Ontario Geological Survey
Permanent Link to this Record:
MDI42A01SW00011
Record Name(s) | William Biederman - 1945, Rib Lake - 1981 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1981-Apr-21 |
Date Last Modified | 2023-Mar-09 |
Created By | |
Revised By |
Primary Commodities: Molybdenum
Township or Area: Bompas
Latitude: 48° 7' 43.78" Longitude: -80° 22' 57.71"
UTM Zone: 17 Easting: 545933.238 Northing: 5330803.254 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 42A01SW
Point Location Description: Approximate location only
Location Method: Based on Assessment
Access Description: A bush trail leads directly to the property from the Englehart Management Road in Burt Township, approximately six miles north of its junction with Highway # 66.
1971-1972: Canadian Johns-Manville CO. Limited: completed a biogeochemical survey, bedrock sampling and geological mapping over the property 1957: Kirkland Minerals Corporation Ltd: diamond drilled 2 holes totalling 170 feet 1939-1940: Greenlee Mines Ltd: considerable trenching and 500 feet of diamond drilling in 7 holes
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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KL0351, 2.1042 | 42A01NW0057 | 42A01NW0057 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
Apr 21, 2010 (D Guidon) - The veins are located in the Watabeag Batholith near the Huronian contact. The quartz veins or quartz-rich pegmatite dikes strike at 230-35. The vein or veins are exposed over about 50 feet and have a mean thickness of 8 feet. Trenching and diamond drilling along strike failed to locate the veins.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz With K-Feldspar Crystals | Pegmatitic, Poorly Developed Chloritic Foliation | Contains |
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Syenite | 2 | Horneblende-Biotite Syenite | Coarse-Grained With Pink Orthoclase Crystals | Footwall |
Syenite | 3 | Horneblende-Biotite Syenite | Coarse-Grained With Pink Orthoclase Crystals | Hanging Wall |
Granite | 4 | Micro-Granite Dyke | Fine-Grained, With Syenite Xenoliths |
Apr 21, 2010 (J Suma-Momoh) - Horneblende-biotite syenite with numerous recrystallized inclusions forms the host rock. From north to south two flat lying quartz veins are exposed at the south edge of a syenite outcrop. The mean strike of the veins is N 50° E, and dip 35° N. The hanging wall quartz vein is 2 feet wide, glassy and with no apparent mineralization. The principal quartz vein is in the footwall of the above and separated from it by 5 feet of syenite.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Molybdenite | Economic | Ore | ||||
2 | Pyrite | Economic | Gangue | ||||
3 | Chalcopyrite | Economic | Gangue |
Apr 21, 2010 (J Suma-Momoh) - Only trace amount of chalcopyrite (occurring in clusters and stringers) is present in the quartz veins. A 63 pound sample of the quartz-rich pegmatite sent to the Mines Branch, Ottawa, in 1939 assayed 0.98 % molybdenum sulphide. REF: ODM 1968, MRC # 7, page 76.
File - Resident Geologist file KL1440
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Publication - Molybdenum deposits of Canada; Geological Survey of Canada, Economic Geology Report 20
Publication Number: Econ Geol 20 Page: 85 Date: 1963
Author: Vokes, F M
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/103994
MonoMap - Geology of Bompas and Grenfell townships, District of Timiskaming
Publication Number: R030 Page: 17 Date: 1997
Author: Grant J.A.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Molybdenum deposits of Ontario
Publication Number: MDC007 Page: 76 Date: 1968
Author: Johnston F.J.
Publisher Name: Ontario Dept. of Mines
Location:
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