Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI41J11SW00058

Record: MDI41J11SW00058

General

Mineral Record Identification
Record Name(s) Reuben McKee Property - 1967
Related Record Type Simple
Related Record(s)
Record Status Prospect
Date Created 1991-Sep-01
Date Last Modified 2022-Oct-07
Created By
Revised By

Commodities

Primary Commodities: Copper



Location

Township or Area: Otter, Casson

Latitude: 46° 34' 5.02"    Longitude: -83° 27' 55.42"

UTM Zone: 17    Easting: 311065   Northing: 5160119    UTM Datum: NAD83

Resident Geologist District: Sault Ste. Marie

NTS Grid: 41J11SW

Point Location Description: Adit

Location Method: Data Compilation

Access Description: 400 metres west of the east boundary of Otter Township, 1 kilometre south of Burden Lake.



Exploration History

1967-68: R. McKee - pitting, trenching. 1968: Riocanex - mapping, ground geophysics, DD-2. 1970: Selco Exploration Limited - ground geophysics, DD-4-1220 ft. 1973-74: W.J. Doughty (Otter Mining and Exploration) - underground development (85 m adit), 50 ton bulk sample processed by Noranda and Copper Corporation, one carload (500 tons) of hand-cobbed direct smelting ore produced and sent to Tribag Mine mill. 1990: N.S.A.I Holdings Ltd. - sampling, assaying. 1996: Houston Lake Mining Inc. - ground geophysics. 2007: Dolan and Edwards - sampling, assaying


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
SSMPOtter 4 / 2.14316 41J11SW0007 41J11SW0007
SSMPOtter 06 /2.16660 41J11SW0031 41J11SW0031
2.37827 20000002862 20000002862
CASSON 0028 / 2.48 41J11SW0018 41J11SW0018

Geology

Province: Southern

Subprovince: Cobalt Basin

Supergroup: Huronian Supergroup

Geological Age: Paleoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Diabase 1 Diabase Granophyric Contains
Vein 2 Quartz-Carbonate Host
Granite 3 Adjacent

Lithology Comments

Apr 29, 2013 (A Wilson) - The property consists of an east striking, north dipping, quartz-carbonate vein that ranges from 1-2 m in width and is exposed for approximately 15 metres. It cross cuts a diabase dike that strikes 120 and the strike of the vein is between 70-110º. Both the dike and the vein dip steeply to the north. The diabase dike is displaced about 15 feet in a right-handed fashion. The vein is hosted within a diabase dike. The surrounding country rocks are composed of massive granite. Outcrops of paraconglomerate and sandstone/wacke also occur in the vicinity of the veins.


Dec 07, 2012 (A Pace) - The property consists of an east-west striking, north dipping quartz-carbonate vein that ranges from 1-2 m in width and exposed for approximately 15 metres. The vein is hosted within massive granitic rock with mineralization consisting of chalcopyrite, pyrrhotite, bornite, and minor specular hematite. Hematite is the dominant alteration mineral and is quite pervasive throughout the vein. An adit was developed along strike of the vein but no evidence of work has been obtained. Two samples taken from the Resident Geologist Staff in 2012 each returned assays of 1.4% Cu.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1ChalcopyriteEconomicOre
3BorniteEconomicOre
2PyrrhotiteEconomicGangue
4HematiteEconomicGangue
5SpeculariteEconomicGangue

Mineralization Comments

Apr 29, 2013 (A Wilson) - Mineralization consists of chalcopyrite, pyrrhotite, bornite, and minor specular hematite. Hematite is the dominant alteration mineral and is quite pervasive throughout the vein. Four chip samples collected by the ODM in 1973 across the 165 foot section of the vein averaged 8.4% Cu across 6 feet. Two samples taken by the Resident Geologist Staff in 2012 each returned assays of 1.4% Cu. Grab samples collected by N.S.A.I Holdings Ltd. from the stock piles near the adit assayed in the range of 22.6% Cu. Assays typically ranged from 0.08% Cu (grab sample from muck pile) to 22.64% Cu from a 0.7 m long chip sample from a vein in a trench. A bulk sample (5 lb) collected by Dolan in 2007 and analyzed by Lakefield returned an average Cu value of 15.8% Cu. A 40 lb sample collected by Dolan and processed by Xstrata assayed 19.9% Cu, 0.03% Au and 0.57% Ag.



