geological and geophysical surveys nov 2 mining … · and geological surveying was completed on...
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42A*3NfM16 2.3137 MCARTHUR
REPORT
ON
GEOLOGICAL AND GEOPHYSICAL
SURVEYS
FOR
WESTFIELD MINERALS LIMITED
MOUNTJOY PROJECT
McArthur Township Property
Timmins Area
Ontario
010
NOV 2 C tt/9
MINING LANDS SICTION
by
Frank P. Tagliamonte, P.Eng.
GEOLOGICAL ENGINEERING SERVICES
29 Beaver Cres. North Bay, Ontario
October 1979
GEOLOGICAL AND GEOPHYSICAL
SURVEYS
REPORT*
WESTFIELD MINERALS LIMITEDMOUNTJOY PROJECT
McArthur Township PropertyOntario
*
INTRODUCTION
Approximately 30 miles of magnetic, electromagnetic,
and geological surveying was completed on the 41 claim property
of Westfield Minerals Limited between 13 August and 23
September, 1979.
The property is situated in the SWest corner of
McArthur Township and overlies two NWest trending bands of iron
formation within felsic metavolcanic rock, principally thinly
stratified tuffs.
Data obtained during the field programme has been
documented on three sets of maps:
1) Magnetometer Survey NW sheet, SE sheet
2) VLF SurveyNW sheet, SE sheet
3) Topographic and geological map NW sheet, SE sheet
A minimum amount of interpretive comment has been used
in the report. The data documented on the maps alluded to above
is complete enough to provide an assessment of the results
- 2 -
obtained with a view to determining the types of additional
exploration work required and the specific anomalous areas
where this work should be directed.
Additional exploration work has nevertheless been
recommended for the LlOON-East of base line anomaly. Bulldozer
stripping and/or diamond drilling are the preferred methods to
be considered.
PROPERTY AND DESCRIPTION
Westfield Minerals Limited holds 41 unpatented
mining claims registered with the Ontario Ministry of Natural
Resources in the Porcupine Mining Division.
The claim group shown on Sketch No. l is oriented
NWest-SEast and is situated between Triple Lake and McArthur
Lake in the South central portion of McArthur Township.
Claim numbers and essential statistics are as
follows:
Claim No.
516802-814
517103-108
522044-047
522056-068
522244-248
Total
No. of Claims
13
6
4
13
J5
41
Anniversary Date
4 October 1978
4 October 1978
4 October 1978
4 October 1978
4 October 1978
- 3 -
LOCATION AND ACCESS
Convenient access to the property is provided by a
good gravel development road which runs south from Timmins
toward Muskasenda Lake and the timbering and mining areas in
the townships further south. This road traverses the SWest
corner of McArthur Township and crosses the McArthur-Bartlett
Townships common boundary immediately south of Triple Lake.
From here a bush road runs through the central portion of the
property in a N-South direction along the East side of Triple
Lake and the Mountjoy River. This bush road is negotiable.rwith
motor vehicles to the approximate centre of the property. It
can be entirely restored to use through the property by
brushing out the overgrowth.
Branch roads from the main bush road traverse the
property in a general E-West direction. One in the central
portion of the property is useable to an old camp location on
the power line, and another through the South portion of the
property is overgrown.
The readily accessible central portion of the
property is about 27 miles from downtown Timmins.
TOPOGRAPHY
Map 3, NW and SE sheets, provides an overview of the
general topographic setting.
Mountjoy River meanders in a general N-South
direction through the NWest portion of the property. It has
- 4 -
carved its course out of fine pleistocene and recent sands.
Sand banks are up to 100' thick or more at the rapids within
the property and vary in height along the extent of its course
down to five feet or so.
All the terrain West of the river and immediately
East of it is gently undulating sand knolls wooded with
jackpine, poplar, birch, and some spruce.
The central portion of the property is drained by
a meandering stream within a relatively broad, flat, NNWest
trending beaver marsh area with random beaver dam basins. To
the East of this drainage system lie low sand knolls wooded
with jackpine and local pothole bogs wooded with small spruce.
