Ontario Geological Survey
Permanent Link to this Record:
MDI000000002049
Record Name(s) | Saturday Night - 2016 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2017-Jan-24 |
Date Last Modified | 2023-Oct-06 |
Created By | |
Revised By |
Primary Commodities: Platinum, Palladium
Secondary Commodities: Copper, Gold
Township or Area: Fowler
Latitude: 48° 38' 26.42" Longitude: -89° 26' 41.39"
UTM Zone: 16 Easting: 319903 Northing: 5390397 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52A11
Point Location Description: DDH SN-16-001 location from Assessment report 20000013542
Location Method: Data Compilation
Access Description: The prospect is accessible via the Gibride Road, off Highway 591. The road is well travelled as they are access to the many cabins lining One Island Lake.
1995: A. Josephson carried out prospecting and sampling. 2015: Transitions Metals staked claims over the target area. 2016: Transition conducted ground magnetic surveys, prospecting, and drilled 1 DDH totalling 601 m. 2018: Transition Metals conducted a ground-based magnetotelluric survey.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.57675 | 20000013542 | 20000013542 |
43467 | 20000019142 | 20000019142 |
W9540-00309 | 52A11NW0001 | 52A11NW0001 |
Province: Superior
Subprovince: Quetico
Terrane: Quetico Basin
Geological Age: Archean
Apr 08, 2022 (Therese Pettigrew) - The Saturday Night Project is located within the Quetico Basin of the Superior Province in Ontario and along the periphery of the Proterozoic Midcontinent Rift (MCR). Rocks of the Quetico Basin, also referred to as the Quetico Subprovince, form a 1000 km, east-west trending belt that averages 70 km in width stretching from Minnesota to Quebec (Williams, 1991; Stott et al. 2010). The basin is bounded to the north by the West Wabigoon, Marmion and East Wabigoon Terranes and to the south by the Wawa Terrane (Percival, 2007). Within the Quetico Basin, turbiditic metasedimentary rocks are dominant with minor iron formation, felsic intrusions, and mafic-ultramafic intrusions (Williams, 1991). These rocks are interpreted to have formed as an accretionary prism between the converging Wabigoon and Wawa Terranes (Percival, 1988). Subsequent tectonism and felsic plutonism resulted in the formation of migmatites, gneisses, and numerous suites of felsic intrusives including tonalites, granodiorites, granites, and peraluminous granites (Williams, 1991). The Midcontinent Rift (MCR) is one of the world’s largest flood basalt provinces, extending nearly 2500 km from Kansas in the southwest, arcing underneath Lake Superior and terminating at the Grenville Front in Michigan (Cannon, 1992). It is remotely observed as a prominent magnetic and gravity anomaly, with exposures of volcanic, sedimentary and intrusive rocks found extending from the shores of Lake Superior in Ontario, Minnesota, Wisconsin and Michigan. The vast majority of volcanic and sedimentary rocks associated with the MCR are concealed beneath Lake Superior where their thickness has been estimated at up to 30 km based on seismic reflection surveys (Cannon et al. 1989).
Rock Type | Rank | Composition | Texture | Relationship | Peridotite | 1 | Peridotite | Host |
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Gabbro | 2 | Melagabbro | Adjacent | |
Gabbro | 3 | Monzogabbro | Adjacent | |
Granitoid-Unsubdivided | 4 | Adjacent |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrrhotite | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore |
Jan 24, 2017 (Andrew Tims) - DDH SN16-001: Assays returned values of 6.25 metres @ 1.07g/t PGMs including a higher grade section of 4.0 g/t PGM, 0.56% Cu over a core length of 0.30 metres.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Cobalt | Unknown | 141 | ppm | 1 | ||
Copper | Unknown | 5570 | ppm | 1 | ||
Gold | Unknown | .33 | ppm | .001 | ||
Nickel | Unknown | 1875 | ppm | 1 | ||
Palladium | Unknown | 1.46 | ppm | .001 | ||
Platinum | Unknown | 2.21 | ppm | .005 |
Rank | Classification |
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1 | Mafic-Ultramafic Intrusion |
Rank | Characteristic |
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1 | Disseminated |
Map - Geological series, Quaternary geology, Onion Lake-Sunshine area, District of Thunder Bay
Publication Number: P2203 Scale: 1:50,000 Date: 1980
Author: Burwasser G.J., Ferguson A.J.
Publisher Name: Ontario Geological Survey
Location:
Thesis - The Petrology, Mineralization and Regional Context of the Thunder Mafic to Ultramafic Intrusion, Midcontinent Rift, Thunder Bay, Ontario
Publication Number: MSc Thesis Date: 2014
Author: Trevisan, B. E.
Publisher Name: Lakehead University
Location: Thunder Bay RGP
Data - Lithogeochemistry of the Dog Lake Granite Chain, Northwestern Ontario
Publication Number: MRD295 Date: 2012
Author: Kuzmich B., Hollings P., Campbell D.A.
Publisher Name: Ontario Geological Survey
Location:
Compend - Summary of Field Work and Other Activities, 2011
Publication Number: OFR6270 Date: 2011
Author: Easton R.M., Burnham O.M., Berger B.R., Beakhouse G.P., Bajc A.F., Parker J.R., Kelly R.I., Debicki E.J.
Publisher Name: Ontario Geological Survey
Location:
Thesis - Geochemistry and petrology of the Dog Lake Granite Chain, Quetico Basin, Northwestern Ontario: 136 p. thesis, Thunder Bay, ON
Publication Number: BSc Thesis Date: 2012
Author: Kuzmich, B.
Publisher Name: Lakehead University
Location: Thunder Bay RGP
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