Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52J02SW00016

Record: MDI52J02SW00016

General

Mineral Record Identification
Record Name(s) Mac-Read Vein - 1936, MacDonald-Read - 1936, Butt Option - 1995
Related Record Type Simple
Related Record(s)
Record Status Prospect
Date Created 1995-May-30
Date Last Modified 2023-Aug-03
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Fourbay Lake Area

Latitude: 50° 1' 45.74"    Longitude: -90° 47' 55.21"

UTM Zone: 15    Easting: 657660   Northing: 5544218    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52J02SW

Point Location Description: Map in assessment report 52J02SW0004

Location Method: Based on Assessment

Access Description: Light aircraft can land on the lake in summer and winter. Boat and snowmobile access to the lake is possible from a number of Sturgeon Lake access points off Hwy. 599 between Cobb Bay and Trappers Point.



Exploration History

1936: Prospectors R.A. MacDonald and W.C. Read worked the property in 1936. 1937: T.L. Gledhill wrote a brief report on the property in Feb. 1937. Dr. Gledhill commented on a small stripped area and 9 drill holes situated at the west end of the property. 1937: During the winter, Denman Securities of Toronto financed drilling to explore the vein at depth. The drilling program was not encouraging. 1938-39: A pitting and sampling program carried out in 1938 and 1939 increased the known length of the vein. A 28.7 m long section of the vein was channel sampled to give an uncut gold content of 0.46 ounce gold per ton. 1939: Sylvanite Gold Mines Ltd. optioned the property in July and examined the vein. A section of the vein 16.7 m long previously sampled to contain 0.49 ounce gold per ton was resampled and gave 1.1 ounce gold per ton over 13.7 m. Sylvanite Gold Mines concluded that the potential tonnage did not warrant additional work and dropped the option in the fall of 1939. 1946: C.J. Ryan contracted H. Lundberg to conduct prospecting, magnetic and SP surveys. 1982: G. Armstrong and A. Best drilled a new vein system to the south of the Mac-Read prospect. Armstrong and Best optioned their property, which included the Mac-Read, to Steep Rock Resources, who in turn optioned portions of the property to Falconbridge Ltd., Hudson Bay Exploration and Almaden Resources during the period between 1983 to 1987. Surprisingly, little to no work was done on the Mac-Read prospect. 1990: Armstrong and Best regained control of the claim block and pumped out the southern pit to evaluate it for small scale mining. At the same time, the Mac-Read prospect was mechanically stripped and the area of exposed vein significantly increased. 1991: The Sioux Lookout Resident Geologist examined the prospect and suggested that it might have small scale mining potential. A. Best has since taken a 1 ton bulk sample. 1992: A. Best and G. Armstrong carried out stripping and sampling.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
52J02SW-0024 52J02SW0056 52J02SW0056
52J02SW-0028 52J02SW0054 52J02SW0054
OP93-248 52J02SW0003 52J02SW0003
OP92-252 52J02SW0005 52J02SW0005
OP91-585 52J02NE0002 52J02NE0002
52J02SW CQ-0072 52J01SW0101 52J01SW0101
52J02SW-0017-C1 52J02SW0013 52J02SW0013
52J02SW-0026-B1 52J02SW0044 52J02SW0044
52J02SW-0075-C1 52J02SW0008 52J02SW0008
52J02SW-0072 52J01SW0101 52J01SW0101
52J02SW-0023 52J02SW0037 52J02SW0037

Geology

Province: Superior

Subprovince: Wabigoon

Belt: Sturgeon Lake

Geological Age: Archean  



Geology Comments

Dec 07, 2005 (R Tuomi) - Both the Armstrong-Best and Mac-Read propects share common characteristics. Both are hosted in south facing, east trending pillowed metabasalt units. The grey to blue quartz veins are located in carbonate-silica replaced zones. So called iron formation is present in both prospects; in fact, a rusty, sulphidized zone would be a better description. Gold tenor in both prospects tends to follow sulphide content. Both prospects have recently been shown to terminate by folding to the north, probably by north trending shear zones.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 Quartz - Sulphide Host
Mafic lava flow-unsubdivided 2 Meta Basalt Host
Quartz Porphyry 3 Quartz Near
Gabbro 4 Gabbro Dyke Near

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1ChalcopyriteEconomicOre
2GoldEconomicOre
3MarcasiteEconomicOre
4PyriteEconomicOre
5PyrrhotiteEconomicOre
6SphaleriteEconomicOre
7GalenaEconomicOre
1CalciteEconomicGangue
2QuartzEconomicGangue
CarbonateAlterationCarbonatization1UnknownDisseminated
QuartzAlterationSilicification2UnknownDisseminated

Mineralization Comments

Dec 07, 2005 (R Tuomi) - Two chip sampling studies done in 1939 produced assays on blue quartz veins of 0.46 ounce gold per ton over 28.7 m and 1.1 ounce gold per ton over a length of 13.7 m. The veins vary from 0.6 m to 1 m in width.



Alteration Comments

Dec 07, 2005 (R Tuomi) - Shearing and folding.




Mineral Record Details

References

Article - Sioux Lookout Resident Geologist's District-1991

Publication Number: MP158.004 Page: 81-84  Date: 1997

Author: Janes D.A., Seim G.Wm., Storey C.C.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of the Six Mile Lake area

Publication Number: OFR5838 Date: 1992

Author: Robinson D.J.

Publisher Name: Ontario Geological Survey

Location:


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