Ontario Geological Survey
Permanent Link to this Record:
MDI41O16SE00010
Record Name(s) | Jefferson Iron Mine - 1910, Lucky Creek - 1980, Smith Claims - 1908, Central Sudbury - 1947, Stackpool - 1957 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Prospect |
Date Created | 1992-Sep-02 |
Date Last Modified | 2022-Sep-23 |
Created By | |
Revised By |
Primary Commodities: Zinc, Lead, Silver, Iron
Secondary Commodities: Gold, Cadmium
Township or Area: Genoa
Latitude: 47° 50' 6.02" Longitude: -82° 12' 10.65"
UTM Zone: 17 Easting: 409979.72 Northing: 5298662.61 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41O16SE
Point Location Description: Pit within a 50m long trench on a southern crest of a ridge.
Location Method: Field Visit with GPS
Access Description: Access is difficult and involves a circuitous road trip using the Sultan access road from Highway 144, then driving along the Mallard forest access road to the old trail to Rush Lake. This trail is a 4x4 trail and is 7km to the landing at Rush Lake. From the landing a boat must be taken up the length of Rush Lake to a bay on the northwest shore. Then from this point the showing is a 2km traverse along a well marked trail and down a grid line. Alternatively secondary forestry roads at the southern end of the Kenogaming Main Haul road come within 2km of the eastern end of Falconbridge grid about 2km from the showing.
1908:Smith - discovery of iron formation. 1910-12: Jefferson Mining Corporation - diamond drilling, trenching, prospecting. 1928: Century Zinc - 10 ddh . 1929: Canam Metals - 4 ddh. 1929: Oliver Iron Mining Company - prospecting. 1950: Sudbury Lead-Zinc Mines - 23 ddh. 1957: Stackpool Mining - EM survey, 13 ddh (1063m). 1978: Texasgulf Canada - HLEM and VLF-EM surveys, mag survey. 1978: Noranda Exploration - mapping, mag and HLEM surveys. 1980-83: Falconbridge Exploration - VLF-EM, mag surveys, lithogeochemical surveys, stripping, mapping. 1992: Falconbridge Exploration - mapping, ground geophysics, diamond drilling. 2006: Vencan Gold Corp. – Aerial electromagnetic and magnetic survey, geochemical survey, assays, DD, sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-1888 / 2.2955 | 41P16SE0021 | 41P16SE0021 |
T-2083 / | 41O16SE0026 | 41O16SE0026 |
T-2345 / 2.5994 | 41O16SE0017 | 41O16SE0017 |
T-2345 / 2.5182 | 41O16SE0450 | 41O16SE0450 |
T-2345 / 2.5183 | 41O16SE0019 | 41O16SE0019 |
T-2345 / 2.2053 | 41O16SE0027 | 41O16SE0027 |
T-2345 / | 41O16SE9057 | 41O16SE9057 |
T-2345 / 2.15108 | 41O16SE9070 | 41O16SE9070 |
T-2345 / 2.14949 | 41O16SE9058 | 41O16SE9058 |
T-1888 / 2.2730 | 41P16SE0023 | 41P16SE0023 |
T-2345 / 2.14747 | 41O16SE0004 | 41O16SE0004 |
T-2083 / | 41O16SE0025 | 41O16SE0025 |
T-1908 / 2.2826 | 41P16SE0022 | 41P16SE0022 |
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
Rock Type | Rank | Composition | Texture | Relationship | Sulphide Ironstone | 1 | Sulphide-Facies | Banded Iron Formation | Host |
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Felsic lava flow-unsubdivided | 2 | Rhyolite | Pyroclastics, Breccia, Flows | Footwall |
Mafic pillowed flow | 3 | Tholeiitic Basalt | Pillowed | Hanging Wall |
Porphyry-unsubdivided | 4 | Near |
Dec 07, 2005 (S Fumerton) - The mineralization is hosted in the Woman River banded iron formation. Regionally this iron formation is composed of vary proportions of chert, jasper, magnetite, hematite, sulphide, silicate, and carbonate. The sulphide facies are more dominant in the northeast in the vicinity of the showing especially where sulphides occur in the underlying felsic metavolcanic. Locally garnet porphyroblasts occur in the amphibole rich horizons. Underlying the iron formation is a sequence of felsic metavolcanics primarily composed of flow breccias, pyroclastics and minor massive flows. These rocks have been subjected to chlorite and sericite alteration. Immediately underlying the sulphide facies iron formation and about 100m northeast of the showing is a wedge of felsic debris breccias. Overlying the iron formation is an altered tholeiitic sequence of pillowed and massive basaltic flows. Alteration is dominantly carbonate with some sericite/biotite. Feldspar porphyry dykes have been intersected in drill core in the vicinity of the showing. Also thin fine grained felsic veinlets with disseminated pyrite cut the iron formation at shallow angles.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Galena | Economic | Ore | ||||
