Ontario Geological Survey
Permanent Link to this Record:
MDI41O16SW00053
Record Name(s) | Leith Zone 1 - 1907, C. K. Leith Estate Claims W.S. 11 and 12 - 1907, Woman River Iron Belt 1 - 1909 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1999-Nov-15 |
Date Last Modified | 2023-Mar-27 |
Created By | |
Revised By |
Primary Commodities: Iron
Township or Area: Heenan
Latitude: 47° 45' 44.78" Longitude: -82° 23' 39.04"
UTM Zone: 17 Easting: 395525 Northing: 5290837.99 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41O16SW
Point Location Description: Prescise: Intersection of linear IF outcrop on Map 2067 and east border of Pat. WS 12
Location Method: Data Compilation
Access Description: Easy access to the area is now possible via a secondary forestry road that extends east from the Heenan Township road. This access road in turn connects with the Dore road just north of the Wakami River.
1906-07: Leith and van Hise carried out staking, trenching, sampling (T-4274; trench locations now unknown). Algoma Ore carried out sampling and evaluation. (GR 38, pp. 47-48). 1965-66: W. G. Wahl completed a ground magnetic survey, mapping, and bulk sampling. (T-2311). 1975: U. S. Steel International / W.G. Wahl completed a VLF-EM survey (T-2311). 1991: G.M. Archibald carried out reconnaissance mapping (T-3661). 2006: VenCan Gold Corporation carried out an airborne geophysical survey (T-5418).
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-5418 / 2.33014 | 20000001584 | 20000001584 |
T-2311 / 2.2085 | 41O16SW9149 | 41O16SW9149 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Tectonic Assemblage: Marion
Geological Age: Neoarchean Geochronological Age: 2729 +/- 5 MA Geochron. Age Ref.: OF 3384C
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
May 29, 2019 (A Wilson) - The banded iron formation is found at the contact between underlying pyroclastic rocks and overlying intermediate to mafic flow rocks. Porphyry sills and dikes and younger diabase dikes transect these rocks.
Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Host |
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Felsic Tuff-Breccia | 2 | Rhyolite | Tuff, Breccia | Footwall |
Mafic pillowed flow | 3 | Basalt To Andesite | Pillowed | Hanging Wall |
Feb 10, 2010 (A Wilson) - White to pink rhyolite breccia predominates as the foot wall of the iron formation. The iron formation is composed of chert, jasper and magnetite with siderite and pyrite locally. The iron content is notably higher at the base of the iron formation in contact with the felsic metavolcanics. Andesitic to basaltic flows containing well-developed pillow structures conformably overlie the banded iron formation. Coarse-grained dioritic phases, as well as granitic sills and dikes, are locally present.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Magnetite | Economic | Ore | ||||
2 | Chert | Economic | Gangue | ||||
3 | Hematite | Economic | Gangue | ||||
4 | Jasper | Economic | Gangue |
Feb 10, 2010 (D Draper) - Zone No. 1 is 30-60 ft wide by 300-700 ft long and is composed of chert, siliceous magnetite and hematite. It contains up to 56% Fe locally, with an average of 30% Fe, 0.018% P and 0.9% S. (GR 38 , p. 49)
Rank | Classification |
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1 | Sedimentary |
Rank | Characteristic |
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2 | Fault |
1 | Layered |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Unknown | 152 | 15 |
File - Resident Geologist files T-2311, T-3661 (OP91-607), T-4274
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Part - Iron Formation of Woman River Area
Publication Number: ARV18-01.008 Page: 254-262 Date: 1998
Author: Allen R.C.
Publisher Name: Ontario Bureau of Mines
Location:
Publication - Iron ore occurrences in Canada; Canada Mines Branch, Publication 217
Publication Number: CMB Pub 217 Page: 91-92 Date: 1917
Author: Lindeman, M E; Bolton, L L; Robinson, A H A
Publisher Name: Canada Mines Branch
Location: https://doi.org/10.4095/305364
Mono - Report Of The Ontario Iron Ore Committee With Appendix 1923
Publication Number: NSP013 Page: 202 Date: 1998
Author:
Publisher Name:
Location:
Part - Geology of the Swayze area
Publication Number: ARV41-03.002 Page: 48-51 Date: 1998
Author: Furse G.D.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of Heenan and Marion townships and the northern part of Genoa Township, District of Sudbury
Publication Number: R038 Page: 15, 22-25, 46-49 Date: 1997
Author: Goodwin A.M.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Heenan, Marion and northern part of Genoa townships, Sudbury District
Publication Number: M2067 Scale: 1:31,680 Date: 1997
Author: Goodwin A.M., Donovan J.F.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Iron deposits of Ontario
Publication Number: MDC011 Page: 338-339 Date: 1968
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
Publication - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Date: 1985
Author: Rose, D.G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
Book - Heenan Township - unpublished GDIF
Publication Number: GDIF Date: 1987
Author: Resident Geologist Staff
Publisher Name:
Location: Timmins RGP office
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: 321-322 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
Map - Geology, Swayze greenstone belt, Rush Lake, Ontario
Publication Number: OF3384c Scale: 1:50,000 Date: 1999
Author: Heather, K B; Shore, G T
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/210451
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