Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42L11NW00007

Record: MDI42L11NW00007

General

Mineral Record Identification
Record Name(s) Stewart Lake Iron Mines DDH 61-8 - 1961, Skibi Lake Iron Occurrences - 1970, Stewart Lake - 1961, Panther Mining Company Ltd. Property - 1957
Related Record Type Partial
Related Record(s)
Record Status Prospect
Date Created 1991-Jan-23
Date Last Modified 2022-Jul-20
Created By
Revised By

Commodities

Primary Commodities: Iron



Location

Township or Area: Stewart Lake Area

Latitude: 50° 42' 52.8"    Longitude: -87° 19' 20.19"

UTM Zone: 16    Easting: 477247.61   Northing: 5618145.13    UTM Datum: NAD83

Resident Geologist District: Thunder Bay North

NTS Grid: 42L11NW

Point Location Description: drill collar for DDH 68-1

Location Method: Data Compilation

Access Description:



Exploration History

1957-58: Panther Mining Company Limited – airborne geophysics, DD-4-1850 ft. 1959-61: Stewart Lake Iron Mines – DD-1-603 ft, bulk sample


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
19 42L11NW0013 42L11NW0013
20 42L11NW0003 42L11NW0003

Geology

Province: Superior

Subprovince: English River

Terrane: English River Basins

Belt: Melchett Lake

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Ironstone-unsubdivided 1 Is
Claystone 2 Argillite Adjacent
Gneiss-Unsubdivided 3 Biotite

Lithology Comments

Aug 15, 2014 (A Wilson) - The Stewart Lake-Skibi Lake occurrences consist of two bands of iron formation, the main one which extends approximately 31 miles from east of Tennant Lake to the Little Current River on the east. The second band is found only in the Melchett Lake area - it extends over a strike length of about 8 miles. The two bands are separated by about 2,000 feet of biotite quartz- feldspar schist (metagreywacke). The older, smaller band consists of "cyclic layers of magnetite, schist, and often quartz". The major unit has a basal band of iron formation separated from an upper, higher grade band by 50-150 feet of biotite-quartz-feldspar schist. The iron formation bands themselves vary from 100 to 400 feet thick in the Melchett Lake area. They are coarsely to finely layered, oxide-facies iron formation with magnetite-rich beds up to 12-18 inches thick and quartzite or cherty interbeds up to 8 to 10 inches thick where observed. As one proceeds eastwards along strike, the two bands of iron formation grade from oxide facies to sulphide facies.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1HematiteEconomicOre
2MagnetiteEconomicOre

Mineralization Comments

Aug 15, 2014 (A Wilson) - Hematite is more abundant, and the magnetite-hematite ratio of 2:1 The iron formation is bounded by sedimentary rocks. Pegmatites are not abundant. The formation is relatively continuous, but as a series of lenses connected by thinner bands. Mill testing of a 500 lb sample returned a concentrate averaging 62-64% Fe, 7% SiO2



Mineral Record Details

Characteristics
Rank Characteristic            
1 Concordant
2 Layered
Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
Skibi Lake Iron Occurrences 1961 Possible 47640000 MP042 p. 56 to a depth of 1000 ft, 47,640,000 tons possible reserves Iron 30 Percent
Skibi Lake Iron Occurrences 1959 Probable 19780000 MP042 p. 56 to a depth of 1000 ft,19,780,000 t probable, 21,780,000 possible reserves Iron 30 Percent

References

Mono - Operation Fort Hope

Publication Number: MP042 Page: 22, 55-56  Date: 1970

Author: Thurston P.C., Carter M.W.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Map - Compilation series, Ogoki Lake sheet, Thunder Bay and Cochrane districts

Publication Number: P0274 Scale: 1:126,720    Date: 1997

Author: Stott G.M., McConnell C.D., Mason J.K.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office