Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42B02NE00002

Record: MDI42B02NE00002

General

Mineral Record Identification
Record Name(s) Keevil Group 31 - 1965, Keevil DDH 65-4 - 1965
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

Commodities

Primary Commodities: Copper



Location

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.



Exploration History

1964: Keevil Mining Group - airborne mag and EM survey, ground mag, HLEM surveys, mapping, diamond drilling.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
T-0871 42B02SE0003 42B02SE0003
T-0871 42B02SE0005 42B02SE0005
T-0871 42B02SE0002 42B02SE0002

Geology

Province: Kapuskasing Structural Zone

Geological Age: Neoarchean  

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Gneiss-Unsubdivided 1 Hornblende Host
Gneiss-Unsubdivided 2 Granitic Adjacent

Lithology Comments

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.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicGangue
2PyrrhotiteEconomicGangue
3ChalcopyriteEconomicGangue

Mineralization Comments

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.



Mineral Record Details

Classification
RankClassification            
1 Unknown
Characteristics
Rank Characteristic            
1 Unknown

Mineral Zones - Size and Shape

Rank: 1       Structure Type: None

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 2

References

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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Ministry Contact Information

For detailed information regarding this mineral record please contact the Timmins Resident Geologist District Office