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41J11SW0033 OP91-638 GOULD f) 1 O
U. PELLERIN PROSPECT
LOCATION:
The Footprint Lake Property is a 12 claims Group in Gould Township, Sault St. Marie District, lot II and 12 Concession 5. Property is accessible by gravel bush road turning Westward from Highway I29 at Huston Lake for approximately 2.5 kilometers.
GEOLOGY:
The claims group are in a sedimentary Huronian age close to diabase dykes and sills of cobalt series, quarts veins systems and shears zone are the best structures for copper occurence.
GEOPHYSIC:
VLF, EM 16 was carried out on the property for 6.2 kilometer, data collected at 25 meter intervals. Conductor: 2 strong conductors in North East. 2 weak conductors in South West (map included).
GEOCHEMICAL:
32 soil samples were collected with ground auger at approximately l to l 1/2 meter depth, screened at 8 mesh fine, assessed by Bell White Lab. of Haileybury, Ontario. Some anomalus values of I85 to I94 P.P.M. copper in soil samples.
ROCKS:
Grab samples taken in IO pits, (see enclosed map) return low values in Gold. From IO to 97 P.P.B., AU.
AG.
From 2.0 to 70 P.P.M. CU. 207o to 90xfc (sheet attached).
RECOMMENDATIONS:
Follow up by detail prospectings of ULF, anomaly with coincident of Geochemical in soils, Detail Grid at 50 meter spacing lines over anomaly zones, magnetometer on exisiting grid line and diamond drilling.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 1 87, POJ 1KO
HAILEYBURY, ONTARIO
nf Analysis
TEL: 672-3 1O7FAX: (7O5) 672-5843
NO. 0544
SAMPLE(S) OF: Fines (32) Rock (10)
SAMPLE(S) FROM: Mr - u- Pellerin
DATE: NoVember 13, 1991
RECEIVED: November 1991
Sample #
2-4973-4984-4985-5006-500 7-5018-5019-50110-501
Auppb
1015121525 18973323
Agppm
NDNDND2.04.0 40.2.070.42.
Cuppm
7948441074
Cuo, "O
2.866.52 8.683.064.469. fin
NOTE: ND denotes not detected,
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE A NALYTICAL LABORATORIES LTD.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 1 87, POJ 1KO
HAILEYBURY, ONTARIO
nfNO. 0 544
SAMPLE(S) OF: Fines (32) Rock (10)
SAMPLE(S) FROM: Mr. U. Pellerin
TEL: 672-3 1O7FAX: (7O5) 672-5843
DATE: November 13, 1991
RECEIVED: November 1991
Auppb
Sample #
1-4972-4973-4984-4985-4986-4987-4988-4989-49710-49711-49812-49813-50014-50015-49916-49917-49918-50019-50020-30121-50122-50123-50124-50125-50126-50127-50128-30129-30430-30431-30332-3031-497 15
Agppm
3.40.81.00.80.40.60.21.00.60.21.00.63.44.00.20.60.40.40.20.20.61.00.60.81.21.20.41.62.00.61.00.6ND
Cu Cuppm %
77419027193020232147161119732562510185185938147261546211941816121266 R tx-K SH^ste "S
NOTE: ND denotes not detected,
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
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41J11SW0033OP91-638 GOULD
020
REPORT ON A VLF-EM SURVEY OVER PART OF THE FOOTPRINT LAKE PROPERTY
GOULD TOWNSHIP SAULT STE. MARIE MINING DIVISION, ONTARIO
July, 1991 Seymour M. Sears
SUMMARY
A VLF-EM Survey was carried out over a six (6) claim Property in the Thessalon area of northern Ontario. The claim group is situated in an area underlain by Huronian sedimentary rocks, granitic intrusive rocks and Nipissing aged diabase dykes. Similar geological environments along strike to the east (the Cheney Mine Prospect) and immediately north of these claims (the Gould Copper Prospect) are locally host to copper bearing quartz vein systems.
The reconnaissance scale VLF-EM survey detected several conductors that should be prospected for similar copper mineralization. Detailed linecutting, prospecting, geophysical and geological surveys are recommended on these claims.
