Ontario Geological Survey
Permanent Link to this Record:
MDI32D12SW00221
Record Name(s) | Brydges Occurrence - 1990, Coastoro - 1990, Jonpol Explorations Ltd - 1990, Insgar Mines Ltd. - 1990, Dst Quality Control Entry - 1997 |
---|---|
Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1997-Mar-04 |
Date Last Modified | 2023-Aug-03 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Silver, Lead
Township or Area: Garrison
Latitude: 48° 30' 58.24" Longitude: -79° 55' 33.37"
UTM Zone: 17 Easting: 579317.375 Northing: 5374230.874 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 32D12SW
Point Location Description: A point located 2.38 km south and 2.86 km west of the northeast corner of Garrison Township.
Location Method: Data Compilation
Pre- 1933: The claims were prospected and/or owned by J. Otis(?) and the Tough Oaks Mining Company. 1933: The claims were restaked by J. Brydges. 1934: Brydges Gold Mines Ltd. was formed and acquired claims from J. Brydges. 1946: Insgar Mines Ltd., a company formed by Inspiration Mining and Development Co. Ltd. to explore options it held on the Brydges, Linton, and Anderson claim groups in northern Garrison Township (Satterly 1949), completed geological mapping and diamond drilled 7 holes totalling 4,668 feet. 1947: The Insgar Mines option lapsed (Satterly 1949) and the claims reverted to Brydges Gold Mines. Pre- 1985: Canadian Johns-Manville Company of Canada Ltd. diamond drilled on the claims (Clayson Brydges, pers. comm., May, 1988). 1985: As part of a geophysical survey completed for Cream Silver Mines Ltd. and Meridor Resources Ltd. of properties south of the claim group, 3 anomalous bedrock conductors were detected on the Brydges Gold Mines claims. 1986: Jonpol Explorations Ltd. completed a geophysical survey of the Brydges Gold Mines claims which was reported (The Northern Mine, May 12, 1986) to have detected what were believed to be the eastern extensions of auriferous zones that were known to occur on the contiguous Garrcon Mines Ltd. claims. 6 holes totalling 2,245 feet were diamond drilled by Jonpol Explorations (A.D. Drummond, project engineer, Jonpol Explorations Ltd., pers. comm., July 15, 1988). 1987: Coastoro Resources Ltd. (a member of the Jonpol Group of companies) acquired the right to earn a 45% interest in the Brydges Gold Mines (and Linton) claim groups (The Northern Miner, September 7, 1987). Jonpol Explorations completed 6,631 feet of diamond drilling (The Northern Miner, September 28, 1987; A.D. Drummond, project engineer, Coastoro Resources Ltd., pers. comm., July 15, 1988). 1988: As of May, Jonpol Explorations had diamond drilled 16 holes on the property. The core from 7 of these holes (totalling 2,657 m).
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
KL-0934 | 32D05NW0187 | 32D05NW0187 |
KL-1324, 63.6120 | 32D12SW0126 | 32D12SW0126 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (A Mitchell) - The Brydges Gold Mines claims straddle the (locally east striking) Porcupine-Destor Fault Zone (PDFZ) in the general area where it (or its Southern Branch in the terminology of Jensen and Langford 1985) joins the west to west northwest striking Munro/Pipestone Fault Zone (in the terminology of Jensen and Langford1985, The Middle Branch of the PDFZ). The Porcupine-Destor/Munro/Pipestone Fault Zones (or, or simply, the PDFZ) is complex, consisting of juxtaposed lithologically and structurally distinct faut/shear bounded blocks each of which may be up to several hundred metres in size which in aggregate comprise a zone up to several kilometres in width. The regional metamorphic grade in the area is greenschist or lower metamorphic facies except marginal to felsic intrusions, where narrow amphibolite grade contact metamorphic aureoles may be developed. North of the PDFZ, basement rocks are mainly moderately north dipping and north facing volcanic, volcaniclastic, and sedimentary rocks of the calc alkalic (Archean) Hunter Mine Group and younger komatiitic and tholeiitic volcanic and intrusive rocks of the (Archean) Stoughton-Roquemaure Group (Jensen and Langford 1985, Jensen 1982). South of the PDFZ, mainly northeast striking, steeply south dipping, and south facing tholeiitic basalt of the (Archean) Kinojevis Group occupies part of the north limb of the east striking and east plunging Blake River Synclinorium (Jensen and Langford 1985; Jensen 1982, 1985).
