Ontario Geological Survey
Permanent Link to this Record:
MDI41O09NE00005
Record Name(s) | Little Rush River - 1980, Canoe Lake - 1968, Best Ore DDH W-1 - 1948, Siragusa #28 - 1993, Siragusa #24 - 1993 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1994-May-31 |
Date Last Modified | 2022-Sep-27 |
Created By | |
Revised By |
Primary Commodities: Zinc, Iron
Secondary Commodities: Gold
Township or Area: Huffman
Latitude: 47° 35' 12.22" Longitude: -82° 6' 35.51"
UTM Zone: 17 Easting: 416550.48 Northing: 5270965.02 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41O09NE
Point Location Description: A trench on the northern iron formation near Camp Lake.
Location Method: Field Visit with GPS
Access Description: The various locations are easily accessed via a number of secondary roads at the end of the New Arbutus logging road which branches off the Sultan Industrial road.
1907: Mr. Leith explored the iron formations in the area for their iron potential on behalf of other interests. 1948: Best Ore Mines carried out a 12 hole drill program in Huffman and Arbutus Townships. Apparently this was follow up work in a gold exploration program. A number of holes were located to test the banded iron formation which forms this prospect. No assays are on file. 1980: Hargor Resources carried out a regional airborne magnetic and electromagnetic survey which covered the area. 1988: Bryndon Ventures assumed control of the ground to the east and carried out a till sampling program over the iron formation and which returned a number of anomalous samples west of Canoe Lake. 1990: Blue Falcon flew a second regional magnetic and electromagnetic survey which covered the area. 2007-2008: Augen Gold Corp. performed an aerial electromagnetic, aeromagnetic and aero-radiometric survey; prospecting, sampling, assays
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-5671 / 2.37373 | 20000002805 | 20000002805 |
T-5852 / 2.40516 | 20000003874 | 20000003874 |
T-2001 / | 41O09SE0515 | 41O09SE0515 |
T-3020 / 2.11518 | 41O09SE0002 | 41O09SE0002 |
T-2357 / 2.3559 | 41O09NW9161 | 41O09NW9161 |
T-3020 / 63.4895 | 32D05NW0010 | 32D05NW0010 |
T-2001 / | 41O09SE0031 | 41O09SE0031 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Tectonic Assemblage: Ridout
Geological Age: Neoarchean Geochronological Age: 2700 MA Geochron. Age Ref.: OF 3384F
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (S Fumerton) - Though some attenuation and tectonic shortening is apparent in the banded iron formation, generally the unit is characterized by a low state of strain except for the amphibole facies where present which tends to be schistose.
Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Banded Iron Formation | Contains |
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Conglomerate | 2 | Conglomerate | Contains |
Dec 07, 2005 (S Fumerton) - There are a number of banded iron formations in the area which are intercalated with pillowed mafic volcanics, coarser mafic flows. The banded iron formation range from several metres up to 10m thick. In the vicinity of the iron formations, the sequence is also locally intruded by coarse, parallel dykes which form part of the Keweenawan Trend. A number of conglomerate horizons and minor porphyry sills were intersected in drill core but not observed in outcrop. The iron formations are variable. They range from:- 1) lean laminated cherts with trails of magnetite intercalated with graphitic mudstones / schists and fine sand arenaceous rocks, 2) thin chert beds intercalated with brown carbonate beds and containing some hematite with trace manganite in cavities, 3) amphibole rich silicate facies lamellae together with chert.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Magnetite | Economic | Gangue | ||||
2 | Hematite | Economic | Gangue | ||||
3 | Manganite | Economic | Gangue | ||||
4 | Pyrite | Economic | Gangue |
Jun 27, 2016 (S Fumerton) - Disseminated pyrite locally forms up to 10% of the amphibole rich silicate facies iron formation. Otherwise only rare sulphides occur along fractures within the banded iron formation.
Dec 07, 2005 (A Wilson) - Grab samples collected by the OGS in 1994 returned values of: 0.01 g/t Au, 0.8 g/t Ag; 0.01 g/t Au, 0.5 g/t Ag; 0.17 g/t Au and 0.5 g/t Ag. A diamond drill hole (GOG-5) intersected a 2-foot long section of schist assaying 0.16% Zn, 0.03 %Cu, 0.5 g/t Ag and 0.05 g/t Au.
Nov 15, 2011 (P Bousquet) - A rock sample taken by Augen Gold Corp returned an assay of 5220 ppm Zn (T-5852 / 2.40516).
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Copper | Unknown | .0266 | % | |||
Copper | Unknown | .0434 | % | |||
Copper | Unknown | .0172 | % | |||
Gold | Unknown | .17 | ppm | |||
Gold | Unknown | .01 | ppm | |||
Gold | Unknown | .01 | ppm | |||
Lead | Unknown | .0035 | % | |||
Lead | Unknown | .0022 | % | |||
Lead | Unknown | .0032 | % | |||
Molybdenum | Unknown | .0002 | % | |||
Molybdenum | Unknown | .0001 | % | |||
Molybdenum | Unknown | .0003 | % | |||
Nickel | Unknown | .0024 | % | |||
Nickel | Unknown | .0031 | % | |||
Nickel | Unknown | .004 | % | |||
Silver | Unknown | .8 | ppm | |||
Silver | Unknown | .5 | ppm | |||
Silver | Unknown | .5 | ppm | |||
Zinc | Unknown | .157 | % | |||
Zinc | Unknown | .22 | % | |||
Zinc | Unknown | .0229 | % |
Rank | Classification |
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1 | Sedimentary |
Rank | Characteristic |
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1 | Stratabound |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Tabular | 10 | 100 | 90 | N/A | N/A |
Map - Geological series, Jerome area (east), District of Sudbury
Publication Number: P2370 Scale: 1:15,840 Date: 1980
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
Publication - Preliminary report on Woman river and ridout map areas, Sudbury district, Ontario
Publication Number: Memoir 157 Page: 26-27 Date: 1929
Author: Emmons, R C; Thomson, E
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/100840
Book - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Page: 51 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
Map - Precambrian Geology, Huffman Township and Part of Arbutus Township
Publication Number: OFM0212 Scale: 1:15,840 Date: 1993
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
Map - Geology, Swayze greenstone belt, Opeepeesway Lake, Ontario
Publication Number: OF3384f Scale: 1:50,000 Date: 1999
Author: Heather, K B; Shore, G T
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/210454
Part - Geology of the Three Duck lakes area
Publication Number: ARV41-03.001 Page: 25 Date: 1998
Author: Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology of the Opeepeesway Lake area
Publication Number: ARV44-07.001 Page: 9 Date: 1997
Author: Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Iron deposits of Ontario
Publication Number: MDC011 Page: 341 Date: 1968
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Chapleau area, districts of Algoma, Sudbury, and Cochrane
Publication Number: R157 Date: 1977
Author: Thurston P.C., Siragusa G.M., Sage R.P.
Publisher Name: Ontario Division of Mines
Location:
MonoMap - Geology, Geochemistry and Mineralization of the Southern Margin of the Swayze Belt
Publication Number: OFR5844 Page: 77 Date: 1993
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Mineral Prospects of the Swayze Greenstone Belt (Volume 1, Parts of NTS 41 O and Volume 2, Parts of NTS 41 P, 42 A and 42 B)
Publication Number: OFR5912 Page: 325-26 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
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