Wawa, Ontario Respectfully submitted. July, 1991
Seymour M. Sears, B.A., B.So. Geologist
11
41J11SW0033 OP91-638 GOULD
TABLE OF CONTENTS
PAGE
SUMMARY . . . . . . . . . . . . . . . . . . . . . . . . . i
INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . l
PROPERTY. . . . . . . . . . . . . . . . . . . . . . . . . l
LOCATION AND ACCESS . . . . . . . . . . . . . . . . . . . l
TOPOGRAPHY AND VEGETATION . . . . . . . . . . . . . . . . l
PREVIOUS WORK . . . . . . . . . . . . . . . . . . . . . . 4
REGIONAL GEOLOGY AND MINERALIZATION . . . . . . . . . . . 4
WORK PROGRAM. . . . . . . . . . . . . . . . . . . . . . . 5
DISCUSSION OF RESULTS . . . . . . . . . . . . . . . . . . 5
CONCLUSIONS 6 RECOMMENDATIONS . . . . . . . . . . . . . . 6
REFERENCES . . . . . . . . . . . . . . . . . . . . . . . 7
STATEMENT OF QUALIFICATIONS . . . . . . . . . . . . . . . 8
TABLE OF FIGURES
Fig. 1. REGIONAL LOCATION MAP . . . . . . . . . . . . . 2
Fig. 2. CLAIM MAP . . . . . . . . . . . . . . . . . . . 3
LIST OF MAPS
Map No. l VLF-EM SURVEY - PROFILE DATA . . . . . Back Pocket
Map No. 2 VLF-EM SURVEY - FRASER FILTERED DATA . Back Pocket
020C
INTRODUCTION
This report is designed to present the results of a VLF-EM survey carried out over reconnaissance scale grid lines over the six claim Footprint Lake Property of Mr U. Pellerin. The survey was completed by S. Sears of Sears, Barry and Associates Ltd. on June 30th and July 1st, 1991.
PROPERTY
The Footprint Lake Property consists of six (6) contiguous unpatented mining claims, located in Gould Township, Sault Ste. Marie Mining Division. The claims are shown on Figure 2 and are numbered as follows:
SSM 1024301 SSM 1098499SSM 1098497 SSM 1098500SSM 1098498 SSM 1098501
LOCATION AND ACCESS
The property occupies parts of Lots 11 and 13, Concession 5 in Gould Township. Footprint Lake, which lies near the center of the property, is located approximately 50 km north of Thessalon, Ontario.
Access to the claim block is achieved by means of a 2.0 km seasonal bush road that departs westward from Highway 129 at Houston Lake near its outlet into Jobammageeshig Lake.
TOPOGRAPHY AND VEGETATION
The property is generally flat with a maximum relief of less than thirty (30) metres. Overburden is relatively shallow, and bedrock exposure is quite plentiful. Drainage is primarily restricted to a northwest trending lineament that passes through Footprint Lake. This drains towards the southwest through a small pond in the southwest corner of the claim group.
Vegetation consists of relatively mature stands of poplar,maple and birch, typically associated with dense undergrowth..The lowland areas contain cedar, spruce and balsam.
95'
U. PELLERIN FOOTPRINT LAKE PROPERTY
SEARS, BARRY S ASSOCIATES INC
9cr
Fig. h Regional Location Map of Ontario.
-*v, 4 -'.. -; ** •V V^v. 3? •- -- '
^•. W *^---.~ . — -i - -;- -^-^-
FIG. 2 Claim Location Sketch - Footprint Lake Property of U. Pellerin; Part of Claim Index Map G.3278, Gould Township, Sault Ste. Marie Mining Division, Ontario.
PREVIOUS WORK
The area covered by the survey was included in regional geological mapping of the Saunders Lake Area for the Ontario Division of Mines by F. W. Chandler (1976), although it is very close to the extreme southeast limits of the map sheet.'
There is no documented work in the assessment files at the Sault Ste. Marie resident geologists Office on the claim group covered by this survey. However, both the Chenev Copper Prospect (2.5 km east) and the Gould Copper Prospect (1.5 km north) have been explored by underground workings and seen limited copper production.
The O.D.M. Geological map of Chandler (1976) shows a copper occurrence, quartz vein and "pit" to be located south of the west end of Footprint Lake. It is shown as striking east-west and may be on strike with the Cheney Copper Prospect. This prospect was not observed during the survey.
REGIONAL GEOLOGY AND MINERALIZATION
According to Chandler (1971), the Footprint Lake Property of U. Pellerin is underlain by Cobalt Series, Huronian aged sedimentary rocks. Nipissing aged diabase dykes and sills ar assumed to cross-cut these rocks, locally.
The immediate area surrounding the surveyed claims hosts many copper occurrences, most noteworthy of which are the Gould and Cheney Prospects. The host quartz veining is often intimately associated with Nipissing Diabase dykes and sills. Copper occurs as chalcopyrite, chalcocite and various carbonate and oxide minerals. It is associated with pyrite, specularite and iron carbonates. The quartz vein systems appear to be developed within shear zones in all rock types. Several of the known prospects in the area contain lenses of up to 50 56 sulphides in widths up to several metres.
Both the Cheney and the Gould Prospects occur within east- west striking quartz-ankerite vein systems that are, at least, spatially related to a major northwest trending shear structure. There are numerous lesser known occurrences along this linear structure, and evidence indicates that other copper occurrences may be associated with parallel shears. The northwest trending lineament which passes through Footprint Lake and the surveyed claims may constitute one such parallel structures.
