Ontario Geological Survey
Permanent Link to this Record:
MDI52K13NE00002
Record Name(s) | Eros Red Lake Gold Mines Ltd. - 1987 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1997-Jan-24 |
Date Last Modified | 2022-May-06 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Byshe
Latitude: 51° 0' 39.19" Longitude: -93° 37' 33.48"
UTM Zone: 15 Easting: 456086.592 Northing: 5651221.842 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52K13NE
Point Location Description: approximate
Location Method: Data Compilation
Eros Red Lake was incorporated in 1953 to acquire the property. 1959: Trenching and seven drill holes totalling 1835 m.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Amphibolite
Dec 07, 2005 (K R Kettles) - GEOLOGICAL DESCRIPTION: The prospect is underlain by units of massive and pillowed basalt and mafic to intermediate tuff units. Thin quartz porphyry dykes intrude the sequence. The metavolcanic units are foliated at approximately N70deg.W and dip 45 deg. to 70 deg. to the southwest. Thin oxide facies iron formation units have been recognized in drill core to the northeast of the auriferous zones. DEPOSIT DESCRIPTION: Three drill holes intersected what appear to be at least 3 parallel to subparallel auriferous zones. These zones are in tuff units which contain quartz-carbonate stringers.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz-Carbonate | Stringers | Host |
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Mafic lava flow-unsubdivided | 2 | Basalt | Pillowed Flows, Massive Flows | Adjacent |
Intermediate Tuff | 3 | Tuffs | Adjacent | |
Quartz-Feldspar Porphyry | 4 | Quartz Porphyry | Porphyry | Intrudes |
Oxide Ironstone | 5 | Oxide Facies | Iron Formation Units | Adjacent |
Dec 07, 2005 (K R Kettles) - The prospect is underlain by units of massive and pillowed basalt and mafic to intermediate tuff units. Thin quartz porphyry dykes intrude the sequence. The metavolcanic units are foliated at approximately N70deg.W and dip 45 deg. to 70 deg. to the southwest. Thin oxide facies iron formation units have been recognized in drill core to the northeast of the auriferous zones. Three drill holes intersected what appear to be at least 3 parallel to subparallel auriferous zones. These zones are in tuff units which contain quartz-carbonate stringers.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
3 | Arsenopyrite | Economic | Ore | ||||
4 | Pyrrhotite | Economic | Ore | ||||
5 | Chalcopyrite | Economic | Ore | ||||
6 | Molybdenite | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Carbonate | Economic | Gangue | ||||
Quartz | Alteration | Silicification | 1 | Medium |
Dec 07, 2005 (K R Kettles) - Several 1.53 m sections of drill core returned anomalous values of gold, the highest being 0.02 oz/ton (0.686 g/tonne) Au.
Dec 07, 2005 (K R Kettles) - The tuffaceous units have been moderately to strongly silicified.
File - Resident Geologist's Files, Red Lake
Publication Number: RGF 1959 Date: 1959
Author: Holbrooke, G.L.
Publisher Name:
Location: Red Lake RGP
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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