06SE006SOP91-243 ELDORADO ————————— 01 OP
TABLE OF CONTENTS
Page
INTRODUCTION 1=2
PROPERTY DESCRIPTION S. LOCATION 2
TOPOGRAPHY S. ACCESSIBILITY 2-3
HISTORY 3-5
REGIONAL GEOLOGY 5-6
LOCAL GEOLOGY 6-9
ECONOMIC GEOLOGY 9-11
CONCLUSIONS 11-13
RECOMMENDATIONS 13-14
APPENDIX
1) Location Map
2) Claim Map
3) Local Geology
4) Ontario Geological Survey/ Map 2455
5) Chemical Analysis Certificate
- l -
INTRODUCTION
The following report is an evaluation of a
property consisting of 24 claims located in the north-
central part of Eldorado Township in the Porcupine Mining
Division of northeastern Ontario. It has been prepared
at the request of Mr. Robert Rousseau of Timmins, Ontario.
The report is based partly upon sources of information
available at the Ministry of Natural Resources, Department
of Mines. These include:
1) Ontario Geological Survey Report 219 with Map 2455
(The Geology of the Timmins Area by D. R. Pyke, 1982)
2) Ontario Geological Survey, Study 20, Nickel Sulphide
Deposits of the Abitibi belt, by Paul R. Coad, 1979
3) Ontario Department of Mines, Report 121
(Geology of Adams and Eldorado Townships, by
D. R. Pyke, 1975)
4) Ontario Geological Survey preliminary Map P 2114 and
Map 81096 (Geophysics)
5) Geological Compilation Series, Map 2205
(Timmins-Kirkland Lake, 1972)
6) Stratigraphic Relationships, Geochemistry and Genesis
of the Redstone Nickel Deposits, Timmins, Ontario
by Donald James Robinson, 1982
7) Assessment work on file at the ministry office in
Timmins, Ontario.
It is also based upon my personal knowledge of the
Timmins area and the property which I visited in August
of 1989.
1*'^
- 2 -
The property is evaluated as a nickel, copper
prospect on the basis of the regional and local geology,
the nature of the mineralization on the property and the
history of exploration, development and production in the
vicinity. It is recommended that an exploration program
be undertaken on this property.
PROPERTY DESCRIPTION AND LOCATION
The claim block lies in the northcentral part of
Eldorado Township, its center being near the north-south
medial line, two miles from the northern boundary. It
consists of 24 claims, a total of 960 acres, forming a
block \ \ miles long from east to west and about l mile long
from north to south.
The following is a list of the claim numbers:
-1034230- 4034236 IW570
1031223 103*831 1034237
II6I564A&
** 1034226 1.034232 1034238
.\lii ivaizi'a i w.i't 1 1 f 1-034233 pi-
U03422D 1034228- 1034234 .1034240
1Q&TF21 . 1034229 H)34235
These claims were staked by George Fournier and recorded
on April 5, 1988. On March 31, 1989, an extention was granted
until December 15, 1989.
TOPOGRAPHY AND ACCESSIBILITY
The area in the vicinity of Eldorado Township is
typical of the Precambrian Shield in the Timmins Region.
It is low and flat, with little relief, its elevation being
- 3 -
about 950 feet above sea level. The western part of the
property is forested mainly by spruce and balsam/ with
poplar in the higher areas while the eastern part is quite
swampy and covered by tag-alders and black spruce.
The overburden is quite thin over most of the property,
generally less than 20 feet in depth, and there are a fair
number of outcrop particularly in the central and western
parts. The northern section/ however, has deeper overburden/
in the order of 100 feet. The water table is high and
there are a number of small lakes in the vicinity. The
Redstone river winds through the western edge of the claim
group, near the boundary.
The property is located about eleven miles southeast
of the center of the City of Timmins. Access is easily
gained from Timmins via Highway 101 to South Porcupine
and a good secondary road, which runs southward through
Shaw Township into Eldorado Township, passing about 3/8
of a mile to the east of the claim group, a distance of
about twenty miles. The City of Timmins is connected to
Toronto by highway, railway and airline services.