2 | Sphalerite | Economic | Ore | ||||
3 | Magnetite | Economic | Ore | ||||
1 | Chalcopyrite | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue | ||||
3 | Pyrrhotite | Economic | Gangue | ||||
Chlorite | Alteration | Chloritic | 1 | Medium | Replacement | ||
Sericite | Alteration | Potassic | 2 | Medium | Replacement | ||
Quartz | Alteration | Silicification | 3 | Weak | Replacement |
Dec 07, 2005 (S Fumerton) - Mineralization varies between near pure sections of massive galena in the centre of the main trench with higher proportions of sphalerite along the margins and the known lateral limits. Chalcopyrite occurs together with sphalerite and galena in bands within the iron formation along strike 15m east of the main pit. Fine disseminated sphalerite has been observed in the chert horizons within the iron formation. This sphalerite is not associated with other sulphides and locally forms discontinuous trails partially concentrated along one contact. Similarly in the amphibole rich beds fine grained pyrite is concentrated along one contact. Within the feldspar porphyry there are trace amounts of very fine grained galena disseminated in the matrix.
Dec 07, 2005 (A Wilson) - Grab samples of the iron formation returned assays ranging from 35.9 to 41.28% in the magnetite iron formation. Samples from the pyritic section returned values of 20.15 to 29.00% Fe. A high grade sample taken in 1908 assayed 73% Pb and 6% Zn. Grab samples taken by the OGS in 1970 returned vlaues of 2.88% Pb, 6.7% Zn;0.6 g/t Au, 24 g/t Ag, 43.5% Pb, 0.26% Zn; 6.2g/t Ag, 0.37% Pb, 0.68% Zn. Grab samples taken by the OGS in 1992 returned values of 37.72% Pb, 7.16% Zn; 0.36% Pb, 0.06% Zn.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Cadmium | Unknown | .07 | % | |||
Cadmium | Unknown | .1 | % | |||
Copper | Unknown | .1376 | % | |||
Copper | Unknown | .0113 | % | |||
Copper | Unknown | .71 | % | |||
Copper | Unknown | .008 | % | |||
Gold | Unknown | BDL | ||||
Gold | Unknown | BDL | ||||
Gold | Unknown | .3 | ppm | |||
Gold | Unknown | BDL | ||||
Gold | Unknown | BDL | ||||
Gold | Unknown | .6 | ppm | |||
Gold | Unknown | 0 | ppm | BDL | ||
Gold | Unknown | BDL | ||||
Gold | Unknown | BDL | ||||
Gold | Unknown | .3 | ppm | |||
Lead | Unknown | 2.88 | % | |||
Lead | Unknown | 3.15 | % | |||
Lead | Unknown | .0431 | % | |||
Lead | Unknown | BDL | ||||
Lead | Unknown | BDL | ||||
Lead | Unknown | 45.3 | % | |||
Lead | Unknown | 37.72 | % | |||
Lead | Unknown | 19.5 | % | |||
Lead | Unknown | .63 | % | |||
Lead | Unknown | .37 | % | |||
Lead | Unknown | .36 | % | |||
Nickel | Unknown | .0088 | % | |||
Nickel | Unknown | .0098 | % | |||
Nickel | Unknown | .0096 | % | |||
Silver | Unknown | 6.2 | ppm | |||
Silver | Unknown | 0 | ppm | BDL | ||
Silver | Unknown | BDL | ||||
Silver | Unknown | BDL | ||||
Silver | Unknown | BDL | ||||
Silver | Unknown | 7.5 | ppm | |||
Silver | Unknown | BDL | ||||
Silver | Unknown | 38.4 | ppm | |||
Silver | Unknown | BDL | ||||
Silver | Unknown | 24 | ppm | |||
Zinc | Unknown | .25 | % | |||
Zinc | Unknown | .1 | % | |||
Zinc | Unknown | 6.7 | % | |||
Zinc | Unknown | .064 | % | |||
Zinc | Unknown | .68 | % | |||
Zinc | Unknown | 7.16 | % | |||
Zinc | Unknown | 10.5 | % | |||
Zinc | Unknown | .026 | % | |||
Zinc | Unknown | 3.24 | % | |||
Zinc | Unknown | .26 | % | |||
Zinc | Unknown | 26.1 | % |
Rank | Classification |
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2 | Exhalative |
1 | Sedimentary |
Rank | Characteristic |
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1 | Stratiform |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Tabular | 100 | 12 | 30 | 85 | 80 | N/A | N/A |
