Ontario Geological Survey
Permanent Link to this Record:
MDI52N04SW00088
Record Name(s) | Commander - East Showing - 1991 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1991-Mar-11 |
Date Last Modified | 2022-Sep-27 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: McDonough
Latitude: 51° 6' 31.62" Longitude: -93° 47' 38.63"
UTM Zone: 15 Easting: 444411.675 Northing: 5662222.021 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04SW
Point Location Description: N/A
Location Method: Conversion from MDI
1936: The property was held by Dawn Red Lake Gold Mines Ltd. Some exploration work done. 1940: The property was optioned by F.M. Connell for Central Patricia Gold Mines Ltd. Prospecting and trenching completed. 1944: Staked by W. Mogridge and H. Kendrick. X-ray drilling was completed on the other claims in the group. 1946: Commander Red Lake Gold Mines was formed to prospect the group. Geological mapping and drilling were completed on adjoining claims in the group.
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 mainly by pillowed and variolitic basalts. Stratigraphic tops are to the northwest. The flows generally strike northeast-southwest and dip subvertically. Foliation is generally parallel to subparallel to the bedding. Thin interflow lenses of intermediate tuffs are present in the sequence. A large mafic to ultramafic intrusion outcrops to the south of the occurrence. DEPOSIT DESCRIPTION: Gold mineralization apparently occurs in narrow quartz cabonate stringers in mafic volcanic rocks.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz-Carbonate Stringers | Host |
---|---|---|---|---|
Mafic lava flow-unsubdivided | 2 | Flows | Pillowed And Variolitic | Adjacent |
Ultramafic-Unsubdivided | 3 | Near |
Dec 07, 2005 (K R Kettles) - The occurrence is underlain mainly by pillowed and variolitic basalts. Stratigraphic tops are to the northwest. The flows generally strike northeast-southwest and dip subvertically. Foliation is generally parallel to subparallel to the bedding. Thin interflow lenses of intermediate tuffs are present in the sequence. A large mafic to ultramafic intrusion outcrops to the south of the occurrence. Gold mineralization apparently occurs in narrow quartz cabonate stringers in mafic volcanic rocks.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Gold | Economic | Ore | ||||
1 | Quartz | Economic | Gangue |
Dec 07, 2005 (K R Kettles) - MDI1 DATA: GRADE 1946? - 4 GRAB SAMPLES: 0.05,0.05, 0.06 AND 0.02 OPT AU Gold mineralization apparently occurs in narrow quartz cabonate stringers in mafic volcanic rocks. Assays from four grab samples returned values of 0.05 oz/ton (1.714 g/tonne) Au and 0.02 oz/ton (0.686 g/tonne)Au.
File - Resident Geologist files AF RL 1947 McDonough #9
Publication Number: AF RL 1947 Date: 1947
Author: Thompson, R.
Publisher Name:
Location: Red Lake RGP
Part - Geology and mineral deposits of the Red Lake area
Publication Number: ARV49-02 Page: 100-101 Date: 1998
Author: Horwood H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 562-563 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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