HISTORY
The earliest record of exploration activity on the
property dates back to 1947, when the ground was held by
MERCURY INVESTORS LTD. Mapping was done on a scale of
l in - 400 ft. A sample taken from a narrow quartz vein
on the east side of the river, yielded a high assay in gold/
but follow-up work, consisting of trenching, stripping and
- 4 -
the sinking of a shallow shaft, failed to discover further
gold values.
In 1966, ACME GAS AND OIL LIMITED followed up an
airborne survey with ground magnetics and electromagnetics
over a large claim block, which included the present property.
In 1971, two diamond drill holes were put down, one on what
is now claim 1034239 and one on present claim 1034229. In
1988, the Ministry released Ontario Geological Survey,
Map 81096, showing the results of an airborne electromagnetic
survey of Eldorado Township. The present claims were then
staked by George Fournier and Robert Rousseau because of
three groups of anomalous responses which were detected
on the property.
Exploration for nickel was started in the region
by TEXASGOLF SULPHUR COMPANY in 1959, in the eastern part
of Langmuir Township. A geophysical survey was carried
out and two core holes were drilled. MINING CORPORATION
OF CANADA carried out an exploration programme in the area
during 1964 to 1966 and, in conjunction with INCO, had
completed 32 holes by 1972, which led to the discovery
of the two Langmuir nickel ore deposits.
Exploration leading to the discovery of the McWatters
deposit to the southwest, was started in 1961. The Hart
deposit on the eastern edge of Eldorado Township, was
discovered by NORLEX MINES in 1964.
The Redstone deposit immediately south of the
subject property, was discovered during the period of 1977
-5-
to 1979 by UTAH MINES LTD and i s now in production as a
result of a joint venture between this company and
TIMMINS NICKEL.
REGIONAL GEOLOGY
The property lies within the Superior Province of
the Precambrian Shield which underlies much of northern
Ontario and northwestern Quebec. Locally/ a large belt
of isoclinally folded metavolcanics and metasediments of
Archean age (early Precambrian), commonly referred to as
the "Abitibi greenstone belt", crosses the region in an
east-west direction, extending eastward into Quebec. These
metavolcanics and metasediments, which have a general local
strike of north-70o- east, have been intruded by felsic
and mafic plutons and by a large number of diabase dikes.
Two ages of volcanics are recognized. The older
"Deloro group" is about 5000 metres thick and consists
mainly of a calc-alkaline seguence of andesites and basalts
in its lower part and of dacitic flows and felsic pyroclastics
in its upper part. The younger "Tisdale group" is about
4000 metres thick and is mainly ultramafic and basaltic
in the lower part, with considerable volcanoclastic dacite
in its upper part.
The metasediments are referred to as the "Porcupine
group", and are about 3000 metres thick. They consist mainly
of interlayered greywacke and siltstone with lesser quartz
conglomerate sections. These are time equivalent with the
"Tisdale group" and the upper part of the "Deloro group".
- 6 -
The intrusive rocks include sill-like bodies of
ultramafic rocks, some of which have gabbroic caps, and
are confined to the "Deloro group" and small quartz-feldspar
porphyry stocks, which may be subvolcanic in origin, and
occur mainly within the lower part of the "Tisdale group".
All of the previously mentioned rock types, have
been cut by numerous diabase and quartz diabase dikes of
Proterozoic age (late Precambrian). The large and younger
dikes have a strike of north-70o-east, but numerous small
and older dikes trend north-south or northwest-southeast.
A major structural feature, the Destor-Porcupine
Fault crosses the region in a general east-west direction.
However, where it passes north of the property, a distance
of about nine miles, its strike is north-70o-east (70O ).
A number of prominent subsidiary faults, whose strikes
vary from north-south (1800 ) to north-500-west (125O ),
cross the region, offsetting the stratigraphy, and the
main Destor Fault to varying degrees. These include the
Montreal River fault and the Burrows-Benedict fault.