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Host |
---|---|---|---|---|
Magnetite Ironstone | 2 | Magnetite And Jasper Iron Fmn. | Complexly Folded | Adjacent |
Terrigenous-Clastic-Unsubdivided | 3 | Timiskaming Type | Clastic Sediments, (Tuffs?) | Adjacent |
Ultramafic lava flow-unsubdivided | 4 | Komatiitic Volcanics | Near | |
Mafic lava flow-unsubdivided | 5 | Thoelitic Volcanic Rocks | Near | |
Syenite | 6 | Syenite | Dikes | Near |
Diorite | 7 | Diorite | Dikes | Near |
Lamprophyre-Unsubdivided | 8 | Lamprophyre | Dikes | Near |
Dec 07, 2005 (A Mitchell) - Bedrock underlying the Brydges Gold Mines claims (as indicated by Jensen (1982) and Satterly (1949)) consists mainly of complexly folded and variably altered Timiskaming type clastic sediments, tuffs(?), carbonate, and (volumetrically minor) magnetitie ironstone and red jasper which are confined to a fault/shear bounded block which is several hundred metres in width. North and south of the sedimentary block, sheared komatiitic and tholeiitic volcanic rocks and intercalated sedimentary and tuffaceous rocks (as represented now by various talc, chlorite, serpentine, carbonate, and sericite schists)are interpreted by these workers to be in fault/shear contact with the sediments. Intrusive rocks including various syenitic dikes and sill-like bodies (many of which are reported to be variably specularitic, hematitic, and molybdenite bearing),dioritic dikes, and lamprophyre dikes have been noted within both the sediments and the bounding shears. These intrusive rocks also form a ubiquitous component of drill logs from the Brydges Gold Mines and surrounding properties. Although locally complexly folded, the regional strike of the major shear elements which form the PDFZ in this area is easterly; steep dips to the south are suggested by data in the assessment files.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Galena | Economic | Gangue | ||||
2 | Quartz | Economic | Gangue | ||||
3 | Carbonate | Economic | Gangue | ||||
4 | Magnetite | Economic | Gangue | ||||
5 | Jasper | Economic | Gangue | ||||
6 | Chlorite | Economic | Gangue | ||||
7 | Silver | Economic | Gangue | ||||
8 | Molybdenite | Economic | Gangue | ||||
9 | Pyrite | Economic | Gangue |
Dec 07, 2005 (A Mitchell) - Anomalous gold mineralization exposed in outcrop is limited (according to Satterly 1949) to two types: auriferious quartz veins and pyritic carbonate. The surface occurrences are reported (assessment files) to have been poorly exposed during 1934, and were evidently no better exposed in 1949 (Satterly 1949). Near the northwest corner of claim 25940, pits and trenches are reported by Satterly to have exposed a 340 striking 6-10 inch wide '...(feldspathic quartz vein)...' (p. 20) which contains galena; when sampled, this is reported by Satterly to have averaged 0.03 ounce of gold per ton and 2.32 ounce of silver per ton. Near the northwest corner of claim 25940 on its north boundary, a second pit is reported (Satterly 1949) to have exposed carbonate bearing 'felsitized' sediment hosting irregular quartz stringers that contain disseminated pyrite; these were reported to also contain visible gold. The Insgar Mines Ltd. diamond drilling is reported (assessment files) to have intersected anomalous (i.e. greater than 0.01 ounce of gold per ton) gold tenors in foliated and carbonatized mafic volcanic) rock associated with quartz and carbonate stringers, in pyritic syenite (with and without associated galena), in diorite, and in pyritic carbonate associated with grey carbonate stringers. Drilling by Jonpol Explorations in 1986 also intersected scattered anomalous gold tenors in pyritic (syenite) intruding variably (brecciated hematitic wake) and (carbonatized and sericitized argillite) assessment files. The sediment encountered in this diamond drilling was also noted to be variably pyritic, with occasional splashes of pyrite and chalcopyrite occupying narrow fractures.
File - Resident Geologist files KL-0298, KL-1258
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - Township of Garrison, District of Cochrane, Ontario
Publication Number: M1949-01 Scale: 1:12,000 Date: 1997
Author: Satterly J., Hogg N.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gneisses of the Parry Sound-Muskoka area: flagstone resources
Publication Number: OFR5725 Date: 1989
Author: Fouts C.R., Marmont C.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of Garrison Township
Publication Number: ARV58-04 Page: 19-20 Date: 1997
Author: Satterly J.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 127 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Folio - Garrison Township, District of Cochrane
Publication Number: GDIF360 Date: 1997
Author: Kirkland Lake RGO
Publisher Name: Ontario Geological Survey
Location:
Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file
Publication Number: OFR5467 Page: G0041 Date: 1983
Author: Hodgson C.J.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral occurrences, deposits, and mines of the Black River-Matheson area
Publication Number: OFR5735 Page: 720-727 Date: 1990
Author: Bath A.C.
Publisher Name: Ontario Geological Survey
Location:
We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.
Please review our Terms of Use agreement for this data product.
For detailed information regarding this mineral record please contact the Kirkland Lake Resident Geologist District Office