Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52B10SE00029

Record: MDI52B10SE00029

General

Mineral Record Identification
Record Name(s) East Coldstream Deposit - 1957, Osmani Gold Deposit - 2012, Shield Developme57 - 1991
Related Record Type Partial
Related Record(s)
Record Status Developed Prospect With Reported Reserves or Resources
Date Created 1991-Mar-25
Date Last Modified 2024-Feb-13
Created By
Revised By

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper, Silver



Location

Township or Area: Burchell Lake Area

Latitude: 48° 36' 19.32"    Longitude: -90° 33' 23.41"

UTM Zone: 15    Easting: 680124.47   Northing: 5386469.98    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 52B10SE

Point Location Description: Precise

Location Method: Data Compilation

Access Description: The Property is approximately 115 km west of Thunder Bay, Ontario via TransCanada Highway 11/17, then Highway 11 and then Highway 802, 2 km west of the village of Kashabowie. The Osmani Gold Deposit is accessed by a series of logging roads from Highway 802.



Exploration History

1952-55: Coldstream Copper Mines Ltd. conducted mapping and drilling. 1987: Noranda conducted prospecting, line cutting, humus and soil sampling, preliminary geological mapping, IP and magnetometer surveys, trenching and channel sampling. Discovered the North, East and Main Zones. Lacana Exploration conducted geological mapping, trenching, prospecting, and VLF, IP and magnetic surveys. Defined Sander’s Zone. 1988: Noranda conducted diamond drilling totalling 1200 m, max/min survey, lithogeochemistry and geological mapping. 1989: Noranda conducted 900 m of diamond drilling, trenching, channel sampling and a magnetometer survey. Lacana drilled 5 DDH into Sander’s Zone. 1990: Independence Mining optioned the property from Lacana conducted line cutting, mapping and sampling. Noranda conducted almost 1500 m of diamond drilling. 1991: Noranda conducted 2600 m of diamond drilling targeting the Main zone. Independence Mining pulled out of Canada and returned the property to Lacana. T. Sanders conducted prospecting, sampling and limited mapping. 2002: Alto Ventures acquired the property. Alto Ventures and Kinross Gold Corp drilled 7 DDH totalling 1668 m in a joint venture. 2005: Alto Ventures conducted airborne and ground geophysics, VTEM survey and IP survey. 2006: Alto Ventures drilled 13 DDH totalling 2062 m and resampled some historic holes. 2007: Alto Ventures trenched and sampled IP targets south of the Sanders Zone. 2009: Alto Ventures and Foundation Resources entered into an agreement to have Foundation earn into the property. Foundation conducted mapping and sampling on Sanders Zone. 2010: Foundation conducted an IP survey and sampling and drilled 36 DDH totalling 9725 m. 2011: Foundation Resources drilled 20 DDH totalling 7263 m and finished the work commitments to earn 100% of the Coldstream property. 2012: Foundation renamed to Coldstream Mineral Ventures Corp. 2013: Coldstream renamed to Birch Hill Gold Corp. 2014: Birch Hill and Canoe Mining merge to form Canoe Mining Ventures Corp. 2016: Wesdome Gold Mines purchased the Hamlin and Coldstream properties from Canoe Ventures Corp. Grid cutting and IP surveys were completed over the OGD as well as 4 00 m of diamond drilling.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
63A.186 52B10SE0150 52B10SE0150
63.379 52B10SE0151 52B10SE0151
OM91-092 52B10SE0019 52B10SE0019
2.31892 20000001255 20000001255
2.35482 20000002602 20000002602
2.27168 52B10SE2022 52B10SE2022
2.53734 20000013648 20000013648
2.47569 20000006200 20000006200
12 52B10SE0143 52B10SE0143

Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Shebandowan

Geological Age: Archean  



Geology Comments

Aug 27, 2015 (Therese Pettigrew) - The North Coldstream-Span-Moss shear zone is a significant northeast-striking regional structure that extends through the Property. The structure is identified as a corridor of variably deformed and altered rocks (sericite, silica, hematite-magnetite, potassium assemblages) of significant strike length. It hosts significant gold and copper-gold mineralization, both on and adjacent to the Property. An intensely altered (silicification) and deformed gabbroic sill-like body hosting copper-gold mineralization at the past producing North Coldstream Mine is located on the Property approximately 2 km west of the Osmani Gold Deposit. Within the regional context, the North Coldstream copper-gold deposit is situated at the contact of felsic-mafic metavolcanic rocks (McCracken, 2011).




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1 Host

Lithology Comments

Aug 27, 2015 (Therese Pettigrew) - The Property is underlain by Archean mafic and intermediate to felsic metavolcanic rocks which have been intruded subconcordantly to concordantly by numerous sills and dikes of gabbro, diorite, quartz, and quartz-feldspar porphyries. The mafic metavolcanics and associated synvolcanic gabbroic intrusions dominate the northeastern portion of the Property, felsic to intermediate metavolcanic rocks being the most predominant lithologies in the central and southwestern parts of the Property. Syn- to post tectonic composite granitoid plutons bound the Coldstream claims on virtually all sides (McCracken, 2011).