LOCAL GEOLOGY
In the region immediately south of the Destor-Porcupine
Fault, the metavolcanics have been folded into a large
elongated dome, which occupies most of Deloro and Shaw
Townships, as well as the northern half of Eldorado Township
and the northwestern corner of Langmuir Township. It is
known as the "Shaw Dome". The dimensions of the structure
at bedrock surface are about 15 miles east to west and about
- 7 -
8 miles north to south, with the major axis of the fold
crossing the southern halves of Deloro and Shaw Townships in
an east-west direction. There are numerous minor complexities
in the fold, but generally, the dip is steeply outward along
the margins and flatter towards the interior. The upper
"Deloro Group" is well exposed along the northern and southern
edge of the dome, the iron formations providing good marker
horizons. The upper "Deloro Group" lies to the inside of the
margins and the lower "Tisdale Group" lies to the outside.
The metavolcanics of the Shaw Dome have been intruded
by conformable ultramafic masses of peridotite. These have
compositions approaching dunite and are found mainly in the
lower flows within the interior of the dome. The upper parts
of these sills have differentiates of coarse grained hornblende
gabbro and quartz gabbro. The intrusives are chemically
similar in their composition to the lower Deloro volcanics.
The southern margins of the Shaw Dome cross the
central part of Eldorado Township and enter Langmuir Township
to the east. Along this area, a thick section of the calc-
alkaline dacite and dacitic pyroclastics of the "Boomerang
formation", which make up the upper Deloro Group, reach
bedrock surface and outcrop in several places. Sulfide facies
iron formations lie concordant with and near the top of this
section. Komatiitic ultramafic flows of the basal Tisdale
group overlie the dacites and iron formations stratigraphically
along the margins of the dome. The Komatiites are, in turn,
overlain by a thick sequence of tholeiitic basalts of the
- 8 -
Schumacher formation. Numerous sub-volcanic porphyry lenses
are interbedded within both the dacites-pyroclastics and the
komatiites. Two large granitic plutons are present, one
occupying the region to the southwest and west of the area
and the other, which is smaller, occupying the eastern part
of Eldorado Township, within the Shaw Dome.
The strike of the volcanic formations is southeasterly
as they enter the northwestern part of Eldorado Township,
changing to easterly as they cross the Township into Langmuir
Township. The dip is predominantly southwestward and southward
(away from the center of the dome). Isoclinal folding is
common along this belt and has been observed by Pyke (1975)
and Green (1978); this has caused interfingering of the
dacitic tuffs and komatiitic flows, in several areas. A series
of large subsidiary faults, including the Burrows-Benedict
fault (described under "Regional Geology 1'), cross the western
and central parts of Eldorado Township in a southeasterly
direction, causing small displacements in the formations
previously described. Several diabase dikes, of considerable
width 200* - 300' cross the region, in a direction of
north-70o-east.
The Rousseau property covers a large section of
komatiitic volcanics, which trend in a general east-west
direction. The western part of this belt has a surface width
of approximately \ mile and is cut by two north-south faults;
in both cases, the western side was moved southward, for a
total displacement of about 1000 feet. At the eastern end.
- 9 -
where the width of the section is about k mile, it terminates
against another fault, which crosses the region in a north
westerly direction; granitic rocks lie on the other side of
this fault. To the north and south of the komatiite belt,
lie massive dacite flows and pyroclastics, which also strike
east-west and dip southward; they also terminate against the
northwesterly striking fault. A large diabase dike crosses
the eastern and southern parts of the property in a direction
of north-700-east. The komatiite, which consists of about
60/6 olivine, shows considerable variation in structure, some
sections being massive, while others show various amounts of
schistocity and alteration to serpentine. One altered area,
which outcrops in several places on claim 1034226, is strongly
sheared in a northeast direction, over a width of several
hundred feet; the shears contain a large amount of reddish
brown oxide and ferro-carbonate. The dacite flows are massive
but contain areas of disseminated pyrrhotite in several places.
ECONOMIC GEOLOGY
The nickel deposits of the area are confined to the
southern margins of the Shaw dome, and specifically, near the
contact between the overlying dacitic rocks of the upper
Deloro Group and the underlying komatiitic flows of the lower
Tisdale Group, and generally closely associated with the iron
formations, at the top of the former. The sulfide facies iron
formations are semi continuous and, in most cases, appear to
be time equivalent with the nickel deposits. They are often
present lateral to a deposit, but may be absent for much of
- 10 -
its length, and, in some cases, they overlap the deposit
when it is in contactr.with'.the -komatiite^ Although the
nickel deposits generally lie at the contact (stratabound),
in some cases, they extend within the komatiite formation;
and in other cases, they lie solely within the dacitic tuffs,
or sub-volcanic porphyries.
