Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42E01SE00004

Record: MDI42E01SE00004

General

Mineral Record Identification
Record Name(s) Big Joe Creek (North) Sulphide Occurrence - 1991, Llyod-Davis Sulphide Occurrence - 9999
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1991-Apr-02
Date Last Modified 2022-Jun-10
Created By
Revised By

Commodities

Primary Commodities: Sulphur/Pyrite



Location

Township or Area: Blood Lake Area

Latitude: 49° 4' 47.18"    Longitude: -86° 13' 35.83"

UTM Zone: 16    Easting: 556476.412   Northing: 5436611.824    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 42E01SE

Point Location Description: Stipped area

Location Method: Field Visit

Access Description: The Big Joe Creek (North) sulphide occurrence is located approximately 31 km west-southwest of Manitouwadge, 6.5 km southeast of Vein Lake, and 750 m east-southeast of the southern end of Little Joe Lake. The occurrence is accessible via motor vehicle followed by travel in boat and on foot. From Manitouwadge, proceed west and north along the Caramat Industrial road for approximately 16.8 km to the Lower Landing road. Proceed west along the Lower Landing road for approximately 7 km to the Pic River. Cross the river and proceed west, on foot, along a well maintained trapline trail for approximately 12 km to the main showing at the Baarts-Donaldson copper occurrence (described elsewhere in this report). Proceed through the bush on a bearing of 130 degrees for approximately 1.4 km to the vicinity of the occurrence. Sulphide mineralization is exposed in several small stripped areas along the northeast end of a small northeasterly- trending hill. Alternatively, the occurrence is accessible via float plane to a small unnamed lake located approximately 1.4 km northeast of the occurrence, followed by travel on foot from the south end of this lake on a bearing of approximately 210 degrees.



Exploration History

1965: Linecutting and a ground geophysical survey (EM); Kerr Addison Mines Limited. 1966: Geological mapping; M.E. Coates (OGS). 1971: Stripping; prospector E. Starr. 1978: Regional lake sediment and water geochemical survey; GSC-MNR. Samples collected from lakes in the vicinity of the occurrence contained slightly anomalous amounts of Ni but not Cu, Zn nor Au. 1989: Dighem airborne geophysical survey (EM, MAG, VLF-EM); Noranda Exploration Company, Limited and Noranda Minerals Inc. (Geco Division). 1991: Lithogeochemical sampling; D.B. McKay (OGS). 1991-1992: Reconnaissance till sampling survey; I.M. Kettles (GSC).


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
63.657 42E01SE8348 42E01SE8348
63.1660 42E01SE0004 42E01SE0004
63.1300 42F05SW0002 42F05SW0002

Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Manitouwadge-Hornepayne

Geological Age: Archean  

Metamorphism Type: Regional

Metamorphism Grade: Amphibolite



Geology Comments

Dec 07, 2005 (D McKay) - The occurrence is located in the Wawa Subprovince and is underlain primarily by a narrow (up to 600 m wide), north- northeasterly-trending (020 ), discontinuous belt of highly deformed and metamorphosed, locally migmatitic, mafic meta- volcanic and metasedimentary rocks interpreted to represent the western extension of the Manitouwadge greenstone belt (Knight 1955; Coates 1970; Hawkins 1971: Kusins 1980). These metavolcanic and metasedimentary rocks are enclosed within granitic gneisses of the Black-Pic batholithic complex and have been intruded locally by dikes of quartz-feldspar pegmatite and diabase (Knight 1955; Coates 1970). The Little Joe Lake fault, a regional-scale, northwesterly-trending, dextral fault is located approximately 250 m north of the occurrence (Coates 1970, Map 2192). The occurrence is located at the northern end of a discontinuous zone(s) of sulphide-mineralized rock approximately 100 m wide and 875 m in length. This mineralized zone trends parallel to the local foliation (approximately 200 degrees) and is centered around a 6 m wide diabase dike (Knight 1955; Hawkins 1972). The Lloyd-Davis sulphide occurrence is located along the same zone approximately 875 m to the south.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Paragneiss 1 Biotitic, Q-Rich Paragneiss Host
Diabase 2 Diabase Near
Mafic lava flow-unsubdivided 3 Near

Lithology Comments

Dec 07, 2005 (D McKay) - The sulphides occur primarily within strongly deformed and metamorphosed, locally migmatitic metasedimentary rocks. The metasedimentary rocks consist primarily of rusty- to tan- and yellow-weathering, moderately to locally strongly foliated, coarse-grained, narrowly banded (on a mm to cm scale), biotitic, quartz-rich schists and gneisses.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicOre
2PyrrhotiteEconomicOre

Mineralization Comments

Dec 07, 2005 (D McKay) - The sulphides consist primarily of pyrite and pyrrhotite. The sulphides typically constitute 2 to 3% of the mineralized zone, and occur as fine- to medium-grained, subhedral, disseminated grains and poorly defined, narrow,foliation-parallel laminae. Grab samples collected from the occurrence in 1991 by D.B. McKay for the OGS returned assay values of up to 124 ppm Cu and 110 ppm Zn. No Au nor Ag was detected.



Mineral Record Details

Classification
RankClassification            
1 Unknown
Characteristics
Rank Characteristic            
1 Disseminated

References

File - Schreiber-Hemlo Resident Geologist Mineral Deposit Files

Publication Number: Min Dep Date: 1996

Author:

Publisher Name:

Location: Thunder Bay RGP


Map - Killala-Vein lakes area, District of Thunder Bay

Publication Number: P0382 Scale: 1:63,360    Date: 1997

Author: Coates M.E.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Vein Lake sheet, Thunder Bay District

Publication Number: M2192 Scale: 1:63,360    Date: 1970

Author: Coates M.E.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Mineral Occurrences in the Manitouwadge Area, Volumes 1, 2 and 3

Publication Number: OFR5906 Date: 1994

Author: McKay D.B.

Publisher Name: Ontario Geological Survey

Location:


Book - AF 63.657

Publication Number: 63.657 Date: 1955

Author: Knight, F.C.

Publisher Name:

Location: Thunder Bay RGP


Map - Manitouwadge sheet, districts of Thunder Bay and Algoma, geological compilation series

Publication Number: P0494 Scale: 1:126,720    Date: 1997

Author: Milne V.G.

Publisher Name: Ontario Dept. of Mines

Location:


Book - AF 63.1660

Publication Number: 63.1660 Date: 1965

Author: MacTavish, R.O.

Publisher Name:

Location: Thunder Bay RGP


Map - Manitouwadge-Wawa sheet, geological compilation series, Algoma, Cochrane, Sudbury and Thunder Bay districts

Publication Number: M2220 Scale: 1:253,440    Date: 1972

Author: Milne V.G., Giblin P.E., Bennett G., Thurston P.C., Wolfe W.J., Giguere J.F., Leahy E.J., Rupert R.J.

Publisher Name: Ontario Division of Mines

Location:


MonoMap - Geology of the Killala-Vein lakes area, District of Thunder Bay

Publication Number: R081 Date: 1970

Author: Coates M.E.

Publisher Name: Ontario Dept. of Mines

Location:


File - Schreiber-Hemlo Resident Geologist Mineral Deposit Files

Publication Number: Min Dep Date: 1971

Author: Hawkins, W.M.

Publisher Name:

Location: Thunder Bay RGP


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For detailed information regarding this mineral record please contact the Thunder Bay South Resident Geologist District Office