WORK PROGRAM
METHOD
The VLF-EM survey was carried out along north-south cut lines established at approximately 200 metre intervals accross the claim group. This involved 6.2 kilometers of grid. Data wascollected at 25 metre intervals.
The data was collected utilizing a Geonics "EM-16" VLF-EM instrument. As with any VLF-EM method, the instrument measures certain components of the electromagnetic fields set up by communication stations operating in the 15 to 30 kHz frequency range. For this survey, the Cutler, Maine (NAA - 24.0 kHz) transmitting station was utilized. When the radio waves from this station encounter conductive bodies in the ground, eddy currents are induced creating secondary fields in the area of these conductors. The EM-16 measures in-phase and quadrature-phase components of the vertical components of these secondary magnetic fields, as a percentage of the primary field of the original signal.
The resulting data was plotted in profile form at a scale of 1:2500, and accompanies this report as Map No. 1. The observed "in phase" field readings (in percent) were converted to "dip- angle" measurements and filtered by a method devised by D. C. Fraser (1969). This technique renders the data into contourable numbers. The resulting "Fraser Filtered" data is presented as Map No. 2.
DISCUSSION OF RESULTS
The survey detected two strong VLF-EM conductors and two weaker trends on the property. These are best observed on Map 2.
The strongest of the conductors extends from the south-east corner of the property (625 S, Line H) to the north-west corner (750 N, Line A), passing under Footprint Lake. It corresponds with a regional fault structure and may not be directly related to sulphide mineralization.
The most interesting anomaly extends from 175 S, Line H to 125 S, Line F where it probably continues under the north shore of Footprint Lake until it reaches the Northwest trending conductor described above, near the beaverdam at 150 to 200 S, Line D. This east-west trending feature may represent the favourable type of structure that hosts the local Copper mineralization. It should be carefully prospected.
Two other east-west trending features are noteworthy. One of these extends from 475 N, Line A to 375 N, Line E. A copper occurrence shown on ODM Map 2331 (Chandler, 1976) appears to be located near the east end of this very weak conductor.
6
A parallel and similarly weak conductor extends from 275 N, Line A to 575 S, Line D. This feature is locally enhanced by swamp, but should be prospected and sampled if possible.
CONCLUSIONS AND RECOMMENDATIONS
The VLF-EM survey on the Footprint Lake Property has detected three conductors that warrant follow-up work. Because the existing grid is of a reconnaissance nature, it is suggested that a detailed grid (50 metre spaced lines) be established over the anomalous zones . This should be controlled with east-west base-lines .
Work on the detailed grid should consist of prospecting, rock sampling, geological mapping, VLF-EM and magnetometer surveys. Trenching and diamond drilling would be contingent upon favourable results.
It is anticipated that such a program would cost as follows:
PHASE l
LINECUTTING (10 km @ S 320/km) . . . .GEOPHYSICAL SURVEYS (Mag fi VLF-EM)
10 km @ S 180/km . . . . . . . . .GEOLOGICAL MAPPING (6 Claims S 300.). PROSPECTING (20 Man-Days @ 3150) . . . ASSAYING (60 samples @ S 10.) . . . .DRAFTING AND SUMMARY REPORT . . . . .
3,200.00
1,800.001,800.003,000.00
600.001,600.00
Subtotal. . . . . . . . . S 12,000.00Contingency . . . . . . . . l,OOP.00
TOTAL PHASE I 13,000.00
A Phase II program involving drilling, stripping and assaying, would follow if results from phase I are encouraging.
July, 1991 Wawa, Ontario
Respectfully submitted.
Seymour M. Sears, B.A., B.Se,Geologist
REFERENCES
Chandler, F.W.1976 Geology of the Saunders Lake Area, District of Algoma;
Ontario Division of Mines, Geoscience Report 155, Accompanied by Map 2331, scale l" to 1/2 mile.
Fraser, B.C.1969: Contouring of VLF-EM Data in Geophysics, Vol. 34,
Pg.958-957.
Sears, S.M.1990: Report on a VLF-EM Survey Over Part of the Cheney
Copper Property, Gould Township, Sault Ste. Marie Mining Division, Ontario (Assessment Report).
Various Assessment Files of the Ontario Geological Survey, and Resident Geologist Office, Ministry of Northern Development and Mines.
STATEMENT OF QUALIFICATIONS
I, Seymour M. Sears, of Wawa, Ontario do certify that:
1. I am a consulting geologist for Sears, Barry and Associates Ltd., P. O. Box 2058, Wawa, Ontario.
2. I am a B.Se. Graduate in Geology and a B.A. Graduatein Psychology from Mount Allison University, Sackville, New Brunswick.