The mineralized areas are commonly mantled by ferro-
carbonate zones and enclosed within a sequence of metasomatized
silicates (talc, chlorite, calcic-amphibole, biolite). They
are sometimes overlain by a thin layer of chloritic rock.
The nickel deposits generally consist of massive
sulfide lenses, several feet thick at the contact, and varying
degrees of disseminations, usually on the komatiite side,
for some distance. The sulfides consist of pentlandite
((Fe, Ni) S), pyrrhotite ( Fe-jSg), millerite (NiS), pyrite
(FeS2) and minor chalcopyrite (CuFeS^)- The pentlandite has
a low nickel tenor when associated with pyrrhotite and a
high nickel tenor when associated with millerite.
Robinson (1982) suggests that evidence at the Redstone
deposit indicates that the sulfide layer was emplaced prior to
the overlying komatiite and has a volcanic-exhalative origin.
He further suggests-that-the-sulfIde~layer"was overlain" by a
thin section of dacitic tuffs which were metasomitized to
chloritite by the komatiitic lava.
The following is a description of some of the nickel
sulfide deposits in the vicinity:
- 11 -
1) Langmuir deposits l S, 2 ( western Langmuir Township)
mined 550,000 tons grading 1.59& nickel
reserves 860,000 tons grading 1.759S nickel S Q .6% copper
2) McWatters deposit (western Langmuir Township)
zone 60 m wide grading Q .43% nickel (sub-economic)
3) Hart deposit (eastern Eldorado Township)
zone 9 m wide, 200 m long, discontinuous nature makes
deposit sub-economic, despite grades of up to 2 .OK nickel
over 3.6 m in width.
4) Redstone deposit (westcentral Eldorado Township)
original reserves of 350,000 tons grading 2.956 nickel to
a depth of 800 feet, now greatly enhanced by a drill hole
intersection at a depth of 2,700 feet which graded 2.76?6
nickel over a width of 19.6 feet. Presently in production
at the rate of 9,000 tons per month.
CONCLUSIONS
Undoubtedly, the dacite-komatiite contact zones
around the periphery of the Shaw dome have considerable
potential for the occurrence of nickel sulfide deposits,
particularly in the vicinity of iron formations. Four of
these deposits have been discovered to date, at least two of
which are of commercial significance. The recent initiative
taken by TIMMINS NICKEL, combined with the recent rise in the
price of the metal, has resulted not only in making the
Redstone deposit an economic reality but also on focussing a
considerable amount of attention on the area.
- 12 -
If one examines Ontario Geological Survey, Map 2455,
the important strategic location of the Rousseau property
becomes evident. This property, tied on to the northern
boundary of TIMMINS NICKEL, has approximately six miles of
dacite-komatiite contact, the geologic horizon which has
hosted the nickel deposits of the region.
Several zones of anomalous electro-magnetic conductivity
have been located, on the claim group-, by previous surveys
(see "Local Geology"). One of these, a ground vertical loop
conductor, may be of considerable importance since its axis
appears to be located near, and parallel to, the north contact
between the dacitic and komatiitic formations; this anomaly
was not properly tested by drilling, although this was attempted,
in the past, the hole having entered a diabase dike at the
point where it cuts through the conductor. Another ground VEM
conductor lies in the northern part of the property, in the
dacites; it also appears to have been improperly tested. Two
airborne electromagnetic anomalies may also be of interest,
since they are unaccounted for; one of these lies in the
dacitic formation, in the northwest quarter of the property/
and the other lies near the southern contact, in the southeast
quarter.
Because of the isoclinal folding, along the outer
margins of the Shaw dome, it is possible that the geologic
section at the Redstone deposit repeats itself to the north,
in a series of tight, truncated synclinal and anticlinal
-13-
structures. This possibility becomes evident on examination
of Ontario Geological Survey, Map 2455, which shows a series
of komatiite bands to the north of the Redstone deposit, the
largest of which crosses the Rousseau property. The occurrence
of iron formation in a drill hole, to the south of the property,
supports this possibility.
