Ontario Geological Survey
Permanent Link to this Record:
MDI52NO4NE00002
Record Name(s) | C.W. Peterson -DDH #F1 - 1987 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1996-Dec-26 |
Date Last Modified | 2023-Mar-24 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Fairlie
Latitude: 51° 2' 37.24" Longitude: -94° 0' 53.17"
UTM Zone: 15 Easting: 428861.686 Northing: 5655172.071 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04NE
Point Location Description: N/A
Location Method: Data Compilation
1971: Property staked by C.W. Peterson of Red Lake. Stripping of overburden and three trenches. 1972: One diamond drill hole completed.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (K R Kettles) - Geological description: the occurrence is underlain primarily by mafic metavolcanics of basaltic composition. Pillow structures have been recognized in the area, with flow tops indicated to the north. The volcanics strike approximately E-W and dip steeply to the south. A thin 'tongue' of intermediate tuff is present to the west of the occurrence. Small lenses of chemical metasediments of chert-magnetite composition occur throughout the area. A long NE-SW trending lineament cuts across the area, and may represent a fault. The basaltic flows are cut by numerous quartz-carbonate stringers, and are locally brecciated and cemented with quartz-carbonate. Deposit description: Little information exists about the nature of the occurrence, but it is believed that the gold is located in quartz-carbonate stringers and quartz veins in basalt. The quartz-carbonate veins which occur as narrow fracture fillings and in brecciated zones. They constitute approximately 10% of the rock.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz-Carbonate Stringers | Stringers | Host |
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Mafic pillowed flow | 2 | Basalt | Pillowed | Adjacent |
Magnetite Ironstone | 3 | Chert-Magnetite | Near | |
Intermediate Tuff | 4 | Tuffs | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Gold | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Carbonate | Economic | Gangue | ||||
Quartz | Alteration | Silicification | 1 | Weak | Veins | ||
Carbonate | Alteration | Carbonatization | 2 | Weak | Veins |
Dec 07, 2005 (K R Kettles) - A grab sample taken in 1971 assayed 0.01 oz/ton (0.343 g/tonne)Au.
Dec 07, 2005 (K R Kettles) - The basalt has undergone varying amounts of silicification and carbonatization, depending on the degree to which it has fractured or brecciated.
File - Resident Geologist's Files, Red Lake
Publication Number: RGF RL Date: 1972
Author: Peterson, C.W.
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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