Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42A15SW00049

Record: MDI42A15SW00049

General

Mineral Record Identification
Record Name(s) Falconbridge DDH Man35-01 - 1996, Falconbrdige Grid Man96-07 - 1996
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 2002-Sep-13
Date Last Modified 2022-Nov-10
Created By
Revised By

Commodities

Primary Commodities: Nickel



Location

Township or Area: Mann

Latitude: 48° 50' 11.96"    Longitude: -80° 57' 21.65"

UTM Zone: 17    Easting: 503227.735   Northing: 5409298.847    UTM Datum: NAD83

Resident Geologist District: Timmins

NTS Grid: 42A15SW

Point Location Description: Drill collar at 8+25N/5+0W on Falconbridge grid on claim P1200922

Location Method: Based on Assessment

Access Description: Access to the site at the time of drilling was via a plowed access road beginning on highway 11 north at the junction of concession 5 and 6. The road ran west along the concession line to an old bridge across the Fredrickhouse River. A second road was pushed to the southeast to access the grid.



Exploration History

1995-96: Falconbridge Ltd. - ground geophysics, 2 ddh (313 m).


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
T-3740, 2.16646 42A15SW0064 42A15SW0064
T-3740, W9660-00324 42A15SW0059 42A15SW0059

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Abitibi

Geological Age: Neoarchean   Geochronological Age: 2706 MA   Geochron. Age Ref.: MP 169 P. 75



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Peridotite 1 Peridotite Host

Lithology Comments

Dec 07, 2005 (A Wilson) - Diamond drilling intersected a thick sequence of strongly magnetitc peridodite. Magnetite was observed in fine veinlets within olivine and continuing into the matrix. Some thin magnetite-rich veins were also observed within the rock. Serpentine-filled veins were common at the top of the hole and patchy serpentine alteration was observed at depth.




Mineralization

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

Mineralization Comments

Dec 07, 2005 (A Wilson) - Diamond drill hole MAN35-01 intersected a 3 m section of perodotite that returned 3235 ppm Ni. The ultramafic was observed to host few sulphides in either of the drill holes completed by Falconbridge.



Mineral Record Details

References

Article - The Kidd-Munro extension project: results of U-Pb geochronology for Year 1

Publication Number: MP169.012 Date: 1998

Author: Barrie C.T., Corfu F.

Publisher Name: Ontario Geological Survey

Location:


Map - Geological Compilation: Brower, Duff, Fournier, Hanna, Lamarche, Little, Mann, McCart, Newmarket, Reaume, St. John and Tully Townships

Publication Number: P3391 Scale: 1:50,000    Date: 1999

Author: Barrie C.T.

Publisher Name: Ontario Geological Survey

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 Timmins Resident Geologist District Office