Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52N04SW00014

Record: MDI52N04SW00014

General

Mineral Record Identification
Record Name(s) Sanshaw Prospect - 1936, Whitehorse Island - 1983, Bonanza Red Lake Explorations Prospect - 1979, Orlac - 1946, Cable Mines and Oils Ltd. - 1953
Related Record Type Simple
Related Record(s)
Record Status Developed Prospect With Reported Reserves or Resources
Date Created 1983-Sep-14
Date Last Modified 2022-Oct-13
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Dome

Latitude: 51° 2' 21.82"    Longitude: -93° 48' 55.23"

UTM Zone: 15    Easting: 442836.62   Northing: 5654521.99    UTM Datum: NAD83

Resident Geologist District: Red Lake

NTS Grid: 52N04SW

Point Location Description: Shaft symbol on Whitehorse Island KRL11325 map 2074

Location Method: Data Compilation

Access Description: From Red Lake, Whitehorse Island can be reached by traveling north along bush access roads and then via winter access roads, snowmobile, boat, or aircraft depending on seasonal conditions.



Exploration History

1936: Sanshaw Mines drilled 15 diamond drill holes totalling 1160 m. 1937: Sunk a shaft to 30 feet. 1939-1940: McKenzie Red Lake Gold Mines drilled 4 holes totalling 350 m. 1946-1947: Orlac Red Lake Mines sank shaft to 137 m. Levels established at 67.5 m and at 112.5 m. 690 m of development on these levels. 1953 to 1977: Name of company changed, sold 80% to Cable Mines and Oils Ltd., property ended up with St. Fabien Copper Mines Ltd. who sold 85% to Xtra Developments. 1979-80: Bonanza Red Lake Mines options property and completes geophysics EM, magnetic and gradient surveys), and 7 diamond drill holes totalling 1030 m. 1987: Pure Gold resources carried out exploration on behalf of Noramco Mining Corp. Surface sampling, IP, VLF and magnetometer surveys, drilling 48 DDH for 6637 m. 1988-89: Noramco drilled 34 holes for 4785 m. 2003: Wolfden Resources Inc and Lateegra Resources Corp entered joint venture and completed a magnetometer survey, surface mapping, sampling and 5 DDH for a total of 625 m on Whitehorse Island. 2004: New joint venture between Red Lake Resources and Grandcru Resources Corp. drilled 7 DDH for 1020 m and conducted magnetometer survey over ice. 2006: Grandview Gold Inc optioned the property and conducted a magnetometer survey. 2008: Grandview completed 5 DDH totalling 991 m but only 3 produced core. 991 m and only 2 reached targets. 2012: Grandview conducted an IP survey. 2015: Grandview delisted from the NEX stock exchange, sold its assets and was renamed to Pudo Inc.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
RL AF# RL5081, AFRO# 2.34059 20000001928 20000001928
2.39778 20000003625 20000003625
2.27080 52N04SW2074 52N04SW2074
19 52N04SW0106 52N04SW0106
63.3611 52N04SW0062 52N04SW0062

Geology

Province: Superior

Subprovince: Uchi

Terrane: North Caribou

Domain: Uchi

Belt: Red Lake

Geological Age: Archean  

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Geology Comments

Dec 07, 2005 (K R Kettles) - The prospect is located along the eastern contact of the Dome granite-granodiorite stock and the adjacent felsic volcanics. The prospect is underlain by a broad zone in which the granodiorite stocks of the Dome Stock, and the adjacent volcanics have been variably fractured, sheared, and hydrothermally altered. Gold mineralization occurs in narrow irregular lenses of intense alteration, fracturing, and quartz veining within this broad zone of deformation and alteration. The auriferous lenses strike north-south, and dip 80 degs E. The granodiorite-volcanic contact strikes N20 degs E and dips 78 degs W. The auriferous lenses occur in a narrow volume of rock 102 m in length, varying from 3 to 7.5 m in width and extending downward to the granodiorite-volcanic contact. No auriferous lense have been discovered in the fractured and altered volcanic rocks.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Granodiorite 1 Fractured/Sheared Contains
Terrigenous-Clastic-Unsubdivided 2 Greywacke Near
Vein 3 Cherty Quartz Lenses And Veins Host
Felsic lava flow-unsubdivided 4 Altered Fractured,Sheared Adjacent