The West and Southerly portions of the drainage trough comprises
relatively flat terrain supporting a mixture of evergreens and
leaf trees, mainly poplar.
The SEast portion of the property contains a mixture
of all the features described above but in more limited extent.
Broad cedar swamp areas predominate West of the power line.
Outcrops are sparse. Where present they protrude
along the edges of broader low knolls. Less than 3% of the
property is outcrop.
The entire property is predominantly low in relief.
An extra high voltage power line cuts across the
Easterly edge of the property. The right of way cuts a 300'
wide swath through the extreme Eastern edge of the property.
9HISTORY AND DEVELOPMENT
A brief, generalized review of recorded past
exploration work on the property and immediate vicinity is
documented below. The information listed here has been
derived from supplied copies of documents obtained from the
Resident Geologist's Files in Timmins as well as Ministry of
Natural Resources Geological Reports:
1. Triple Lake Porcupine Gold Mines Limited 1938
Adjoins the SWest pbrtion of the McArthur claims.Shaft to 55 feet.Quartz vein from 1.5 - 3.5 1 wide striking N50 E,and dipping at 60O South on East shore of TripleLake.Free gold and values up to $50.00 Au reported.Band of NW trending intercalated iron formationtraverses the NEast corner of the claim group nearthe boundary with the McArthur Township claims ofWestfield Minerals Limited.
2. Erie Canadian Mines Limited 1938
Two claims near the 2 mile..post between McArthur andBartlett Townships.On SEast projection of a band of iron formation runningthrough the McArthur Township property.Visible gold reported in narrow quartz veins fillingcross fractures in iron formation.Small shaft sunk to 120'.
3. Paymaster Consolidated Mines Limited 1957-1960
Two claim groups worked on: NEast group, and South group. The NEast group overlaps" the NEast portion of the McArthur Twp. property. The South group overlaps the Southern portion of the McArthur Township property.
Aeromagnetic surveying.Ground magnetic and electromagnetic surveying.Diamond drilling:NEast group: 4 DDKs - 2266'No significant assay results for precious or basemetals.South group: 6 DDKs - 2645'.Varying lengths of iron formation intersected.Sulphides of pyrrhotite with minor chalcopyriteintersected.Best assay was 27.41 iron across 29'.
4. Acme Gas and Oil Company Ltd. 1966
The current McArthur Twp. group lies within a largergroup of claims held by Acme in the Township.Short grids were cut over anomalies that lie withinthe NWest portion, and Centre portion of the currentMcArthur Twp. group.Magnetic and airborne electromagnetic surveyingcarried out.A series of magnetic and electromagnetic anomalieslie along NWest tending iron formation bands.Diamond Drilling: 2DDHs - 764'.Iron formation with pyrrhotite and minor chalcopyriteintersected.Hostrocks comprise sediments and some meta-diorite.
5. Abitibi Asbestos Company Limited/ 1973.
A large group of claims held by Abitibi would barelyoverlap the East edge of the current McArthur Twp.group. Ground Magnetic and Electromagnetic surveyingcarried out.
6. Texas Gulf Incorporated, 1972
A large group of claims, formerly held in the Southernpart of McArthur Township and the Northern part ofBartlett Township, overly two parallel bands of ironformation intercallated with intermediate and felsicmetavolcanics.-The Texas Gulf claims occupied the SEast portion ofthe current McArthur Township group.Texas Gulf completed magnetic and electromagneticsurveys on the claims.Magnetic and electromagnetic anomalies are attributedto the iron formations which contain magnetite, minorsulphides and graphite.No data available from an indicated 5 DDKs put downin what is now the extreme SEast portion of theMcAfthur claim group.
GENERAL GEOLOGY
Reference: 1) Map #2363, McArthur and Douglas Twps.
2) Map #2345, Peterlong Lake.
- 7 -
The McArthur Township claim group overlies a NWest
trending band of intermediate to felsic metavolcanics
comprising massive, tuffaceous, brecciated, and lapilli units.
Two narrow bands of metasediments containing iron
formation, chert, and siltstone lie at the approximate centre
of the felsic metavolcanic horizon snaking in a NWesterly
course through it. Narrow, discontinuous mafic intrusive
sills and dykes of the gabbro clan, and olivene diabase dykes,
trend NWesterly within the metavolcanics generally conformable
with the iron formation host structures.
