Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42A08SE00099

Record: MDI42A08SE00099

General

Mineral Record Identification
Record Name(s) Chamandy-North Occurrence - 1948, Golden Cradle Resources Ltd. - 1983, Domego Resources Ltd. - 1985, Highway 11 Property - 1985
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1979-Aug-07
Date Last Modified 2023-Jan-23
Created By
Revised By

Commodities

Primary Commodities: Copper

Secondary Commodities: Gold, Silver



Location

Township or Area: Benoit

Latitude: 48° 21' 14.09"    Longitude: -80° 14' 41.72"

UTM Zone: 17    Easting: 555939   Northing: 5355912.99    UTM Datum: NAD83

Resident Geologist District: Kirkland Lake

NTS Grid: 42A08SE

Point Location Description: Property symbol

Location Method: Based on Assessment



Exploration History

1948: K. Chamandy – pitting, trenching, sampling.. 1983: Golden Cradle Resources Ltd. – VLF-EM and magnetometer surveys. 1985: Domego Resources Ltd. – mapping, soil sampling. 1990: Queenston Gold Mines Ltd. – DD-1-379 ft.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
22 42A08SE0066 42A08SE0066
2.6401 42A08SE0092 42A08SE0092
KL-0694/2.8903 42A08SE0086 42A08SE0086

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Abitibi

Tectonic Assemblage: Blake River

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic pillowed flow 1 Basalt Pillowed Adjacent
Intermediate lava flow-unsubdivided 2 Andesite Adjacent
Vein 3 Quartz Contains
Granodiorite 4 Adjacent
Syenite 5 Adjacent

Lithology Comments

May 25, 2016 (A Wilson) - A shear zone 2-3 ft. wide in pillowed lava has been exposed by stripping on the southeast side of a hill. The shear strikes N36ºW and dips steeply to the southwest. The intermediate rocks of the property area are dominated by massive andesite. This rock type is restricted to the north-eastern portion of the property and occurs as a massive, very hard (cherty), fine grained, significantly fractured, non-magnetic outcrop. The rock is a light brownish grey on the weathered surface and a lighter greenish colour than its mafic equivalent on the fresh surface. This rock also typically contains quartz veinlets with associated minor sulphides. Mafic to intermediate intrusive rocks dominate the exposed outcrop of the property, and are most prominent in the eastern and central portions of the mapped area. These rocks represent portions of differentiated mafic to intermediate irregular-shaped sills. The rocks gabbroic in composition were distinguished in the field from their more felsic dioritic counterparts on the basis of colour and magnetizability. Both these characteristics are a result of the rock's mineral compositions. The gabbroic rocks consist of strictly mafic minerals and are usually free of magnetite and thus non-magnetic, whereas the rocks dioritic in compostion usually appear lighter in colour because of the presence of felsic minerals and are magnetic due to the presence of magnetite




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
2ChalcopyriteEconomicOre
1PyriteEconomicGangue

Mineralization Comments

May 25, 2016 (A Wilson) - A 3 foot channel sample across the face of the shear zone assayed 4.5 to 7.7% Cu, trace to 0.14 oz./t Ag and up to 0.01 oz./t Au. One sample, B-3, lies just west and directly on strike with the southern geochemical anomaly. This sample contains 0.001 oz/ton Au and 4.6 oz/ton Cu which corresponds closely with the Au soil anomaly found at the west end of the above-mentioned geochemical soil anomaly. Another sample, B-2, contains the highest concentration of each element assayed. These values, in oz/ton, are as follows: 0.001 Au, 0.16 Ag, 34 Cu, 5.3 Pb and 1.5 Zn. Both above samples were collected from old pits found on the property.



Mineral Record Details

Characteristics
Rank Characteristic            
1 Sheared

References

File - Resident Geologist files KL-0478, KL-1907, KL-2940

Publication Number: Date:

Author:

Publisher Name:

Location: Kirkland Lake RGP office


Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file

Publication Number: OFR5467 Page: G0100  Date: 1983

Author: Hodgson C.J.

Publisher Name: Ontario Geological Survey

Location:


Mono - Gold deposits of Ontario, part 2, part of District of Cochrane, districts of Muskoka, Nipissing, Parry Sound, Sudbury, Timiskaming, and counties of southern Ontario

Publication Number: MDC018 Page: 16  Date: 1979

Author: Gordon J.B., Lovell H.L., de Grijs J.W., Davie R.F.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of the Bourkes area, District of Timiskaming

Publication Number: R092 Page: 17  Date: 1971

Author: Lovell H.L.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Map - Benoit and Maisonville townships, Timiskaming District

Publication Number: M2215 Scale: 1:31,680    Date: 1971

Author: Lovell H.L.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Map - Geological Compilation of the Lake Abitibi Area, Abitibi Greenstone Belt

Publication Number: P3398 Scale: 1:100,000    Date: 1999

Author: Ayer J.A., Berger B.R., Trowell N.F.

Publisher Name: Ontario Geological Survey

Location:


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