Ontario Geological Survey
Permanent Link to this Record:
MDI42A04NW00033
Record Name(s) | Tremblay Option - 1984, Card Lake - 1974, A.N. Wright Property - 1972, Reeves J. V. Property - 1988, R. Tremblay Property - 1984 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1992-Sep-26 |
Date Last Modified | 2022-Sep-27 |
Created By | |
Revised By |
Primary Commodities: Gold, Silver
Secondary Commodities: Copper, Lead
Township or Area: Sewell
Latitude: 48° 12' 50.94" Longitude: -81° 59' 41.01"
UTM Zone: 17 Easting: 426106.07 Northing: 5340580.85 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A04NW
Point Location Description: Southern end of the stripped area.
Location Method: Field Visit with GPS
Access Description: Access is relatively easy as secondary logging roads branching off the Kenogaming Main Haul Road pass the stripped area. However, a beaver pond covers the secondary road about half way down and an old culvert under the road bed in the beaver pond has been damaged.
1946: Kalbrook Mining - geological mapping. 1972: J. Johnson and A. Wright - mag and EM surveys, 2 ddh. 1974: Card Lake Copper - 3 ddh (290m). 1982: Gold Fields Mining Corporation - mag and VLF-EM surveys. 1983-1984: R.J. Sheppard – AEM, AMag.1984: R. Tremblay - trenching. 1986: New Texmont Mines: 5 ddh (777m). 1986: Goldrock Resources - reconnaissance mapping; mapping, mag and EM surveys. 1987: Glen Auden - mapping; magnetic surveys, sampling. 1989: American Barrick- drilling. 1996-1997: M.G. Caron – IP, Mag. 2007: F. Ross, G. Ross, G. Windsor and R.B. Durham – Str, Tr, GL. Amador Gold Corp. – Samp, Str, Anlys. 2011: Benton Resources Corp. – Assays, GL, Samp, IP, Mag
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-1519 / | 42A04NW0051 | 42A04NW0051 |
T-1519 / 2.1093 | 42A04NW0035 | 42A04NW0035 |
T-2722 / 2.10452 | 42A04NW0018 | 42A04NW0018 |
T-2722 / 2.10291 | 42A04NW0017 | 42A04NW0017 |
T-2722 / 2.11119 | 42A04NW0014 | 42A04NW0014 |
T-2722 / 2.11646 | 42A04NW0013 | 42A04NW0013 |
T-2722 / 2.12782 | 42A04NW0004 | 42A04NW0004 |
T-2799 / 2.8066 | 42B01NE0105 | 42B01NE0105 |
T-2799 / 2.6342 | 42A04NW0028 | 42A04NW0028 |
T-2971 / W8506-00302 | 42A05SW5004 | 42A05SW5004 |
T-3119 / 2.9737 | 42A04NW0021 | 42A04NW0021 |
T-3868 / 2.17497 | 42A04NW0071 | 42A04NW0071 |
T-5531 / 2.35043 | 20000002160 | 20000002160 |
T-5689 / 2.38096 | 20000003009 | 20000003009 |
T-6313 / 2.50088 | 20000006980 | 20000006980 |
T-6417 / 2.51789 | 20000007194 | 20000007194 |
T-2971 / | 42A04NW0022 | 42A04NW0022 |
T-44 / | 42A04NW0046 | 42A04NW0046 |
T-2535 / 2.4891 | 42A04NW0031 | 42A04NW0031 |
T-3119 / 2.9684 | 42B01NE8571 | 42B01NE8571 |
T-1519 / | 42A04NW0044 | 42A04NW0044 |
T-2722 / 2.11120 | 42B01NE0032 | 42B01NE0032 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Geological Age: Neoarchean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Vein | Host |
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Mafic lava flow-unsubdivided | 2 | Basalt | Near | |
Granodiorite | 3 | Near | ||
Schist-Unsubdivided | 4 | Adjacent | ||
Vein | 5 | Contains |
Dec 07, 2005 (S Fumerton) - Mineralization is hosted in a massive medium to coarse grained flow though there are reports of quartz stockworks in strongly carbonatized material in drill core. This quartz carbonate material may represent altered ultramafics.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Chalcopyrite | Economic | Ore | ||||
2 | Galena | Economic | Ore | ||||
3 | Gold | Economic | Ore | ||||
1 | Tourmaline | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue | ||||