The felsic metavolcanics are flanked on the West by
mafic metavolcanics and broad mafic intrusives. A broad area
of serpentinized ultramafics are located on the East flank.
All these units; the felsic and mafic metavolcanics,
and the ultramafics, are sandwiched between the Peterlong Lake
felsic intrusive complex on the West and the Adams and Geikie
granodioritic plutons on t.he East.
Several prominent NWest trending fault structures
parallel or sub-parallel the NWest formational trend in
McArthur and Fripp Townships.
A large trondhjemite intrusive body in the SEast
corner of McArthur Township and the NEast corner of Bartlett
Township penetrates the felsic metavolcanics and ultramafic
rocks. This unit may represent a feeder for the felsic
volcanics.
- 8 -
LOCAL GEOLOGY
Outcrops are sparse and of limited size within the
property. They comprise no more, but perhaps less than 3% of
the property.
Outcrops intersected by the grid have been located
on Map 3(2). Small samples from each exposure have been
collected and labelled for reference and identification.
Tuffaceous (Tf) rock units predominate. For the
most part these rocks are thinly bedded and all trend NWest -
SEast with dips invariably steeply to the NEast. Individual
observations are as shown on Map 3. Varieties include minor
massive unstratified (T) types and more abundant lapilli (Tl)
varieties. One small Tuff breccia (TV^) occurrence was
observed in the SWest end of the property. Sills or dykes of
the gabbro^diorite (G) clan are next in abundance as shown on
Map 3. These rocks are characteristically granular ranging
from medium to fine grained. They vary from leuco to
melanocratic in composition. Disseminated pyrite is
sometimes present in these mafic intrusives as indicated.
An exposure of fine grained, black, peridotite,
that is noteably magnetic, occurrs on the extreme East end
of line 100N.
A very small questionable felsic intrusive on L112N,
East of the base line is pale pink, fine grained granular and
sparsely mineralized with very fine pyrite. It is probably
a small narrow dyke.
- 9 -
A wedge of pale pink aphanitic felsic material is
exposed on the outcrops on the rapids in the Mountjoy River.
It is situated between the lapilli tuffs and gabbro.
Iron formation is predominantly exposed at three
locations as shown on Map 3. The iron formation is
essentially finely laminated pyritic and cherty material.
This material is occasionally intercallated with fine seams
of magnetite in white chert. Pyrite is the predominant and
most pervasive sulphide noted but pyrrhotite was observed to
occur in discreet lenses or patches on the exposure on the
power line right of way.
The iron formations trend generally NWest - SEast
but are locally contorted and folded.
Two narrow chloritic shears zones generally
conformable with the regional trend of the rock formations
are exposed at the rapids on the Moungjoy River.
SHOWING AND SAMPLING
A small local exposure of sulphide facies iron
formation occurs East of the base line between lines 100N
and 104N.
The iron formation here strikes NSO0*? and dips
steeply Westerly. Both strike and dip are different from
observations made on other areas of the property.
Sample results are shown on Sketch No. 2 and
tabulated below:
-10-
Sample
3
2
1
Width
3'
3 1
4'
OBAu Ag
.002 .28
.002 .12
.002 .04
ppmCu Ln
500 810
240 3400
217 3200
Sulphide iron formation is also exposed at the
following locations:
1. On some small outcrop exposures between L4N andL12N.Westof the base line but adjacent and East of the power line right of way.
2. Within the power line right of way between L12N and L20N.
3. In an old trenched area on L12N 27 -f 50 W.
GEOPHYSICAL SURVEYS
A statistical presentation of the geophysical surveys
is tabulated below:
Line.Cutting
Grid: 400* interval grid lines - whole property.
Stations: 100' interval pickets.
Mileage: Base Line: 2.92 miles (310O - )Grid Lines: 26.70 milesTotal: 29.62 miles
Electromagnetic Survey
Instrument: Crone Radem VLF EM
Parameters: 1) dip angle - degrees2) out of phase - % of normal field
Sources ofPrimary Field: 1) Annapolis, Maryland 21.4 kHz
2) Seattle, Washington 17.8 kHz
Base Stations: Between 150 and 200 on field strength meter.
