Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52F09SE00043

Record: MDI52F09SE00043

General

Mineral Record Identification
Record Name(s) HW 673 - 1960, Revell Twp Conc IV Lot2 - 1960
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 2000-Nov-22
Date Last Modified 2022-Aug-04
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Revell

Latitude: 49° 35' 56.71"    Longitude: -92° 9' 27.85"

UTM Zone: 15    Easting: 560862.728   Northing: 5494397.57    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52F09SE

Point Location Description: Mineral occurrence at surface symbol (Map, GDIF398)

Location Method: Field Visit

Access Description: The H.W. 673 Occurrence is located on mining location H.W. 673 in lot 2, Concession IV, Revell Township, north of Tache. The occurrence is accessible from a narrow gravel road which branches east from the Basket Lake Road, approximately 7.3 km north of its intersection with the Trans Canada Highway. Located 6 km northeast of Tache Station - continue north of Tache for 4.5 km then east for 300 metres (across the river) then south for 1 kilometre. The shaft is 100 metres east of the road.



Geology

Province: Superior

Subprovince: Wabigoon

Terrane: Western Wabigoon

Belt: Eagle-Wabigoon-Manitou

Geological Age: Precambrian  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1 Amphibolitized Contains

Mineralization Comments

Aug 04, 2022 (Q Unknown) - The occurrence is situated within amphibolite grade, mafic, metavolcanic flows intruded by wide felsic dikes within a northwest-trending shear zone. The occurrence is 1.2 km north of the contact between dioritic rocks of the Revell Batholith and the mafic metavolcanics. The geology at the occurrence consists of amphibolitized, dark green, chloritic, intensely sheared (120°/76° SW), mafic metavolcanic flows intruded by a 6 m wide quartz-feldspar porphyry dike which hosts the majority of the quartz veins. The dike is intensely sheared, and contains tiny, white, feldspar phenocrysts, and small [

Mineral Record Details

References

Part - Geology of Errington Township, Little Long Lac area

Publication Number: ARV60-06 Page: 26  Date: 1997

Author: Pye E.G.

Publisher Name: Ontario Dept. 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 Date: 1989

Author: Parker J.R.

Publisher Name: Ontario Geological Survey

Location:


Report an Error

We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.


Terms of Use

Please review our Terms of Use agreement for this data product.


Ministry Contact Information

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