Ontario Geological Survey
Permanent Link to this Record:
MDI42F15NW00004
Record Name(s) | Savoff Claim Group - 1980, Fatima Mining Company Property - 1956 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1980-Aug-12 |
Date Last Modified | 2022-Nov-02 |
Created By | |
Revised By |
Primary Commodities: Iron
Township or Area: Shuel
Latitude: 49° 56' 13.44" Longitude: -84° 58' 4.58"
UTM Zone: 16 Easting: 645816.57 Northing: 5533613.1 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42F15NW
Point Location Description: Fe triangle symbol on P0552
Location Method: Data Compilation
Access Description: Former rail flagstop of Savoff Station in the northern part of Shuel Township was near the center of the initial discovery claimblock. Savoff is on the former Hearst - Nakina line of the Can. National railway, 63 miles west of Hearst. Road access via 19 mile dirt road off Highway 11 at point 70 miles west of Heast, running northeasterly to the railroad at a point approximately 2 miles west of the showing. (AF T-368).
circa 1932-1955: minor trenching; dip-needle surveys; reconnaissance survey. 1956-57: Fatima Mining Co. Ltd. - Drilling, trenching, airborne geophysical surveys (unfiled); ground mag and VLEM surveys. 1991: McKinnon Prospecting Ltd.- Airborne mag and VLFEM survey.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-0368 | 42F15NW0003 | 42F15NW0003 |
T-3179/2.14246 | 42K01SE0001 | 42K01SE0001 |
T-0371 | 42F15NW0010 | 42F15NW0010 |
Province: Superior
Subprovince: Quetico
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Is |
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Paragneiss | 2 | Hornblende-Biotite | Near | |
Claystone | 3 | Argillite | Adjacent |
Apr 01, 2014 (D Draper) - Two parallel zones of iron formation 1.2 km apart and traced for 4.8km with a strike of 060 deg az, and steeply dipping to the south. North Zone 60 - 122m wide; South Zone 244 - 305m wide. Iron formation is interbedded with Archean greywacke, phyllite, quartzite and graphitic phyllite. North Zone consists of pyrite and pyrrhotite with some magnetite in greywacke and quartzite; South Zone contains magnetite-hematite-jasper rich sections in argillite and greywacke.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Magnetite | Economic | Ore | ||||
2 | Hematite | Economic | Ore | ||||
1 | Jasper | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue | ||||
3 | Pyrrhotite | Economic | Gangue |
Apr 01, 2014 (D Draper) - Magnetite-rich zones were cut by early drilling. Visual estimates of the percentage were given in the logs. Best zones noted: DH 1, 275 - 460ft, 37.6% ; DH 2, 125 - 473ft, 33.2%; DH 3, 425 - 575ft, 54%.
Rank | Characteristic |
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1 | Stratiform |
Book - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Page: 4 Date: 1985
Author: Rose, D.G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
File - Resident Geologist files T-0368, T-0370, T-4273
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Pagwa River-Calstock sheet, districts of Cochrane and Algoma, geological compilation series
Publication Number: P0552 Scale: 1:126,720 Date: 1997
Author: Innes D.G.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Iron deposits of Ontario
Publication Number: MDC011 Page: 128 Date: 1968
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
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