Readings:
Operator:
Dates:
Plans
50' interval on grid lines.
1) Annapolis, Marylanda) Dip Angleb) Out of Phase
Total
700700nw
2) Seattle, Washingtona) Dip Angle - 2100b) Out of Phase - 2100
Total T2M
Total All Parameters 5600
Frank P. Tagliamonte, P.Eng.
13 August - 23 September 1979
2 - 200 scale plans NW sheet, SE sheet.
Magnetic Survey
Instrument:
Sensitivity:
Parameters:
Barringer GM-122 Protomag.
l gamma-
Vertical component of earth's magnetic field in gammas.
Readings:
Corrections:
Grid Lines Base Line Total
50 ' interval 100'
1) Diurnal2) Base Stations
Base Stations: 400' intervals along base line.
Plans:
Contour Interval:
Operators
Dates:
2 - 200 scale plans. NW sheet, SE sheet
Irregular - 1000, 3000, 5000
Peter TagliamontiClifford McLeodFrank P. Tagliamonte, P.Eng.13 August - 23 September, 1979.
280376
-12-
Supplementary Data
DuplicateReadings: Approximately 300 duplicate readings were
taken along portions of several lines to compare dip angle and out of phase response from each transmitter station. Results were not deemed complete enough to provide meaningful conclusions.
Fraser Filter: Anomalous areas were filtered by the Fraserprocess.Very strong results were obtained on the line 4N-W.est of base line VLF anomaly, whereas the other anomalies produced relatively weaker results.The supplementary data has been recorded on work sheets only.
Power LineInterference: The Extra High Voltage power line which runs
through the Eastern portion of the property interferes to varying degrees both with the VLF and magnetic equipment. Anomalous features along the power line are consequently suspect.
The Line 4N-West base line, VLF and magnetic anomalies are, however, real and to some extent confirmable since iron formations and sulphides are observable on adjacent outcrop exposures on the power line right of way.
MAGNETIC SURVEY RESULTS
A gross review of magnetic data with minimal
interpretive comment follows. The review is based on data and
magnetic contours on Map 2, NW and SE sheets.
Two generally parallel gently arcuate bands (East
and West bands) of iron formation lie along the 310 trending
base line. The iron formation bands are 1600' apart in the
South portion of the property but remain about 1200' apart
NWesterly through the property.
The most prominent magnetic anomaly is identified as
LlOON-East of base line. This anomaly is, a narrow dipole
-13-
feature up to 2400' long on the East band iron formation.
The L4N-West of base line anomaly is a narrow,
perhaps short magnetic dipole anomaly possibly distorted
somewhat by power line interference. It also lies within the
East band iron formation.
A somewhat broader dipole anomaly is situated
between lines 56N and SON West of the base line on the West
band iron formation.
A weaker, narrow, linear expression of the East band
iron formation lies along the base line between L36N and L64N.
ELECTROMAGNETIC SURVEY RESULTS
As indicated on Map 3, NW and SE sheets, there are
4 prominent conductors present in the survey area. An in depth
review of the data will likely produce other not so obvious
conductors and cross-overs.
Those conductors or cross-overs that lie within, or
immediately adjacent to the power line right of way are to be
treated with reservation because of very apparent interference
from the power line.
Two transmitter stations were used during the survey
in order to avoid delay during transmitter shut down periods.
The more prominent conductors are as identified
below:
1. LlOON-East of base line conductor.
This conductor is co-incident with a magnetic anomaly and adjacent to a showing of sulphide facies iron formation that contains anomalous amounts of precious and base metals. See sketch No. 2 ,
The conductor axis is segmented or displaced in the
- 14 -
area of the showing between L100N and L104N. The Southerly projection of the anomaly becomes very weak toward L84N where it is again segmented and possibly displaced.
2. L4N-West of base line conductor.
This is a strong conductor along the scarp edge of a hill and South of prominent iron formation exposures on the power line right of way which contain pyrite and pyrrhotite.