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
2ChalcopyriteEconomicOre
3PyriteEconomicOre
4GoldEconomicOre
SilicaAlterationSilicification1UnknownDisseminated
CarbonateAlterationCarbonatization2UnknownDisseminated
AlbiteAlterationAlbitization3UnknownDisseminated
SericiteAlterationSericitization4UnknownDisseminated
HematiteAlterationHematization5UnknownDisseminated

Mineralization Comments

Aug 27, 2015 (Therese Pettigrew) - The Property hosts several gold and copper-gold deposits, which are roughly aligned along the North Coldstream Shear Zone-Span-Moss Shear Zone, identified by a northeastsouthwest-trending mineralized corridor/structure. This structural corridor is characterized by variably altered, schistose and mineralized host rocks. The most significant mineralization on the Property is contained within the North Coldstream (copper-gold) and Osmani (gold) deposits, which occupy roughly one-third of the mineralized corridor. Mineralization is predominantly associated with sheared and altered mafic to intermediate metavolcanic rocks as well as quartz and quartz-feldspar porphyries. The mineralized metavolcanic rocks are typically both bounded and intruded by the porphyries. The mineralized rocks are variably schistose, silicified, carbonatized,oxidized and locally display strong to intense iron-carbonate and hematite alteration. Sulphide mineralization occurs in both the metavolcanics and porphyry rocks as disseminations and seams along the schistosity planes within and/or adjacent to shear zones. Significant assays from the 2010 drill program include: DDH C-10-15: 4.88 g/t Au over 27.28 m; DDH C-10-16: 1.12 g/t Au over 111.3 m; DDH C-10-25: 3.06 g/t Au over 13 m; DDH C-10-32: 1.84 g/t Au over 34.8 m; DDH C-10-39: 2.1 g/t Au over 35.65 m; DDH C-10-49: 1.01 g/t Au over 49.9 m. Significant assays from the 2011 drill program include: DDH C-11-66: 1.10 g/t Au over 38.25 m; DDH C-11-62: 1.06 g/t Au over 16 m; DDH C-11-62: 1.04 g/t Au over 23 m, DDH C-11-71: 8.26 g/t Au from 186.5-189.85 m; DDH C-11-75: 11.65 g/t Au from 172.65-174 m and 10.95 g/t Au from 197-199 m (McCracken, 2011) .



Mineral Record Details

Classification
RankClassification            
1 Lode (Gold)
Characteristics
Rank Characteristic            
1 Sheared

Mineral Zones - Size and Shape

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 1300 75 450 90
Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
East Coldstream Open Pit 2024 Inferred Mineral Resource 5360000 Goldshore Resources news release May 8, 2023 198 Koz Au contained Gold 1.15 g/t
East Coldstream Open Pit 2024 Indicated Mineral Resource 7670000 Goldshore Resources news release May 8, 2023 307 Koz Au contained Gold 1.25 g/t
East Coldstream Underground 2024 Inferred Mineral Resource 820000 Goldshore Resources news release May 8, 2023 82 Koz Au contained Gold 3.10 g/t
East Coldstream Open Pit 2023 Inferred Mineral Resource 19800000 Goldshore Resources news release May 8, 2023 0.57 Moz Au contained Gold 0.89 g/t
East Coldstream Underground 2023 Inferred Mineral Resource 200000 Goldshore Resources news release May 8, 2023 0.01 Moz Au contained Gold 2.24 g/t
Osmani Gold Deposit 2011 Indicated Mineral Resource 3500000 Foundation Resources, Technical Report and Resource Estimate on the Osmani Gold Deposit, Coldstream Property, Northwestern Ontario 96,400 contained ounces, 0.4 g/t cut-off grade, average grade: 0.85 g/t Gold .85 Grams per Tonne
Osmani Gold Deposit 2011 Inferred Mineral Resource 30500000 Foundation Resources, Technical Report and Resource Estimate on the Osmani Gold Deposit, Coldstream Property, Northwestern Ontario 763,276 contained ounces, 0.4 g/t cut-off grade, average grade: 0.78 g/t Gold .78 Grams per Tonne
East Coldstream Property 1991 Unclassified 5107190 Osmani 2009 p. 71 7,278,762 contained ounces in 4 zones Gold 1.43 Grams per Tonne

References

MonoMap - Geology of the Burchell Lake area, District of Thunder Bay

Publication Number: R019 Page: 35  Date: 1997

Author: Giblin P.E.

Publisher Name: Ontario Dept. of Mines

Location:


Press Release - Goldshore Announces an Indicated Mineral Resource Estimate of 1,535Koz Contained Gold at 1.23 g/t Au and an Inferred Mineral Resource Estimate of 5,198Koz Contained Gold at 1.11 g/t Au at the Moss Gold Project

Publication Number: Press Release Page: Date: 2024

Author: Dufresne, M., Black, W.

Publisher Name: Goldshore Resources Inc.

Location: SEDAR


Book - Coldstream Property, West Shebandowan Greenstone Belt, Burchell Lake area, Technical report, 87p.

Publication Number: 2009 43-101 Date: 2009

Author: I.A. Osmani

Publisher Name:

Location:


Book - Technical Report and Resource Estimate on the Osmani Gold Deposit, Coldstream Property, Northwestern Ontario

Publication Number: 2011 43-101 Date: 2011

Author: McCracken, T.

Publisher Name: Wardrop for Alto Ventures and Foundation Resources

Location: SEDAR (under Coldstream Mineral Ventures


Map - Burchell Lake area, Thunder Bay District

Publication Number: M2036 Scale: 1:31,680    Date: 1997

Author: Giblin P.E.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Precambrian Geology, Burchell-Greenwater Lakes Area, West Half

Publication Number: M2622 Scale: 1:20,000    Date: 1997

Author: Osmani I.A.

Publisher Name: Ontario Geological Survey

Location:


Map - Precambrian geology, geology and mineral potential of the western Greenwater Lake area

Publication Number: OFM0202 Scale: 1:15,840    Date: 1992

Author: Osmani I.A.

Publisher Name: Ontario Geological Survey

Location:


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