Ontario Geological Survey
Permanent Link to this Record:
MDI42C02SE00011
Record Name(s) | Holdsworth Prospect - 1933, Soocana-Holdsworth Gold - 1933 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect Without Reported Reserves or Resources |
Date Created | 1982-Nov-09 |
Date Last Modified | 2022-Sep-27 |
Created By | |
Revised By |
Primary Commodities: Gold, Silver
Township or Area: Corbiere
Latitude: 48° 6' 33.14" Longitude: -84° 35' 2.7"
UTM Zone: 16 Easting: 679830.26 Northing: 5331261.25 UTM Datum: NAD83
Resident Geologist District: Sault Ste. Marie
NTS Grid: 42C02SE
Point Location Description: Old open cut on north side of Pokorney Lake
Location Method: Conversion from MDI
Access Description: The property is accessible by driving north, through the community of Hawk Junction for a distance of approximately 1.5 km past the village limits. From there the property can be accessed either by traversing the railway tracks for a distance of approximately 4 km or by a bush traverse for a distance of approximately 3 km. The occurrence is located on the north side of Pokorney Lake.
The occurrence was discovered by John Holdsworth in 1933. Prospected for gold by Holdsworth in 19333-34. Property taken over by Soocana Mining Company Limited in 1933. Six diamond drill holes completed in 1933, 5-ton test mill set up, open cut made in more promising section of the vein. A sixty-ton bulk sample was extracted from the vein. The property by sampled by a succession of companies from 1935-1940. They included Falconbridge Nickle Company Limited,Erie Canadian Mines Limited, Compass Gold Mines Limited and Sylvanite Gold Mines Limited. In 1982 the property was optioned by Falconbridge and they completed an airborne geophysical survey over the property in 1983. The company also completed ground geophysical surveys, geological mapping and drilled 3 diamond drill holes (295 m).
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
CORBIERE 0016 | 42C02NE8867 | 42C02NE8867 |
Corbiere-0015 | 42C02SE0727 | 42C02SE0727 |
Corbiere-0031 | 42C02NE8836 | 42C02NE8836 |
Corbiere-0020-A1 | 42C02SE8869 | 42C02SE8869 |
Corbiere-0032 | 42C02SE0301 | 42C02SE0301 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Michipicoten
Tectonic Assemblage: Wawa
Geological Age: Neoarchean Geochronological Age: 2750 MA Geochron. Age Ref.: OFR 5888
Dec 07, 2005 (A Wilson) - The quartz vein is hosted by mafic metavolcanic rocks of the Wawa Assemblage. In the vicinity of the occurrence the mafic metavolcanics have been sheared to a chloritic schist. The vein contact is locally hosted by sericitic schist. The vein occupies a ductile shear zone which may display monor left lateral offset across a NW-grending transverse fault. This fault zone is now occupied by a diabase dike. Drag along this fault may account for the thickening of the vein. The vein appears to occur at the contact between mafic and intermediate metavolcanics.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Host |
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Schist-Unsubdivided | 2 | Chlorite | Hanging Wall | |
Intermediate Schist | 3 | Sericitic Schist | Footwall |
Dec 07, 2005 (A Wilson) - The vein consists of milky quartz with minor carbonate and sulphide mineralization. Near the old mill site where the open cut was constructed, disseminated pyrite and chalcopyrite are present in the vein. The host rock is a mafic intrusion that has been locally sheared to a chlorite schist. Chlorite clots up to 1.5 mm in some areas may be former mafic phenocrysts now completely altered to chlorite. The vein width varies from location to location, and the vein is reported to be traceable for 213 m.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue | ||||
3 | Pyrrhotite | Economic | Gangue | ||||
4 | Tourmaline | Economic | Gangue |
Dec 07, 2005 (A Wilson) - Gold values are extremely erratic within the vein, however, the best gold values are reported to occur in association with chalcopyrite. Pyrite mineralization is not an apparent indicator for gold. Grab samples by the Ontario Geological Survey from the occurrence range from trace Au to 0.55 oz/t Au from a milky quartz vein with traces of cp and py to 3.28 oz/t Au from a milky quartz vein with 1% cp and visible gold. Gold values have been described as erratic, but interesting.
Rank | Classification |
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1 | Unknown |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Regular | 213 | 285 | 75 |
Year | Tonnes | Commodities | Reference | Comment |
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1933 | 60 |
Silver 5 Gold 10 |
OFR 5587, P.282 | TOTAL PRODUCTION 10 OZ AU, 5 OZ AG |
Map - Michipicoten area, compilation sheet, District of Algoma
Publication Number: P0184 Scale: 1:126,720 Date: 1997
Author: Goodwin A.M.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geological series, Precambrian geology, Corbiere Township, Algoma District
Publication Number: P2607 Scale: 1:15,840 Date: 1984
Author: Sage R.P., Calvert T., Epstein R., England D., Koscinsko K., Worona R., Oudkerk G., Inasi J., Lockwood M.B., Thomas D.
Publisher Name: Ontario Geological Survey
Location:
Folio - Corbiere Township, District of Algoma
Publication Number: GDIF297 Date: 1997
Author: Sault Ste Marie RGO
Publisher Name: Ontario Geological Survey
Location:
Part - The Michipicoten-Missinaibi area
Publication Number: ARV44-08.001 Page: 17-18 Date: 1997
Author: Burwash E.M.
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: 23 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Mono - Wawa mineral deposits data base
Publication Number: OFR5775 Page: 46 Date: 1991
Author: Frey E.D., Stewart R.C.
Publisher Name: Ontario Geological Survey
Location:
Book - ROBINSON,D.,1983,UNPUB RPT P25 WRGO
Publication Number: N/A Date: 1996
Author:
Publisher Name:
Location:
MonoMap - Geology of Abotossaway, Corbiere, Leclaire and Musquash Townships and Part of Dunphy Township, District of Algoma
Publication Number: OFR5587 Page: 281-284 Date: 1993
Author: Sage R.P.
Publisher Name: Ontario Geological Survey
Location:
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