Mineral Record Details

Classification
RankClassification            
1 Vein
Characteristics
Rank Characteristic            
1 Vein

Site Visit Information

Date: Sep 04, 2012

Geologist: A Pace

Notes: The property consists of an east-west striking, north dipping quartz-carbonate vein that ranges from 1-2 m in width and exposed for approximately 15 metres. The vein is hosted within massive granitic rock with mineralization consisting of chalcopyrite, pyrrhotite, bornite, and minor specular hematite. The composition coupled with the geochemistry that illustrates elevated Fe, FeO levels suggests that hematite is the dominant alteration mineral. Sulphide minerals particularly the chalcopyrite and bornite crystals are concentrated along the margins of the quartz veins with minor disseminated sulphides within the altered areas. The contact between the mineralized quartz-carbonate vein and the granitic rock is quite visible with the contact being irregular. Veining is more prevalent along the contact where they appear to be irregularly oriented into the granitic rock with mineralization only present in the form of specular hematite.



Production Data
Year Tonnes Commodities Reference Comment
1974 508 41J11SW0007 500 tons grading 4.5% Cu

References

File - Resident Geologist files SSMP Otter 15

Publication Number: Date:

Author:

Publisher Name:

Location: SSM RGP office


Mono - Copper, nickel, lead and zinc deposits of Ontario

Publication Number: MDC012 Page: 103  Date: 1969

Author: Shklanka R.

Publisher Name: Ontario Dept. of Mines

Location:


Article - Wakomata Lake area (west half), District of Algoma

Publication Number: MP049.022 Page: 77  Date: 1997

Author: Chandler F.W., Masson S.L.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Article - Sault Ste. Marie District

Publication Number: MP057.004 Page: 86, 88-89  Date: 1997

Author: Rupert R.J.

Publisher Name: Ontario Division of Mines

Location:


Article - 1974 report of the Northeastern Regional Geologist and Sault Ste. Marie Resident Geologist

Publication Number: MP060.007 Page: 155  Date: 1997

Author: Giblin P.E.

Publisher Name: Ontario Division of Mines

Location:


MonoMap - Geology of the Saunders Lake area, District of Algoma

Publication Number: R155 Page: 35-36  Date: 1976

Author: Chandler F.W.

Publisher Name: Ontario Division of Mines

Location:


Map - Geological series, Wakomata Lake area (west half), District of Algoma

Publication Number: P0737 Scale: 1:15,840    Date: 1997

Author: Chandler F.W., Masson S.L., Faust D., Raudsepp M.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Map - Saunders Lake, Algoma District

Publication Number: M2331 Scale: 1:31,680    Date: 1976

Author: Chandler F.W.

Publisher Name: Ontario Division of Mines

Location:


Map - Sault Ste. Marie-Elliot Lake, geological compilation series, Algoma, Manitoulin and Sudbury districts

Publication Number: M2419 Scale: 1:253,440    Date: 1979

Author: Giblin P.E., Leahy E.J.

Publisher Name: Ontario Geological Survey

Location:


Map - Precambrian Geology Compilation Series - Sault Ste. Marie-Blind River Map Sheet

Publication Number: M2670 Scale: 1:250,000    Date: 2003

Author: Johns G.W., McIlraith S.J., Muir T.L.

Publisher Name: Ontario Geological Survey

Location:


Article - Preliminary Results from the Otter-Morin Townships Bedrock Mapping Project, Southern and Superior Provinces

Publication Number: OFR6280.017 Page: 17-1 to 17-10  Date: 2012

Author: Gordon C.A.

Publisher Name: Ontario Geological Survey

Location:


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