3. I have been practicing my profession continuously since 1972.
4. I am a Fellow of the Geological Association of Canada.
Respectfully submitted,
22 Caverhill Street P.O. Box 2058 Wawa, Ontario POS 1KO July, 1991
Seymour M. Sears, B. A., B. Se Geologist
TOWNSHIP
Blue HeavLa li f ———
, y !S:r^n, -04 - h-\M IX
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41J11SW0033 OP91-638 GOULD
RECEIVED© Ministry of Natural Resources
Ontario
Ministry of Northern Development and Mines
L.- , 1.
BLIND
' 1990 ' ' *"
RIVER
INDEX TO LAND DISPOSITION
PLAN
G-3278TOWNSHIP
GOULD
M.N.R. ADMINISTRATIVE DISTRICT
BLIND RIVERMINING DIVISION
SAULT STE. MARIELAND TITLES/REGISTRY DIVISION
ALGOMA :
Scale 1:20000
1000 1000 2000Metres Metre*
1000 1000 2OOO 3000 4OOO 5OOOFeet
8000 7000 MOO SOCK) 100M
Contour Interval 10 Metres
SYMBOLSBoundary
Township. Meridian. Baseline ..
Road allowance surveyed . . shoreline
Lot/Concession; surveyed. .unsurveyed . .
Parcel; surveyed .. .... .....unsurveyed
Rigiit-of-way. road
railway . .....utility. . .
Reservation ..
Cliff, Pit, Pile ................. ...
Contour .................. ..Interpolated ........Approximate .....Depression.... ..... ..... .....
Control point (horizontal) .................................. ... A
Flooded land..... ............. .. .. . .......... ----:-"-M-r-~-:o-:
Mine head frame .................. .......................... a
Pipeline (above ground) . ... ..................... - -
Railway, single track............. ................ ————'—— —double track .................... .. . .... -abandoned............................... -
Road, highway, county, township .access .................................. .. -trail, bush ........... ....................... -
Shoreline (original) .........
Transmission line
Wooded area.......................... ........... -
DISPOSITION OF CROWN LANDSPatent
Surface 4 Mining Rights Surface Rights Only... Mining Rights Only
LeaseSurface S Mining Rignts
Surface Rights Only . .. . Mining Rights Only
Licence of Occupation
Order-in-Council.
Cancelled
Reservation
Sand S Gravel.........................
.e
.e
..H
..y
..T
.oc
. ®
.O
.0
AREAS WITHDRAWN FRCW DISPOSITION^MRO- Mining Rights OnlySRO - Surface Rights OnlyM -t- S - Mining and Surface Rights
Description
SEC 36 /SO
Order No
w 4 /re
Date Disposition
SRO
Flic
29019
SEC 36 '60 W .0/80 30/7/ftO SRO ia8iO5
F.OO: NG CN JOBAMMAGEESH.G AMCJ CHUfa ^AKES TO CONTOUR FLEVATlOM 1120'
("I SEC 56 'BO W ,/BI 8 5/BI SRO. 18850^
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON
R " " ; i v L
' - : ^ 1 ' ;; M*.
Map base and land disposition drafting by Surveys and Mapping Branch, Ministry of Natural Resources.
The disposition of land, location of lot fabric and parcel boundaries on the index was compiled for administrative purposes only.
Cbl/D01
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Q
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V J
O 01
loT ir r 111 I
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41J11SW0033 OP91-638 GOULD
f ft? o T ffi.
41J11SW0033 OP91-638 GOULD
T/t/v QF IK'o K k 6 /v220
B
H
Footprint Lake
Heel of
Footprint Lake
CI a ioi~Bounclary
KEY MAPSi dip 1-l.ilH.UflO or 1 inch In J", miles
INSTRUMENT: Geonica EM-16 OPERATOR: S. Sears
(Field Strength) \ 1 QUADRATURE \^^*
A
(Dip Angle) IN PHASEl-
\
"CROSSOVER"
SEARS, BARRY A ASSOCIATES LTD.
41J11SW0033 OP91-638 GOULD 230
U . f^EJ^JL^ER J JN7
FOOTER INT JL.AKE
GOULD TffP., ONTARIO
JPJROFIL.E DATA
SCALE 1:2500 JULY. 1991 MAP No. l
BH
00 T
825 N
P-
41J11SW0033 OP91-638 GOULD 240
3 O
Z. O
Footprint Lake
Claim Boundary
r
KEY MAPSuit- 1 I.VM.onil DI l me h In J", miles
NOTES
INSTRUMENT: Geonica EM-16 OPERATOR: S. Seara
SEARS, BARRY SL ASSOCIATES LTD.
t/.
I^AKE JPRO &ER T
GOULD TWP. , ONTARIO
SURVEY FRASER FILTERED DATA
SCALE 112500 JULY, 1991 MAP No. 2
