Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52B09SW00011

Record: MDI52B09SW00011

General

Mineral Record Identification
Record Name(s) Discovery Point - 1913, INCO Shebandowan - 1936
Related Record Type Partial
Related Record(s)
Record Status Past Producing Mine Without Reserves or Resources
Date Created 1991-Feb-27
Date Last Modified 2022-Sep-26
Created By
Revised By

Commodities

Primary Commodities: Nickel, Copper, Platinum, Palladium

Secondary Commodities: Gold, Silver, Cobalt, Chromium



Location

Township or Area: Hagey

Latitude: 48° 35' 58.2"    Longitude: -90° 16' 7.3"

UTM Zone: 15    Easting: 701361.99   Northing: 5386537.13    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 52B09SE, 52B09SW

Point Location Description: Precise

Location Method: Conversion from MDI



Exploration History

1913-14: W.W. Benner discovered nickel at Discovery Point. Test pits blasted by Cross brothers. 1927-30: Cross conducted trenching, stripping, and diamond drilling. 1936-52: Claims purchased by INCO, who carried out trenching, test-pitting, geophysical surveys, and diamond drilling. 1952-65: INCO carried out intermittent diamond drilling. 1966-67: No. 1 Shaft development commenced in 1966 and was completed in 1967. Underground diamond drilling conducted on 305 m level. Mag and EM geophysical surveys were performed. 1968: No. 2 production shaft started. 1970: No. 2 shaft at 670.6 m. 1972: Headframe for No. 2 shaft completed. Five compartment No. 2 shaft completed to 730 m with levels at 60.96 m (200 foot) intervals. 1972-81: mine in production. Mine closed 1981. 1983: production resumed. 1985: mine placed on standby in November. 1989: mine resumed production. 1992: mine placed on standby in the spring. 1995: mine resumed production in May. 1998: mine closed. Production totals recorded in MDI52B09SE00003.


Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Shebandowan

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Peridotite 1 Peridotite Sill/Dyke Host
Mafic lava flow-unsubdivided 2 Adjacent

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1ChalcopyriteEconomicOre
2PentlanditeEconomicOre
3PyriteEconomicOre
4PyrrhotiteEconomicOre

Mineralization Comments

May 30, 2018 (Therese Pettigrew) - A series of replacement sulphide lenses, connected by very narrow widths of sulphides, occur in sheared peridotite. The lenses range from 800-1600 feet (244-488 m) in length and extend over a linear distance of at least 4000 feet (1219 m). The larges lens lies under the lake. The deposit averages 16 feet (4.9 m) in width and contains pyrite, chalcopyrite, pyrrhotite and polydmite in massive and disseminated form (Shklanka, 1969). The Shebandowan orebody is associated with a serpentinized peridotite sill/dyke in contact with mafic metavolcanic rocks and the Shebandowan Lake Stock. The orebody is contained within a sequence of steeply-dipping volcanics, the ore occurring as stringers of sulphides, with the principal ore minerals being pyrrhotite, pentlandite, and chalcopyrite. The ore contains nickel and copper in a 3 to 2 ratio as well as small amounts of cobalt, silver, gold, and the platinum-group metals. Also associated with the orebody along the southern contact is a narrow chromite zone which is adjacent to a fault locally known as the Crayfish Creek Fault (CIM Reporter, April 23, 1980). The chromite zone occurs within serpentinite at the Crayfish Creek fault. Chromite occurs over a 10 foot (3 m) wide zone in layered, brecciated, and finely disseminated form. The main chromite layer is 10-11 cm thick and is defined by a 40-50% modal concentration of very fine-grained chromite. On either side of this main layer is found brecciated fragments of chromitiferous serpentinite (Whittaker, 1979 report in RGP MDI files). Sample F-9-79 collected by OGS staff member J. Scott in 1979 assayed 5.68% Ni, 1.34% Cu, 1950 ppm Co, 0.013 opt Pd, 0.02 opt Au, and 0.44 opt Ag.



Mineral Record Details

References

Mono - Copper, nickel, lead and zinc deposits of Ontario

Publication Number: MDC012 Page: 289-290  Date: 1969

Author: Shklanka R.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of the Lower Shebandowan Lake area, District of Thunder Bay

Publication Number: R110 Page: 21-27  Date: 1973

Author: Morin J.A.

Publisher Name: Ontario Division of Mines

Location:


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