Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52F07NE00024

Record: MDI52F07NE00024

General

Mineral Record Identification
Record Name(s) Oxford - 1899, Robin Hood Gold Mine - 1936
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1991-Jan-22
Date Last Modified 2022-Mar-18
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Boyer Lake Area

Latitude: 49° 27' 14.08"    Longitude: -92° 44' .57"

UTM Zone: 15    Easting: 519315.241   Northing: 5477950.953    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52F07NE

Point Location Description: General

Location Method: Conversion from MDI

Access Description: The Oxford Prospect is located at the southeast corner of mining claim K.740289 (former mining location S.V. 129) in the Boyer Lake area, immediately south of Sharp Lake, northwest of the old Goldrock townsite, and approximately 2 km north of Trafalgar Bay on Upper Manitou Lake. The property is accessible by a number of overgrown trails. (OFR 5723, p. 263, 264, 1989)



Exploration History

1899: A 77 ft. shaft with 24 ft. of crosscutting was developed on mining location S.V. 129 which was part of a group of four mining locations (S.V. 128, 129, 131, and 166). 1936: Robin Hood Mining Syndicate acquired the four patented claims, as well as twelve additional claims, and conducted trenching and diamond drilling. 1983: Staked by M. Woitowicz. 1984: Transferred to St. Joe Canada Incorporated who conducted geological mapping and sampling over the shaft area. 1986: Transferred from M. Woitowicz to Falconbridge Limited. 1987: Falconbridge Ltd. dropped the option on the property. (Assessment Files, Resident Geologist's Office, Kenora). (OFR 5723, p. 263, 264, 1989)


Geology

Province: Superior

Subprovince: Wabigoon

Terrane: Western Wabigoon

Belt: Eagle-Wabigoon-Manitou

Geological Age: Precambrian  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 quartz stringers Host
Schist-Unsubdivided 2 Contains

Lithology Comments

Feb 24, 2010 (C Ravnaas) - The prospect is situated within northeast facing massive and pillowed mafic metavolcanic flows of the Pincher Lake Group, on the northwest limb of the Manitou Anticline. The Oxford Prospect is underlain by strongly sheared, sericitized, chloritic, weakly to moderately carbonatized (calcite and iron carbonate), mafic flows and intermediate tuffs containing variable amounts of fine-grained, disseminated, magnetite and pyrite. The shear zone is 30 m to 46 m wide and strikes northeast for approximately 150 m. The sheared rocks have variable strikes and dips within the main shear zone. The shear zone controls a 2.1 m wide stockwork of white quartz veins containing black tourmaline, chlorite stringers, iron carbonate, pyrite [ -cl-4%], and chalcopyrite. A 2.1 m x 3.6 m x 30 m deep shaft has been sunk on t he quartz veins, as well as four trenches southwest of the shaft. Quartz veins are 2 cm to 10 cm wide in the trenches and 0.9 m to 1.5 m wide in the shaft. Two grab samples, taken by the author, of quartz vein material and altered wall rock assayed 130 ppb gold and 185 ppb gold respectively. Grab samples taken from the dump by St. Joe Canada Incorporated, assayed consistent anomalous gold values ranging between 30 ppb gold and 795 ppb gold. Sampling at the 77 ft. level of the shaft, conducted by the Robin Hood Mining Syndicate, gave assays as high as 0.67 ounce gold per ton, and abundant visible gold was observed and panned from the vein (Assessment Files, Resident Geologist's Office, Kenora). (OFR 5723, p. 263, 264, 1989)




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
5ChalcopyriteEconomicOre
10GoldEconomicOre
15PyriteEconomicOre
20TourmalineEconomicOre

Mineralization Comments

Feb 24, 2010 (C Ravnaas) - BEST ASSAY: 0.67 OPT AU FROM 23 M DEPTH. Two grab samples, taken by the author, of quartz vein material and altered wall rock assayed 130 ppb gold and 185 ppb gold respectively. Grab samples taken from the dump by St. Joe Canada Incorporated, assayed consistent anomalous gold values ranging between 30 ppb gold and 795 ppb gold. Sampling at the 77 ft. level of the shaft, conducted by the Robin Hood Mining Syndicate, gave assays as high as 0.67 ounce gold per ton, and abundant visible gold was observed and panned from the vein (Assessment Files, Resident Geologist's Office, Kenora). (OFR 5723, p. 263, 264, 1989)



Mineral Record Details

References

Part - Mines of northwestern Ontario

Publication Number: ARV09.003 Scale:     Date: 1998

Author: Bow J.A.

Publisher Name: Ontario Bureau of Mines

Location:


Part - Statistical review of the mineral industry of Ontario for 1936

Publication Number: ARV46-01.001 Scale:     Date: 1997

Author: Young A.C.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River

Publication Number: MDC016 Scale:     Date: 1976

Author: Beard R.C., Garratt G.L.

Publisher Name: Ontario Division of Mines

Location:


Mono - Geology, gold mineralization and property visits in the area investigated by the Dryden-Ignace economic geologist, 1984-1987

Publication Number: OFR5723 Scale:     Date: 1989

Author: Parker J.R.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Kenora Resident Geologist District Office