Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42C03SW00042

Record: MDI42C03SW00042

General

Mineral Record Identification
Record Name(s) Harper Showing - 1997, Areseno Creek Showing - 1987, University Zone - 1987, Asarco Conductor 22 East - 1973
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 2001-Aug-20
Date Last Modified 2022-Sep-13
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: St. Germain

Latitude: 48° 2' 45.31"    Longitude: -85° 16' 6.34"

UTM Zone: 16    Easting: 629050.74   Northing: 5322854.54    UTM Datum: NAD83

Resident Geologist District: Sault Ste. Marie

NTS Grid: 42C03SW

Point Location Description: Exposure in Arseno Creek bed

Location Method: Based on Assessment

Access Description: The site is accessible by helicopter from Wawa.



Exploration History

1973: Asarco Exploration Co. - airborne geophysics, mapping, sampling. 1984-94: MacMillan Gold Corp/Granges Inc. - airborne geophysics, ground geophysics, soil sampling, stream sediment sampling, prospecting, mapping, 5 ddh (338.72 m). 1997: Mishibishu Gold Corporation/MacMillan Gold Corp. - soil survey, mapping.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
Groseilliers-0015 42C03SE0013 42C03SE0013
WP St. Germain-4 42C03SE0001 42C03SE0001
WP St. Germain-5 42C03SW0003 42C03SW0003
ST GERMAIN 0010
WP Mishibishu Lake.48 42C03SW0024 42C03SW0024
42C03SW0028 42C03SW8783 42C03SW8783
WP Mishibishu Lake.42 42C03SE2001 42C03SE2001
WP St. Germain-6 42C03SW2001 42C03SW2001

Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Mishibishu Lake

Geological Age: Neoarchean   Geochronological Age: 2.7 GA   Geochron. Age Ref.: GOO VOL 1 P. 494



Geology Comments

Dec 07, 2005 (A Wilson) - The Mishibishu Deformation Zone (MDZ) is the largerst of the deformation zones in the belt, measuring approximately 40 km in length and several hundred metres up to 1.5 km in width. The zone is located north of the Mishibishu Lake Stock and lies along the lithological contact of mafic metavolcancis to the north, with clastic metasediments to the south. The Eastern Mishibishu Deformation Zone becomes narrower approaching Lake Superior where the zone transects the external granitoids east of the greenstone belt. Deformation and alteration are less pervasive and shear zones become more dicrete than in the central MDZ. Stretchin lineations plunge to the east. The style of deformation is more brittle-ductile in the eastern MDZ. Alteration is less pervasive than, yet similar to, other zones within the belt.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic Tuff 1 Amphibolitized Tuff Host
Schist-Unsubdivided 2 Quartz-Feldspar Host
Sandy Mudstone 3 Greywacke, Argillite Near

Lithology Comments

Dec 07, 2005 (A Wilson) - At depth, elevated gold values are returned from a quartz sericite schist which occurs at the contact between amphibolitized mafic tuffs and overlying argillite/greywacke. Quartz veining is present but minor.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1ArsenopyriteEconomicGangue
2PyriteEconomicGangue
3PyrrhotiteEconomicGangue

Mineralization Comments

Dec 07, 2005 (A Wilson) - Grab samples at surface returned values raning from 850 ppb Au to 4400 ppb Au. Elevated gold values have been returned from drill core. These values range from 0.95 g/t au over 4.88 m to 2.96 g/t Au over 4.26 m.



Mineral Record Details

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Shear

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Regular 150 25 250 75

Site Visit Information

Date: Aug 20, 2001

Geologist: A Wilson

Notes: The mafic tuffs in this area strike 250 and dip 70 to 80 north. Two outcrops in the immediate area display fold axial planes that have a similar strike but dips 70 south. The fold axes plunge 20 to the NE. Mineralized extensions may be related to the attitutde of the axial plane.



References

File - Resident Geologist files WP Mishibishu Lake.40, St. Germain-0010

Publication Number: Date:

Author:

Publisher Name:

Location: SSM RGP office


Folio - St. Germain Township, Sault Ste. Marie Mining Division, NTS No. 42C/03S

Publication Number: GDIF591 Date: 1997

Author: Wawa RGO

Publisher Name: Ontario Geological Survey

Location:


Map - Precambrian geology, Mishibishu Lake area, Dog Harbour sheet

Publication Number: P3157 Scale: 1:15,840    Date: 1992

Author: Reid R.G., Bowen R.P., Heather K.B., Logothetis J., Reilly B.A.

Publisher Name: Ontario Geological Survey

Location:


Map - Geological series, Precambrian geology, Mishibishu Lake area, northeastern section, districts of Thunder Bay and Algoma

Publication Number: P2970 Scale: 1:15,840    Date: 1986

Author: Bowen R.P., Logothetis J., Heather K.B.

Publisher Name: Ontario Geological Survey

Location:


Mono - Geology, structure and economic geology of the Mishibishu Lake area

Publication Number: OFR5774 Page: 153-154, 159-160  Date: 1991

Author: Reid R.G., Bowen R.P., Reilly B.A., Logothetis J., Heather K.B.

Publisher Name: Ontario Geological Survey

Location:


Map - Operation Pukaskwa, districts of Algoma and Thunder Bay

Publication Number: P0541 Scale: 1:126,720    Date: 1997

Author: Bennett G., Thurston P.C., Giguere J.F.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Operation Pukaskwa, University River sheet, districts of Thunder Bay and Algoma

Publication Number: P0507 Scale: 1:63,360    Date: 1997

Author: Bennett G., Thurston P.C., Giguere J.F.

Publisher Name: Ontario Dept. of Mines

Location:


Map - University River, Algoma and Thunder Bay districts

Publication Number: M2333 Scale: 1:63,360    Date: 1976

Author: Bennett G., Thurston P.C., Giguere J.F.

Publisher Name: Ontario Division of Mines

Location:


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