Ontario Geological Survey
Permanent Link to this Record:
MDI000000000356
Record Name(s) | Watt and Durham - 1944 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2007-Aug-30 |
Date Last Modified | 2023-Aug-03 |
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Revised By |
Primary Commodities: Gold
Secondary Commodities: Silver
Township or Area: Setting Net Lake Area
Latitude: 52° 46' 44.52" Longitude: -93° 33' 19.81"
UTM Zone: 15 Easting: 462530 Northing: 5847835 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 53C13SE
Point Location Description: Location of sample 89123 on map in Assessment report 53C13SE0036
Location Method: Data Compilation
1944: Kega Gold Mines discovered the showing. 1956-57: Senet Copper Mines Ltd. sunk 6 shallow test pits and carried out geoliogcal mapping, sampling, resistivity, SP, EM, and magnetic ground geophysical surveys. 1969-70: Newconex Canadian Exploration Ltd. conducted ground magnetic and EM surveys. 1987: Geotest Corporation conducted prospecting and sampling. 1988: Geotest conducted airborne magnetic and VLF-EM surveys. 2014: GoldenShare conducted prospecting and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.11129 | 53C13SE0036 | 53C13SE0036 |
2.55232 | 20000008320 | 20000008320 |
53C13SE0019 | 20000004856 | 20000004856 |
63.2848 | 53C13SE0013 | 53C13SE0013 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Belt: Favourable Lake
Geological Age: Mesoarchean
Rock Type | Rank | Composition | Texture | Relationship | Felsic Tuff | 1 | Tuff | Host |
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Mafic lava flow-unsubdivided | 2 | Near | ||
Gabbro | 3 | Near | ||
Vein | 4 | Quartz | Host |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore | ||||
3 | Pyrite | Economic | Ore | ||||
4 | Pyrrhotite | Economic | Ore |
Aug 31, 2007 (Mark Puumala) - Atkinson et al. (1990) indicate that the Watt and Durham occurrence is situated within massive mafic metavolcanic flows hosting narrow units of felsic tuff intruded by a gabbro sill. The occurrence was reported by Kega Gold Mines to be hosted within a single quartz vein ranging in width from 0.9 to 9 m. Senet Copper Mines reported that the vein was strongly auriferous, and that mineralization consisted of disseminated pyrite and trace chalcopyrite. Cruickshank (1988) reported finding quartz veins of geochemical interest in the general vicinity of this showing, although not apparently locating the wide vein described above. Quartz veins a few centimeters in width, striking in a general north-south orientation, and either barren or mineralized with trace chalcopyrite, pyrite, pyrrhotite and/or arsenopyrite, were reported in this general area. Reported gold assays from these veins were quite low (<95 ppb). However, Cruickshank (1988) reported the discovery of a 5 m by 2 m patch of gossan mineralized with 5% pyrite at this location. The gossan is hosted in an outcrop of felsic tuff, and a composite grab sample of this material assayed 2.9 g/t Au, 2.9 g/t Ag and 0.1% Pb.
Jul 31, 2019 (Therese Pettigrew) - Samples collected in 2014 returned results up to 0.22 ppm Au, 2.8 ppm Ag, and 0.04% Cu (Assessment report 20000008320).
Rank | Classification |
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1 | Lode (Gold) |
Rank | Characteristic |
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1 | Disseminated |
Article - Red Lake Resident Geologist's District - 1990
Publication Number: MP152.003 Page: 43-44 Date: 1997
Author: Atkinson B.T., Parker J.R., Storey C.C.
Publisher Name: Ontario Geological Survey
Location:
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