Ontario Geological Survey
Permanent Link to this Record:
MDI52F05SW00025
Record Name(s) | INCO North - 1982 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1991-Mar-02 |
Date Last Modified | 2022-Sep-09 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Dogpaw Lake Area
Latitude: 49° 19' 8.03" Longitude: -93° 45' 42.69"
UTM Zone: 15 Easting: 444632.69 Northing: 5463186.16 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F05SW
Point Location Description: Transfer
Location Method: Conversion from MDI
1982: Canadian Nickel Ltd. staked the claims and conducted a reconnaissance exploration program. 1983: Canadian Nickel conducted a mag and VLF geophysical survey. 1984: Canadian Nickel conducted an IP survey and drilled 5 DDH totalling 680.6 m. Canadian Nickel and Nuinsco Resources entered into a joint venture agreement. Echo Bay Mines Ltd. subsequently joined the joint venture.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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40 | 52F05SW0160 | 52F05SW0160 |
52 | 52F05SW0046 | 52F05SW0046 |
2.5559 | 52F05SE0109 | 52F05SE0109 |
63.4648 | 52F05SE0026 | 52F05SE0026 |
Province: Superior
Subprovince: Wabigoon
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Intermediate lava flow-unsubdivided | 1 | Andesite |
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Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore |
Sep 01, 2017 (C Ravnaas) - Best assay: 0.125 opt Au (3.9 g/t Au) over 3.0 m in DDH 57773.
Sep 01, 2017 (Therese Pettigrew) - The 1984 drill program by Canadian Nickel tested two IP anomalies. These were found to be caused by pervasive 1-5% pyrite associated with quartz and carbonate within an altered schist zone. No anomalous gold values were detected in the core (AFRI 52F05SE0026).
File - Resident Geologist files 52F05SE F-9
Publication Number: Date:
Author:
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Location: Kenora RGP office
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