4 | Arsenopyrite | Economic | Gangue | ||||
Chlorite | Alteration | Chloritic | 1 | Weak | Replacement | ||
Ankerite | Alteration | Carbonatization | 2 | Weak | Replacement |
Mar 15, 2016 (S Fumerton) - Parallel and undulating quartz veins spaced 2 to 3m apart cut the outcrop. These veins are between 2 and 25cm thick with well-preserved intrusive horns and are enclosed in a strongly altered iron carbonate zone. Locally several small veins, 1 to 3cm in size, are closely spaced, 10 to 30cm apart, and contained within a single alteration zone. Individual quartz veins are discontinuous within and alteration zone but do form closely spaced en echelon sets. Individual vein are up to 10m long and individual alteration zones are between 10 and 100m long. The veins are composed of coarse grained quartz with a translucent to milky appearance. Other minerals include calcite and erratic, fine grained, tourmaline concentrations which may be acicular. Pyrite is the most common sulphide but even so is sparsely disseminated in subhedral grains up to 3mm in size. Chalcopyrite and trace amounts of galena occur in some of the old trenches. The chalcopyrite is locally mantled by pyrite. The large quartz veins reported in some of the earlier work were not found though most of the reported trenches where found.
Mar 15, 2016 (A Wilson) - Grab samples collected by A. N. Wright returned values of 0.02 oz/t Au, 0.26 oz/t Ag, 0.03% Cu and 0.27% Pb from a quartz vein and 0.04 oz/t Au, 0.68 oz/t Ag, 0.05% Cu and 0.68% Pb from carbonated host rock. In 1987, Glen Auden obtained assays of 15 g/t and 3.7 g/t from the old trenches. The best grab samples obtained from the stripped area returned values of 0.37 g/t Au and 0.48 g/t Au. A sample from the muck pile from the trenches returned 4.7 g/t Au.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Gold | Unknown | .37 | ppm | |||
Gold | Unknown | .48 | ppm | |||
Gold | Unknown | 4.73 | ppm | |||
Silver | Unknown | 0 | ppm | |||
Silver | Unknown | 0 | ppm | |||
Silver | Unknown | 0 | ppm |
Rank | Classification |
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1 | Mesothermal |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 365 | 15 | 188 | 48 | N/A | N/A |
Map - Precambrian Geology, Northern Swayze Greenstone Belt
Publication Number: M2627 Scale: 1:50,000 Date: 1995
Author: Ayer J.A.
Publisher Name: Ontario Geological Survey
Location:
Publication - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Date: 1985
Author: Rose, D.G
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
MonoMap - Geology of the Kukatush-Sewell Lake area, District of Sudbury
Publication Number: R097 Date: 1972
Author: Milne V.G.
Publisher Name: Ontario Division of Mines
Location:
Compend - Report of activities, 1988, Resident Geologists
Publication Number: MP142 Page: 256 Date: 1989
Author: Fenwick K.G., Giblin P.E., Pitts A.E.
Publisher Name: Ontario Geological Survey
Location:
File - Resident Geologist files 1980, air photos
Publication Number: Date: 1996
Author:
Publisher Name:
Location:
MonoMap - Precambrian Geology, Northern Swayze Greenstone Belt
Publication Number: R297 Page: 48 Date: 1995
Author: Ayer J.A.
Publisher Name: Ontario Geological Survey
Location:
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 Page: 494-495 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
Book - Sewell Township - unpublished GDIF
Publication Number: GDIF Date: 1991
Author: Resident Geologist Staff
Publisher Name:
Location: Timmins RGP
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