Finally, three important characteristics of the
komatiite formation, on the property, have been revealed
through field examination of outcrop and analysis of samples.
Firstly, ultramafic contains anomalous nickel values up to
0.16/6. Secondly, a large sheared area contains substantial
ferro-dolomite carbonatization, some of which has been
oxidized, a feature common in the vicinity of nickel sulfide
deposits in the area. Thirdly, this rock type is similar,
in several aspects, to those which host these nickel deposits.
For these reasons, it is my opinion that the Rousseau
property is an excellent prospect for the occurrence of
nickel sulfide deposits, and that the exploration of this
claim group is definitely warranted on the basis of the facts
which have been presented in this report.
R ECOMMENDATIONS
Due to the nature of the mineralization, which is the
target of exploration on this property, and its association
with iron formations, a geophysical program consisting of dual
frequency electromagnetics supported by a magnetometer survey
is recommended, with the ultramafic-dacitic contacts as the
main focus. These surveys should be conducted along north-
- 14 -
south picket lines, 100 metres apart and the entire property
should be covered.
The geophysical program should be followed up by
surface stripping of the anomalous areas, where overburden
thickness permits, and by diamond drilling, where it does not.
This second phase would be greatly facilitated by the building
of a road, if a suitable route can be found.
The following is an estimate of the costs of the
recommended programs:
1) Geophysics
a) line cutting: 25 miles @ $400/mile =$10 000
b) dual frequency E-M (150 m cable):
: 25 miles @ SBOO/mile = *7 500
c) magnetometer survey: 25 miles @ $160/mile= $4 000
d) interpretation, report: = ? 2 500
Total Geophysics Sf24 000~ ~~ . .i
2) Surface stripping: 16 days @ $1000/day '^f =$16 000
3) Diamond drilling: 2000 feet @ $20/ft =$40 000
4) Building of road =$20 000
5) Supervision, engineering B, other costs =$20 000
•i- 10* contingency ^ 12 000
TOTAL OF ALI. PROGRAMS ^fl32 000
Respectfully submitted
John : R!. J Solisso'MWuit^ B. Se. P. Eng,
GeologistV.Engin'e.tfr/
42A06SE0065 OP91-243 ELDORADO
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Swastika LaboratoriesA Division of Assayen Corporation Ltd.
Assaying - Consulting - RepresentaUon
Geochemical Analvsis Certificate
Company:Project:Ann:
R. ROUSSEAU
2W-0060-RG1
JAN-23-92
We hereby certify the following Geochemical Analysis of 13 DRILL CORE samples submitted JAN-16-92 by BILL KERR.
Sample Nurber1201 1202 1203 1204 12051206 1207 1208 1209 12101211 1212 1213
Cd PFM
1 2 2 2 22 1 1 2 11 1 2
Co PFM92 88 87 93 8988 88 89 82 8173 76 15
Ni PAI2340 2400 2300 1420 24402450 2260 2340 2180 21801940 2080
73
RH Pt ppb PPB
^ -CIO ^ ^0 ^ ^0 ^ ^0^5 ^.IQ
^ -CIO ^ ^0
Pd ppb
1
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Co-R
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c.0
Certified by QC
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244. FAX (705)642-3300
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IM4O IS^Z*
INFORMATION T APPEARS ON THIS •4AS Bf EN PROM VARIOUS AND ACCURACY IS
WISHING TO STAKE k IN INQ CLAIMS SHOULD C6N 5ULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP WENT AND MINES. FOR AD DITIONAL INFORMATION ON THE tTATUS OF LANDS SHOWN
Douglas Tp. - M. 274
THE TOWNSHIP OF
ELDORADODISTRICT OF TIMISKAMING
PORCUPINE MINING DIVISION
SCALE: 1-INCH *4O CHAINS
LEGEND
FATtNTCO LAND CROWN LAND SALE UAtCBLoairco LANDLICCNSC OF OCCUPATION MINING ftltMTt ONLY SURRKC HIOHTf ONLY
MPNOVEOKlNfl^ HlOHWAYtRAILWAY!POWER LINESMARSH OR MUSKCO
IAT|iNT.D SRO. *
* C.
