Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI32DO4NW00001

Record: MDI32DO4NW00001

General

Mineral Record Identification
Record Name(s) L.2972 Pit 2 - 1996
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1996-Oct-17
Date Last Modified 2022-Jun-10
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Lebel

Latitude: 48° 9' 59.1"    Longitude: -79° 57' 41.37"

UTM Zone: 17    Easting: 577218.167   Northing: 5335318.386    UTM Datum: NAD83

Resident Geologist District: Kirkland Lake

NTS Grid: 32D04NW

Point Location Description: Northwest pit located in claim L.2972 on Map 53A.

Location Method: Field Visit

Access Description: North on the most westerly street in the hamlet of King Kirkland. At the north end, the street intersects a trail running west. A sandy clearing on the north side of the trail is located approximately 80 metres west of the intersection. At this point a snowmobile runs north. Follow the snowmobile trail for approximately 200 metres. Run a compass line from this point at a bearing of 325 degrees for 140 metres. The pit was not located but a large vein follows the northwestern edge of the outcrop.



Exploration History

No recorded exploration. The pit is plotted on ODM Map 53A.


Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Abitibi

Tectonic Assemblage: Timiskaming

Geological Age: Neoarchean   Geochronological Age: 2685 MA   Geochron. Age Ref.: CORFU ET.AL. 1989

Metamorphism Type: Regional

Metamorphism Grade: Zeolite



Geology Comments

Dec 07, 2005 (D Guidon) - The pit is located in a large outcrop of what has been mapped as syenite and basic syenite. To the east and north are the sands of the King Kirkland Esker. To the west are Timiskaming conglomerates. The rock is brick red, fine-medium grained with rounded feldspars and some feldspars as laths. The quartz vein is about 60 cm wide striking about 060 to 070 degrees. The vein material contains abundant inclusions of the host material. The vein itself appears brecciated.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 Quartz Host
Syenitoid-Unsubdivided 2 Footwall
Syenite 3 Syenite Tuff Hanging Wall

Lithology Comments

Dec 07, 2005 (D Guidon) - Gelogy map indiicates that the pit is in basic syenite. Cut hand samples suggest that the rock is syenite.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1QuartzEconomicGangue
QuartzAlterationSilicification1MediumVeins
SericiteAlterationSericitization2MediumDisseminated
ChloriteAlterationSericitization3MediumDisseminated
DolomiteAlterationCarbonatization4MediumNetwork

Alteration Comments

Dec 07, 2005 (D Guidon) - Quartz vein has no carbonate minerals but host rock has veinlets of iron-rich dolomite.




Assay Samples

Assay Samples
CommodityAnalytical MethodDigestion Method ResultUnitLimitQualifier
GoldUnknownBDL

Mineral Record Details

Classification
RankClassification            
1 Epigenetic
Characteristics
Rank Characteristic            
1 Vein

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Vein

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 60 .6 240 70

Site Visit Information

Date: Oct 18, 1996

Geologist: D Guidon

Notes: Visit Date: July 21, 1994 - rain shortened visit Attempted to find the pit without success. The outcrop was found and the vein was found near the edge of the outcrop. The 25 inch wide vein is exposed for a length of over 200 feet. Samples 94327 - Course grained pink couloured rock conatining no carbonate minerals. Contains 20% fragments of syenite and about 10% interstial sericite. Analyses - <3 ppb Au Analysis by OGC Laboratories, Sudbury. 94328 - Brick red medium grain syenite. 40% red feldspars, 30% white feldspars, 5-10% sericite, 10% chlorite and about 10% rock fragments. Moderate carbonate alteration as threads of iron-rich dolomite.



References

Map - Township of Lebel, District of Timiskaming, Ontario

Publication Number: ARM53A Scale: 1:12,000    Date: 1997

Author: MacLean A., Hogg N.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Geology Of Lebel Township

Publication Number: B150 Date: 1998

Author:

Publisher Name:

Location:


Mono - Geology of Lebel Township, District of Timiskaming

Publication Number: OFR5211 Date: 1976

Author: Lovell H.L.

Publisher Name: Ontario Division of Mines

Location:


Journal - U–Pb zircon geochronology in the southwestern Abitibi greenstone belt, Superior Province; Canadian Journal of Earth Sciences (1989) vol. 26, no. 9

Publication Number: CJES26 Page: 1747-1763  Date: 1989

Author: Corfu, F., Krogh, T.E., Kwok, Y.Y., Jensen, L.S.

Publisher Name: Canadian Journal of Earth Sciences

Location:


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