Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31M05NE00112

Record: MDI31M05NE00112

General

Mineral Record Identification
Record Name(s) M.J. O'Brien Ltd. - 1915, The Cobalt Silver Syndicate Ltd. - 1936, Coballoy Mines and Refiners Ltd. - 1957, C.L. Murray - 1968
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1980-Sep-16
Date Last Modified 2022-Mar-02
Created By
Revised By

Commodities

Primary Commodities: Silver, Cobalt

Secondary Commodities: Lead, Copper



Location

Township or Area: Gillies Limit

Latitude: 47° 22' 44.67"    Longitude: -79° 41' 41.39"

UTM Zone: 17    Easting: 598521.64   Northing: 5248116.51    UTM Datum: NAD83

Resident Geologist District: Kirkland Lake

NTS Grid: 31M05NE

Point Location Description: Cobalt Silver Syndicate Shaft.

Location Method: Data Compilation



Exploration History

1915-1916: M.J. O’Brien: York-O’Brien shaft sunk; underground work from this shaft continued into 1916 with no ore found; 1936-37: Cobalt Silver Syndicate Ltd.: underground operations from an old shaft (Cobalt Silver Syndicate Shaft?).


Geology

Province: Southern

Subprovince: Cobalt Basin

Supergroup: Huronian Supergroup

Formation Group: Cobalt Group

Geological Age: Paleoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1 Near
Conglomerate 2 Cobalt Series Hanging Wall

Lithology Comments

Aug 08, 2017 (A Wilson) - Keewatin andesitic lava and interflow sediments occur in a synclinal fold whose axis trends and plunges west-northwest. On the north limb of the fold these rocks strike south-east and face south-west, on the south limb east-northeast and face north-northwest. In the southeast corner of the claim, Cobalt Series conglomerate faulted off by the north-northeast striking Cobalt Lake Fault; unconformably overlies the Keewatin volcanics. The York-O’Brien shaft vein strikes ENE for 200 ft. along an interflow sedimentary bed in the Keewatin rocks. Cobalt Silver Syndicate shaft vein strikes ENE 150 ft. along the same sedimentary bed in the Keewatin rocks. A third vein occurs striking northwest for 150 ft., 500 ft. southwest of the north post.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1SilverEconomicOre
3GalenaEconomicGangue

Mineralization Comments

Aug 08, 2017 (A Wilson) - Galena occurs largely as a replacement of a cherty Keewatin sedimentary band between lava flows. In addition, silver-cobalt mineralization is present in carbonate veins cutting Cobalt sedimentary rocks.



Mineral Record Details

Classification
RankClassification            
1 Vein (Cobalt-Type)

References

Map - Cobalt silver area, northern sheet, Timiskaming District

Publication Number: M2050 Scale: 1:12,000    Date: 1997

Author: Thomson R.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Silver cobalt calcite vein deposits of Ontario

Publication Number: MDC010 Scale:     Date: 1968

Author: Sergiades A.O.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Copper, nickel, lead and zinc deposits of Ontario

Publication Number: MDC012 Scale:     Date: 1969

Author: Shklanka R.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Preliminary report on parts of Coleman Township and Gillies Limit to the south and southwest of Cobalt

Publication Number: PR1960-03 Scale:     Date: 1998

Author: Thomson R.

Publisher Name: Ontario Dept. of Mines

Location:


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Ministry Contact Information

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