eNOTES
400 Surfac* Rights Retfrvotion along tht thoret cf oil lokti and nveri
r hit township lies within the Municipality of UT Y of TIMMINS
SAND andGRAVEL
Hi
OHAVH. F li t IfltM 04 Ktt I7t**4
DULU* (NiiMi'H) *IM(HH* *CCLH * 1(0" uwOtP i n*
|ANL)A f NO H llMLM^Wh
pnLOl UN i iMllffi KtHOINtf APPl x ATlOfc "NUtN ! H*
l *HU* ALI S H O WITHDRAWN
PLAN NO. (Vi. ?76
r * - * n r- r\CTUrNATURAL
4*.
REFERENCES
AREAf WITHDRAWN FROM OtyOfcMTION
M.R.O. -MINING RIGHTS ONLYS.R.O. - SURFACE RIGHTS ONLYM.+ S. - MINING AND SURFACE RIGHTS
DwrliMlon Orator N*. D*** OlNMtltJon PH* lit H/tt——0*V*6———IJiOiO*——M.*-*——— l*i*lll
NOTES
THIS TOWNSHIP Lire WITHIN THE MUNICIPALITY OF
MIGHTS ON NiDHiHtwK L*nt TO THE CONTOUR(LlVATlON 9 0\ B ' NCSCftVEO TO ONT H.VOHO
THE INFORMATION THAT APPEAR* ON THIS MAP HA8 BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY 18 NOT GUARANTEED THOSE WISHING TO STAKE MIN MO CLAIMS SHOULD CON 8ULT WITH THE MININGRecoftoea MINISTRY OFNORTHERN DEVELOP MEMT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HflRCON.
•5
.J TP
f ^V *.M A * MottF- -- -—- -* i—— -^ -w ——i —- —— —v^^ -^ -^ ^ *w ^
l -- i ll*7*7t l 11*7*71 11*7*74
7*99'. i H B*JllM044 ' 11)0041 ' Iisb04*' ( ||*OO47jC^.,—'—' v "r 70*04---
4—4"
™W*M j 'P****T JP.—t—-r4
..-, L-~—l—t-—r"""^ ''i \ ! i A 1
M* M1 ST"
FALLON TP.
r u
LEGENDHIGHWAY AND ROUTE No M OTHER ROADS sa TRAILS ~ SURVEYED LINES
TOWNSHIPS. BASE LINES. ETC *- LOTS. MINING CLAIMS, PARCELS. ETC -
UNSURVEYEO LINESLOT LINES — PARCEL BOUNDARY — MINING CLAIMS ETC ~-
RAILWAY AND RIGHT OF WAY *- UTILITY LINES -*- NON-PERENNIAL STREAM — F LOODING OR F LOOQING RIGHTS ti SUBDIVISION OR COMPOSITE PLAN 32 RESERVATIONS BJBj ORIGINAL SHORELINE . . MARSH OR MUSKEG 1̂ MINES TRAVERSE MONUMENT
DISPOSITION OF CROWN
TYFt OF DOCUMENTPATENT, SURFACE ft MINING RIGHTS
.SURFACE RIGHTS ONLY......" .MINING RIGHTS ONLY,— .
LEASE, SURFACE ft MINING RIGHTS.." .SURFACE RIGHTS ONLY........" .MINING RIGHTS ONLY......,.,
LICENCE OF OCCUPATION ... . ...,OROER-IN-COUNCIL .. . . .RESERVATION
SANO'II GRAVEL
NOT! MINING RIGHTS IN PARCELS PATfNTfD l 1*13. VC8TCO IN ORIGINAL PATiNTEE LAND* ACT K S O IB70 CHAP 3*0, SE
SCALE: 1 INCH - 40 CHAINS
FEtTO 10OO 7000 4000 6OOi
O 200 METRES
1000H KM)
TOWNSHIP
LANGMUIRM.N.R. ADMINISTRATIVE DISTRICT
TIMMINSMINING DIVISION
PORCUPINELAND TITLES/ REGISTRY OIVISIOI
COCHRANEMinistryof LandNatural ManageResources Branch
Ontario
MARCH, 1985N*m**rG-:
eSEooes opoi-243 ELPORADO 210