3. L56-L60N along base line conductor.
This conductor lies along a weak linear magnetic anomaly. No surface exposures were observed.
All prominent conductors encountered appear to be
confined to the East band iron formation. These intermittent
conductors are segmented as noted.
SUMMARY AND CONCLUSIONS
Magnetic, Electromagnetic and geological surveys
were carried out over the Westfield Minerals Limited claim
group in McArthur Township, Timmins, area during August and
September, 1979.
The claim group overlies a NWest trending horizon of
intermediate to felsic metavolcanics containing two parallel
bands of iron formation.
The immediate area and some anomalous features
within or adjacent to the iron formation have been sporadically
explored by a variety of companies over the years. The
Westfield programme of geophysical and geological surveying on
400' interval grid lines is the only comprehensive exploration
work carried out over a continuous three mile stretch of
favourably regarded metavolcanics and iron formation.
-15-
Anomalous features comprising the LlOON-East of
base line anomaly suggest one specific area where detailed
exploration investigations should be carried out. There is
no field evidence of any extensive work having previously
been done in this area.
The anomaly may be further investigated by
prospecting, by fill-in geophysical work on 100 interval grid
lines, by bulldozer stripping and rock trenching, or simply
and most expeditiously by a series of diamond drill holes.
A programme of reasonably detailed exploration on
the LlOON-East of base line anomaly will determine the economic
importance of this and similar geophysical and geological
anomolies within or adjacent to the iron formations -
particularly the East band, which appears to be most
responsive to geophysics as shown by the current exploration
work. Data thus derived will dictate the most effective
exploration approach to be considered for other anomalous areas
on the property.
Respectfully submitted,
GEOLOGICAL ENGINEERING SERVICES - ^ 29 BEAVER CRESCENT NORTH BAY, ONTARIO P1A 3N1
WESTPIELDMountjoy project
MOArthur Township propertyTimmins Area
Ontario
CLAIM PLAN SCALE; l'^2640' DATE; NOV. 1979
FPTIT-.w ..w y(.*woe 'OZZU6Z
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522068 j 822064(922089
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MOArthur twp.BM. Bartlett twp.
e F. P. TA6L.1AMONTE Kportion of MNR Plan no. M.298
SKETCH NO. l
INDEX SKETCH FOR MAP SHEET;
1) Magnetometer Survey (2) NW sheet, SE sheet
2) V. L. F. Survey (2) ' NW sheet, SE sheet
3) Topographic b Geological Map (2) NW sheet, SE sheet
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Ministry of Natural Resources File.
tarioGEOPHYSICAL - GEO'
TECHNICAL
TO BE ATTACHED AS AN AFACTS SHOWN HERE NEE
TECHNICAL REPORT MUST CONTA300
Type of Survey(s)Township c Claim Hold
Survey Cor Author of ! Address of Covering D
Total Miles
)r Area M^ A-Ker(s) U^T^'E
Tcsanpany fS^/HQjfti
Report ^Y Qyi^jk
Author j2 ^ fS
ates of Surveyjj^.
of Line Cut.
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
AIRBORNI Magnetome
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(linecutting to office)
DAYS^ i . , per claim Geophysical—Electromagnetic. ,?JU
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S CREDITS (Special provision credits do not apply to airborne surveys) ter Rl*Ttrnrn?gn*-Hr RaHinmprrir
(enter days per claim)
n\\±fi?Q .^r^^^^^V^M^^r^•^ Author-c*fKepoV^r Agent
Res. Geol.'S . 'J O ''y
Qualifications ' ^Previous Surveys
File No. Type Date Claim Holder
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THE TOWNSHIPOF
MCARTHURDISTRICT OF TIMISKAMING
PORCUPINEMINING DIVISION
SCALE;MNCH-4O CHAINS
LEGEND
PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEG
MINESCANCELLED
C.S.
NOTES
400 surface rights reservation along the shores of all lakes and rivers.
RESERVATIONS L
I) -Reserved for recreational purposes jnder Sec 3 PI .A. File IBB543
DATE OR ISSUE
MOV 3 01979
SURVEYS AND MAPPING
PLAN NO.- M .298
ONTARIO
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