Ontario Geological Survey
Permanent Link to this Record:
MDI000000000285
Record Name(s) | Aoi 3 - 1986 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2007-Mar-30 |
Date Last Modified | 2022-Jun-08 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Stoughton Lake Area
Latitude: 51° 34' 31.35" Longitude: -91° 35' 34.82"
UTM Zone: 15 Easting: 597499.997 Northing: 5714750.002 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52O12SE
Point Location Description: Assessment file map (Weidner 1987).
Location Method: Data Compilation
1960: Diamond drilling by Castlebar Silver & Cobalt Mines in the area between Lang Lake and Saddle Lake. 1968-1972: Bochawna Copper Mines Ltd. and the Hanna Mining Company conducted an extensive exploration program in the area north of Lang Lake, including a diamond drilling program that outlined a copper deposit. 1969-1971: The Algoma Steel Corporation Ltd. conducted extensive diamond drilling and geophysics in northwest of Lang Lake for iron ore. 1969-1970: Card Lake Copper Mines Limited conducted grid mapping geophysics and diamond drilling for gold and base metals in the Saddle Lake, Boyes Lake, Card-Cannon Lakes, and Heinz Lake areas. 1970: Mextor Mineral Ltd. and Kennco Exploration Limited conducted geophysics and diamond drilling for base metals in the Saddle Lake area. 1984-1986: Duration Mines conducted geophysics, grid mapping and diamond drilling on the southern arm of the Lang Lake greenstone belt for base metals mineralization. 1985-1986: Geological, geochemical and geophysical surveys in the western Lang Lake area by Utah Mines. 1991-1992: Noranda Exploration Company Limited conducted grid mapping, geophysics and diamond drilling for base metals in the Lang Lake and Saddle Lake areas. 2003-2007: East-West Resource Corporation conducted geological and geophysical surveys and diamond drilling of the Lang Lake copper deposit.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.11008 | 52O12NE0001 | 52O12NE0001 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Lang Lake
Geological Age: Neoarchean
Mar 30, 2007 (Mark Puumala) - The area geology is described in MDI52O12SE00012.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Host |
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Intermediate Tuff | 2 | Tuff | Contains | |
Intermediate lava flow-unsubdivided | 3 | Intercalated Flows And Tuffs | Near | |
Anorthosite | 4 | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
Carbonate | Alteration | Carbonatization | 1 | ||||
Fuchsite | Alteration | 2 |
Mar 30, 2007 (Mark Puumala) - This occurrence is found within a quartz vein hosted within intermediate tuff (Weidner 1987). The rocks in the immediate area of the occurrence are indicated to be dominated by intercalated mafic to intermediate metavolcanic flows and tuffs. These metavolcanics are intruded by a relatively narrow (< 3m wide) anorthosite. Foliation in the area of this occurrence is oriented approximately 110/90 (Weidner 1987). The metavolcanic/anorthosite contact is also oriented 110/90. The metavolcanics are indicated to be moderately carbonate altered, with intense fuchsite alteration and moderate quartz veining occurring in proximity to the anorthosite contact. An anomalous gold assay of 0.038 oz/ton was reported by Weidner (1987) from a grab sample of quartz vein material. Significant sulphide mineralization does not occur in the veins, with pyrite only observed rarely.
Rank | Classification |
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1 | Lode (Gold) |
Rank | Characteristic |
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1 | Vein |
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