Ontario Geological Survey
Permanent Link to this Record:
MDI42B02NE00002
Record Name(s) | Keevil Group 31 - 1965, Keevil DDH 65-4 - 1965 |
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Related Record Type | Simple |
Record Status | Discretionary Occurrence |
Date Created | 1999-Nov-19 |
Date Last Modified | 2022-Jan-05 |
Created By | A Wilson |
Revised By | A Wilson |
Primary Commodities: Copper
Township or Area: Carty
Latitude: 48° 7' 27.65" Longitude: -82° 36' 36.93"
UTM Zone: 17 Easting: 380172.525 Northing: 5331375.125 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42B02NE
Point Location Description: Inferred position taken from company drill plan
Location Method: Data Compilation
Access Description: Relatively easy access is possible from highway 101 via an old drill trail starting in a gravel quarry. This trail extends 600m to the south and has been kept open by wildlife.
1964: Keevil Mining Group - airborne mag and EM survey, ground mag, HLEM surveys, mapping, diamond drilling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-0871 | 42B02SE0003 | 42B02SE0003 |
T-0871 | 42B02SE0005 | 42B02SE0005 |
T-0871 | 42B02SE0002 | 42B02SE0002 |
Province: Kapuskasing Structural Zone
Geological Age: Neoarchean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Rock Type | Rank | Composition | Texture | Relationship | Gneiss-Unsubdivided | 1 | Hornblende | Host |
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Gneiss-Unsubdivided | 2 | Granitic | Adjacent |
Dec 07, 2005 (A Wilson) - THe drill holes intersected a series of hornblende and granitic gneisses. The hornblende gneisses consist of hornblende, feldspar and quartz. The granitic gneisses consist of quartz, feldspar, hornblende, biotite and garnets. There are also local pegmatitic phases. To the north along the highway, the biotite granitic gneisses have a contorted foliation, and have some biotite and hornblende rich resistates, probably derived from mafic dikes and supracrustal rocks.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Pyrite | Economic | Gangue | ||||
2 | Pyrrhotite | Economic | Gangue | ||||
3 | Chalcopyrite | Economic | Gangue |
Dec 07, 2005 (A Wilson) - Coarse-grained pyrite and some semi-massive stringers of pyrite, pyrrhotite and minor local chalcopyrite form up to 15% of a hornblende gneiss.
Rank | Classification |
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1 | Unknown |
Rank | Characteristic |
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1 | Unknown |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Unknown | 2 |
Map - Chapleau-Foleyet, geological compilation series, Algoma, Cochrane and Sudbury districts
Publication Number: M2221 Scale: 1:253,440 Date: 1976
Author: Thurston P.C., Sage R.P., Siragusa G.M.
Publisher Name: Ontario Division of Mines
MonoMap - Mineral Prospects of the Swayze Greenstone Belt (Volume 1, Parts of NTS 41 O and Volume 2, Parts of NTS 41 P, 42 A and 42 B)
Publication Number: OFR5912 Scale: Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
MonoMap - Geology of the Chapleau area, districts of Algoma, Sudbury, and Cochrane
Publication Number: R157 Scale: Date: 1977
Author: Thurston P.C., Siragusa G.M., Sage R.P.
Publisher Name: Ontario Division of Mines
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For detailed information regarding this mineral record please contact the Timmins Resident Geologist District Office