Ontario Geological Survey
Permanent Link to this Record:
MDI52J02SE00047
Record Name(s) | Coveney Island - 1955, New Santiago #2 - 1955 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1995-May-26 |
Date Last Modified | 2023-Jun-09 |
Created By | |
Revised By |
Primary Commodities: Thorium, Uranium
Secondary Commodities: Cerium, Lanthanum, Niobium, Rare Earth Elements
Township or Area: Squash Lake Area
Latitude: 50° 0' 18.17" Longitude: -90° 43' 46.35"
UTM Zone: 15 Easting: 662692.78 Northing: 5541662.05 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52J02SE
Point Location Description: Precise
Location Method: Conversion from MDI
1955: property optioned by New Santiago Mines Ltd. OGS field party dug pits and collected samples. 1964: OGS staff collected samples. 1970: Amax Exploration Inc. carried out a magnetometer survey.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.336 | 52J02SE8769 | 52J02SE8769 |
Province: Superior
Subprovince: Wabigoon
Belt: Sturgeon Lake
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Syenite | 1 | Host |
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Mafic lava flow-unsubdivided | 2 | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Fluorite | Economic | Ore | ||||
2 | Magnetite | Economic | Ore | ||||
1 | Feldspar | Economic | Gangue | ||||
2 | Carbonate | Economic | Gangue |
Apr 29, 2020 (Therese Pettigrew) - An occurrence of higher radioactivity was located on the southwest tip of Coveney Island, Sturgeon Lake. It occurs on the contact zone between the Sturgeon Lake syenite and the altered volcanic country rock. A small pit, 4-5 feet across and about 6 feet deep, has been sunk on a radioactive, highly altered, red-coloured contact phase of the syenite. This is a red feldspar rock containing purple fluorite, minor magnetite, traces of sulphides and an unidentified black mineral. Abundant secondary carbonate occurs in both the volcanic rocks and the syenite. Qualitative spectrographic analysis of a grab sample taken by the author from this pit gave: about 0.05 percent niobium; detectable amounts of thorium, cerium, and lanthanum; and 0.06 percent U3O8 equivalent (Rogers 1964). Four radioactive dykes were located on Coveney Island. The best assays were 0.15% U3O8 and 0.48% ThO2 (radiometric equivalent) and 0.015-0.020% Nb2O5 (radiometric equivalent) (Robertson and Gould, 1983).
Map - Sioux Lookout-Armstrong sheet, geological compilation series, Kenora and Thunder Bay districts
Publication Number: M2169 Scale: 1:253,440 Date: 1970
Author: Davies J.C., Pryslak A.P., Pye E.G.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Metionga Lake area, districts of Thunder Bay and Kenora
Publication Number: R024 Page: 44 Date: 1997
Author: Rogers D.P.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Uranium and thorium deposits of northern Ontario
Publication Number: MDC025 Page: 126-127 Date: 1984
Author: Robertson J.A., Gould K.L.
Publisher Name: Ontario Geological Survey
Location:
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