Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42C02NW00024

Record: MDI42C02NW00024

General

Mineral Record Identification
Record Name(s) Band-Ore East Occurrence - 2000
Related Record Type Simple
Record Status Occurrence
Date Created 2000-Nov-30
Date Last Modified 2022-Jan-05
Created By A Wilson
Revised By A Wilson

Commodities

Primary Commodities: Diamond



Location

Township or Area: Musquash

Latitude: 48° 7' 56.76"    Longitude: -84° 46' 13.77"

UTM Zone: 16    Easting: 665880.67   Northing: 5333423.69    UTM Datum: NAD83

Resident Geologist District: Sault Ste. Marie

NTS Grid: 42C02NW

Point Location Description: Stripped outcrop on south side of road

Location Method: Field Visit with GPS

Access Description: Drive north along Highway 17 for approximately 22 km from the junction between Highway 17 and Highway 101. Follow the Musquash Township forestry road northeast for approximately 4.5 km to the junction between the forestry road and a skidder trail. The showing is in a stripped area to the southeast of the road.



Exploration History

2000: Band-Ore Resources Ltd. - sampling, airborne geophysical survey, stripping, mapping.


Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Michipicoten

Tectonic Assemblage: Wawa

Geological Age: Neoarchean   Geochronological Age: 2750 MA   Geochron. Age Ref.: GOO VOL 1

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Geology Comments

Dec 07, 2005 (A Wilson) - The diamond occurrences appear to be restricted to a D1 recumbent nappe in the west-central portion of the Michipicoten greenstone belt. The nappe is imbricated by south-vergin reverse faults. The direction of nappe transport is from south to north and it lies immediately north and adjacent to the Kapuskasing Structural Zone. This thrusting and shortening may be related to the tectonic events along the Kapuskasing Structural Zone. The western limit of the nappe is likely the Dickenson Lake fault that passes to the west of the Dickenson Lake stock. The nappe is not likely to extend east beyond the Marsden Fault.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Breccia-unsubdivided 1 Intermediate Host

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1DiamondEconomicOre

Mineralization Comments

Dec 07, 2005 (A Wilson) - A 68-kg sample collected by Band-Ore Resources in 2000 yielded 6 microdiamonds.



Mineral Record Details

References

Map - Geological series, Precambrian geology of Musquash Township, Algoma District

Publication Number: P2568 Scale: 1:15,840    Date: 1982

Author: Sage R.P., England D., Calvert T., Oudkerk G., Worona R., Koscinsko K.

Publisher Name: Ontario Geological Survey


MonoMap - Geology of Abotossaway, Corbiere, Leclaire and Musquash Townships and Part of Dunphy Township, District of Algoma

Publication Number: OFR5587 Scale:     Date: 1993

Author: Sage R.P.

Publisher Name: Ontario Geological Survey


Book - BAND-ORE RESOURCES PRESS RELEASES

Publication Number: Clippings Scale:     Date: 2000

Author:

Publisher Name:


Map - Precambrian Geology Compilation Series - White River Sheet

Publication Number: M2666 Scale: 1:250,000    Date: 2001

Author: Santaguida F.

Publisher Name: Ontario Geological Survey


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For detailed information regarding this mineral record please contact the Sault Ste. Marie Resident Geologist District Office