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicOre
2PyrrhotiteEconomicOre
3ChalcopyriteEconomicOre
4SphaleriteEconomicOre
5TetrahedriteEconomicOre
6StibniteEconomicOre
7JamesoniteEconomicOre
8GoldEconomicOre
1QuartzEconomicGangue
2ChertEconomicGangue
CarbonateAlterationCarbonatization1UnknownDisseminated
SericiteAlterationChloritic2UnknownDisseminated
ChloriteAlterationChloritic3UnknownDisseminated
SilicaAlterationChloritic4UnknownDisseminated

Mineralization Comments

Dec 07, 2005 (K R Kettles) - The auriferous lenses have highly variable geometries, and dimensions. They consist of irregular zones of silification adjacent to fractures in altered granodiorite, and irregular zones of altered granodiorite containing cherty blue grey quartz stringers. The best gold values occur in association with these cherty quartz stringers, either in the cherty stringers, or in the adjacent silicified wall rocks. Minor amounts (<1%) of sulphides are associated with the gold, Jamesonite?, and stibnite?. Late, and barren quartz-tourmaline veins, stringers, and small masses occur in close association with the auriferous lenses.


Apr 28, 2016 (Therese Pettigrew) - In 1979, Bonanza Red Lake Explorations Ltd. conducted geophysical surveys and drilled six holes. The best intersection was reported from hole B79-1, which returned 0.159 oz/t over 17.02 feet (4.95 g/t Au over 5.2 m). Hole NBZ-88-10 drilled by Pure Gold Resources in 1988 graded 4.53 g/t over 26 m, with a 5.5 m interval grading 13.65 g/t, 3.3 m grading 22.22 g/t, and 2 m grading 34.94 g/t (AFRO 2.39778).



Alteration Comments

Dec 07, 2005 (K R Kettles) - In the immediate vicinity of the prospect , the feldspars in the granodiorite have been altered to sericite and carbonate, and the hornblende has been chloritized. In the auriferous lenses, the altered granodiorite has been silicified.




Mineral Record Details

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Shear

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Irregular 102 5 360 80

Site Visit Information

Date: Jan 24, 1997

Geologist: K R Kettles

Notes: N/A



Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
Sanshaw Prospect 1958 Possible 158760 OFR 5558 P. 354, Northern Miner - June 11, 1953 Between surface and 112.5 metre level Grade: 6.86 g/t Au (175 000 tons at 0.2 opt Au) Gold 6.86 Grams per Tonne

References

Map - Dome Township, Kenora District

Publication Number: M2074 Scale: 1:12,000    Date: 1997

Author: Ferguson S.A.

Publisher Name: Ontario Dept. of Mines

Location:


Part - Geology and mineral deposits of the Red Lake area

Publication Number: ARV49-02 Page: 128-133, 207-210  Date: 1998

Author: Horwood H.C.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of Dome Township, District of Kenora

Publication Number: R045 Page: 49-51  Date: 1997

Author: Ferguson S.A.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay

Publication Number: MDC013 Page: 214-215  Date: 1971

Author: Ferguson S.A., Groen H.A., Haynes R.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2

Publication Number: OFR5558 Page: 353-354  Date: 1987

Author: Durocher M.E., Burchell P.S., Andrews A.J.

Publisher Name: Ontario Geological Survey

Location:


Book - Canadian Mines Handbook 1975

Publication Number: CMH 1975 Date: 1975

Author: Fieldor, F.M. and Wordobec, A.

Publisher Name:

Location:


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