Ontario Geological Survey
Permanent Link to this Record:
MDI31M05SE00132
Record Name(s) | T.J. Newton - 1968, Quebec Metallurgical Industries Ltd. - 1953, Newton Limit Syndicate - 1927 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect Without Reported Reserves or Resources |
Date Created | 1980-Sep-19 |
Date Last Modified | 2022-Mar-02 |
Created By | |
Revised By |
Primary Commodities: Silver, Cobalt
Township or Area: Gillies Limit
Latitude: 47° 20' 52.47" Longitude: -79° 42' 36.82"
UTM Zone: 17 Easting: 597416.62 Northing: 5244633.5 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 31M05SE
Point Location Description: Claim C.1023 Block 3, 4, 9
Location Method: Data Compilation
1927: Newton Limit Syndicate –a shaft was put down 156 ft. with cross-cuts driven 40’ SE, 30’E and 30”W at the 150 level. 1953-1956: Quebec Metallurgical Industries Ltd.- DD-9; shaft dewatered to a depth of 50’ and a crosscut was driven 37’ southwest; 1956: shaft dewatered to a depth of 50 ft. 1972: Teck Mining Group Ltd. (Silverfields Division) – DD-9-4059 ft, assays. C. Camsell: DD-3-208’. Adjacent Occurrence: 95m north, 55m west of shaft; 410 g/t Ag/0.30m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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63A.392 | 31M05SE0085 | 31M05SE0085 |
Province: Southern
Subprovince: Cobalt Basin
Supergroup: Huronian Supergroup
Formation Group: Cobalt Group
Geological Age: Paleoproterozoic
Rock Type | Rank | Composition | Texture | Relationship | Intermediate lava flow-unsubdivided | 1 | Host |
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Conglomerate | 2 | Host | ||
Vein | 3 | Footwall |
Aug 11, 2017 (A Wilson) - Steeply dipping Keewatin pillowed andesite strikes northwest and faces southwest. A northwest striking schistosity occurs in the Keewatin rocks.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Silver | Economic | Ore |
Aug 11, 2017 (A Wilson) - In a 20-foot pit about 250 feet northeastward of the shaft is another vein which has an attitude similar to the one in the shaft. The shaft vein (strike northwest, dip nearly vertical) traverses Keewatin rocks with similar attitude; it has been traced by trenches for about 100 feet southeasterly from the shaft. At surface this vein is up to 7 inches wide; in a gangue of quartz and calcite cobalt mineralization occurs in small amount. Bert Page, present when the work was being done, states that the vein left the shaft at a depth not precisely known but believed to be at about 50 feet; at about this depth the writer saw during a brief examination in 1956 cobalt mineralization in a ¼ inch veinlet. Cobalt mineralization was said to have occurred at greater depth in the shaft but no information is available on the grade or attitude of the veins in which it was contained. Much of the drilling by Quebec Metallurgical Industries Ltd. was to test the vein at less than 50 feet from surface and in the vicinity of the shaft. The shaft is reported to be 156 feet deep and cross-cuts 40 feet northeast, 40 feet southwest, 30 feet east (?) and 30 feet west (?) were driven on the 150-foot level. At about 50 feet below the collar a crosscut, made in 1956, goes about 22 feet southerly from the northwest shaft compartment and then 15 feet in an easterly direction. In a 20-foot pit about 250 feet northeastward of the shaft is another vein which has an attitude similar to the one in the shaft. The shaft vein is 200 ‘long, 7 “ wide and strikes northwest. A second vein occurs northeast of the shaft vein and parallel to it.
Rank | Classification |
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1 | Vein (Cobalt-Type) |
Mono - Silver cobalt calcite vein deposits of Ontario
Publication Number: MDC010 Page: 274-275, 295 Date: 1968
Author: Sergiades A.O.
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 Date: 1998
Author: Thomson R.
Publisher Name: Ontario Dept. of Mines
Location:
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