Date: Aug 26, 1992
Geologist: S Fumerton
Notes: The showing was visited together with Marc Leroux (MNDM) while visiting the Falconbridge Exploration camp on the Rush river. The showing is located on a grid line L168E at 49+50N on the present Falconbridge grid. This line follows various other cut lines some of which are very old. At the showing there are a series of trenches that follow the stratigraphy, a few trenches across the stratigraphy and some old diamond drill casing. Old AX core is stacked in three piles which are now overgrown with moss. There are no markers on the core and the boxes are falling apart. More recently this core in the upper boxes has been resampled in various ways, 1) composite samples collected in double 20cm wide swaths across the boxes, 2) composite samples collected by selecting alternate pieces of split core.
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
---|---|---|---|---|---|---|
Jefferson | 1928 | Possible | 91000 | based on 10 closely spaced drill holes | Lead 3.3 Percent, Zinc 4.6 Percent |
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: 145 Date: 1985
Author: Rose, D.G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
File - Resident Geologist files T-2158
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
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:
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
Part - Sahkatawich (Rush) Lake section, Woman River iron range, District of Sudbury
Publication Number: ARV35-02.003 Page: 94-96 Date: 1998
Author: Moore E.S.
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: 51, 54-55 Date: 1997
Author: Goodwin A.M.
Publisher Name: Ontario Dept. of Mines
Location:
Book - A Lead and Zinc Deposit in Keewatin Iron Formation, p. 371-378
Publication Number: CIM No. 167 Page: 371-378 Date: 1926
Author: Moore, E.S.
Publisher Name: CIM
Location: Timmins RGO
MonoMap - Geology of the Chapleau area, districts of Algoma, Sudbury, and Cochrane
Publication Number: R157 Page: 160 Date: 1977
Author: Thurston P.C., Siragusa G.M., Sage R.P.
Publisher Name: Ontario Division of Mines
Location:
Publication - Mineral deposits of the eastern part of Rush River map-area, Woman River district, Ontario; Geological Survey of Canada, Summary Report 1928, pt. C
Publication Number: SR 1928-C Date: 1930
Author: Bannerman, H.M.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/102074
Publication - Mineral occurrences in Woman River district, Ontario; Geological Survey of Canada, Summary Report 1929, pt. C
Publication Number: Sum Rep 1929 C Date: 1930
Author: Bannerman, H M
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/102021
Publication - Rush Lake area, Sudbury District, Ontario; Geological Survey of Canada, Summary Report 1933, pt. D
Publication Number: SR33-D Date: 1934
Author: Bannerman
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/102113
Mono - Copper, nickel, lead, and zinc deposits in Ontario
Publication Number: MDC001 Page: 48 Date: 1954
Author: Thomson J.E., Carlson H.D., Ferguson S.A., Pye E.G., Savage W.S.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Copper, nickel, lead and zinc deposits in Ontario (revised to February, 1957)
Publication Number: MDC002 Date: 1957
Author: Thomson J.E., Ferguson S.A., Johnston W.G.Q., Pye E.G., Savage W.S., Thomson R.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Copper, nickel, lead and zinc deposits of Ontario
Publication Number: MDC012 Page: 245 Date: 1969
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
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: 246-249 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
Folio - Genoa Township - unpublished GDIF
Publication Number: GDIF Date: 1986
Author: Resident Geologist Staff
Publisher Name: Ontario Geological Survey
Location: Timmins RGO
Mono - Report Of The Ontario Iron Ore Committee With Appendix 1923
Publication Number: NSP013 Page: 201-202 Date: 1998
Author:
Publisher Name:
Location:
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