Ontario Geological Survey
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MDI52F10NW00120
Record Name(s) | Pidgeon-Trap Lake Occurrence - 1952, Lantz-Pidgeon - 1952 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1984-Feb-27 |
Date Last Modified | 2022-Nov-04 |
Created By | |
Revised By |
Primary Commodities: Copper, Gold, Cobalt, Silver
Secondary Commodities: Nickel
Township or Area: Contact Bay Area
Latitude: 49° 39' 34.24" Longitude: -92° 45' 27.33"
UTM Zone: 15 Easting: 517495 Northing: 5500803.01 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F10NW
Point Location Description: Location of Pit 1 from AFRI 52F16SE0014
Location Method: Conversion from MDI
1952: Staked by G. L. Pidgeon and A. Lantz who conducted 160 ft. of trenching, sampling, and drilled two holes. 1955: Optioned to Preston East Dome Mines Limited who conducted 1300 ft. of diamond drilling in 3 DDH, and chip sampling. 1986: Staked by J. Harrison. 1988: Bond Gold Canada conducted magnetometer and VLFEM surveys. 1992: B. Barton conducted prospecting and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.11598 | 52F10NW0064 | 52F10NW0064 |
OP92-258 | 52F16SE0014 | 52F16SE0014 |
2.14872 | 52F10NW8400 | 52F10NW8400 |
2.10659 | 52F10NW0067 | 52F10NW0067 |
Province: Superior
Subprovince: Wabigoon
Geological Age: Archean
Apr 15, 2010 (J Bongfelt) - The occurrence is situated within dioritic rocks of the Atikwa Batholith approximately 600 m south of its contact with mafic metavolcanics of the Eagle Lake Volcanics. The batholith is intruded by a wide west-northwest-trending diabase dike immediately north of the occurrence. (OFR 5723, Pidgeon-Trap Lake Occurrence, pg. 274)
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Host |
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Diorite | 2 | Diorite | Adjacent |
Apr 15, 2010 (J Bongfelt) - A deep test pit has been sunk on a 1.5 m to 1.8 m wide quartz vein striking 142º/ 82º SW within fine-grained, massive, gray, quartz-hornblende diorite. The diorite is relatively unaltered with very weak carbonatization and sericitization, and strong chloritization, in proximity to the quartz vein, with epidote along hairline fractures. The wall rocks next to the vein contain ? 1% disseminated pyrite and chalcopyrite. The diorite contains abundant small [<1 mm] elliptical, blue quartz "eyes" which may be a cataclastic texture. The quartz vein consists of white and gray quartz containing xenoliths of dark green chlorite and large, abundant, massive, "blobs" of pyrite and chalcopyrite with malachite and azurite. Narrow quartz veins occur sub-parallel to the main vein. The diorite is not pervasively sheared but hosts sub-parallel, narrow, shears generally striking 120º-140º and dipping steeply southwest. Quartz veins are controlled by tension fractures. Some veins appear to have shallow dips and variable strikes but exposure was too poor to determine their orientations. (OFR 5723, Pidgeon-Trap Lake Occurrence, pg. 274)
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore | ||||
3 | Malachite | Economic | Ore | ||||
4 | Azurite | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
Chlorite | Alteration | Chloritic | 1 | Strong | Massive | ||
Carbonate | Alteration | Carbonatization | 2 | Weak | Disseminated | ||
Sericite | Alteration | Sericitization | 3 | Weak | Disseminated |
Apr 15, 2010 (J Bongfelt) - An average of three channel samples, taken by G. L. Pidgeon and A. Lantz, assayed 0.11 ounce gold per ton, 1.02 ounces silver per ton, and 2.31% copper across an average width of 4 ft. Assays up to 0.08% nickel and 0.05% cobalt were also obtained. Another chip sample assayed 0.03 ounce gold per ton, 0.57 ounce silver per ton, and 3.03% copper (Thomson 1954, 1957; Shklanka 1969). Three grab samples of the sulphide-rich quartz vein, taken by the author (J.R. Parker), assayed 1355 ppb gold, 55 ppm silver, 6.9% copper, 490 ppm nickel and 92 ppm cobalt; 530 ppb gold, 30 ppm silver, 4.05% copper, 170 ppm nickel and 180 ppm cobalt; and 0.27 ounce gold per ton, 26 ppm silver, 1.78% copper, 100 ppm nickel and 234 ppm cobalt. A grab sample of the wall rock assayed 27 ppb gold and 130 ppm copper. (OFR 5723, Pidgeon-Trap Lake Occurrence, pg. 274)
Nov 23, 2017 (Therese Pettigrew) - The vein is 9 feet wide and exposed for a length of 170 feet (Shklanka, 1969). Samples from the 1992 prospecting program returned assays of 0.559-2.024 ppm Au and 25,420-42,190 ppm Cu (2.54-4.22% Cu) (AFRI 52F16SE0014).
Rank | Classification |
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1 | Vein |
Rank | Characteristic |
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1 | Sheared |
1 | Vein |
File - Resident Geologist files 52F10NW, Y-3 Pidgeon -Trap Lake
Publication Number: Date:
Author:
Publisher Name:
Location: Kenora RGP office
Map - Kenora-Fort Frances, geological compilation series, Kenora and Rainy River districts
Publication Number: M2443 Scale: 1:253,440 Date: 1981
Author: Blackburn C.E., Beard R.C., Rivett A.S.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology, gold mineralization and property visits in the area investigated by the Dryden-Ignace economic geologist, 1984-1987
Publication Number: OFR5723 Page: 274-275 Date: 1989
Author: Parker J.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Copper, nickel, lead and zinc deposits of Ontario
Publication Number: MDC012 Page: 165-166 Date: 1969
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Copper, nickel, lead and zinc deposits in Ontario (revised to February, 1957)
Publication Number: MDC002 Page: 21 Date: 1957
Author: Thomson J.E., Ferguson S.A., Johnston W.G.Q., Pye E.G., Savage W.S., Thomson R.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Copper, nickel, lead, and zinc deposits in Ontario
Publication Number: MDC001 Page: 12 Date: 1954
Author: Thomson J.E., Carlson H.D., Ferguson S.A., Pye E.G., Savage W.S.
Publisher Name: Ontario Dept. of Mines
Location:
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