Ontario Geological Survey
Permanent Link to this Record:
MDI42C13SE00013
Record Name(s) | Shuman-Daniels Zn - 1992 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1996-Nov-28 |
Date Last Modified | 2022-May-09 |
Created By | |
Revised By |
Primary Commodities: Zinc
Secondary Commodities: Copper
Township or Area: White Lake Area
Latitude: 48° 47' 28.24" Longitude: -85° 41' 11.19"
UTM Zone: 16 Easting: 596476.84 Northing: 5405074.52 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 42C13SE
Point Location Description: Small trench
Location Method: Field Visit
Access Description: The occurrence is located approximately 38 km southeast of Manitouwadge and 2.25 km northeast of the northeastern tip of Etna Lake. The occurrence is situated on the west shore of Spruce Bay opposite the mouth of the channel connecting the bay with the main body of the Lake. The occurrence is accessible via motor vehicle followed by travel in boat. From the junction of Hwys 614 and 17, proceed east along Hwy 17 for approximately 17 km to an unnamed gravel road that leads north to a public boat launch on the west shore of White Lake. Proceed northerly, via boat, along the west side of White Lake for approximately 9 km to the entrance of Spruce Bay. Proceed westerly along the south shore of the channel leading into Spruce Bay for approximately 2.25 km to the west shore of the bay. The occurrence is exposed in a small trench located in the vicinity of what G. Siragusa (Map P.2738) refers to as Gossan 33.
1964-1965: Geological mapping; ODM (V.G. Milne). 1977: Line cutting, ground geophysical surveys (MAG, CEM, VLF-EM), geological mapping; Noranda Exploration Co., Ltd. 1978-1979: Lake sediment and water geochemical sampling; GSC and MNR. Samples collected from the vicinity of the occurrence contained slightly anomalous amounts of Au. 1983: Airborne geophysical survey (HLEM, VLF-EM, MAG); Aerodat Ltd. 1984: Geological mapping; OGS (G.M. Siragusa). Siragusa noted the presence of gossanous rock in the vicinity of the occurrence. 1992-1993: Prospecting, sampling, ground geophysical survey (Beep Mat); prospectors B. Fowler, M. Shuman and M. Daniels. Sampling; OGS (D.B. Mckay), Minnova Inc., Granges Inc., Homestake Mining Corp. 1994: line cutting, ground geophysical surveys (MAG, VLF-EM, HLEM, IP); prospectors B. Fowler, M. Shuman and M. Daniels. 1996: Homestake Canada Inc. optioned the property. 1997: Homestake Canada carried out mapping and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.15209 | 42C13SE8800 | 42C13SE8800 |
2.17973 | 42C13SE2002 | 42C13SE2002 |
OP93-331 | 42F13NE2001 | 42F13NE2001 |
OP93-731 | 42C13SE0074 | 42C13SE0074 |
2.15509 | 42C13SE0001 | 42C13SE0001 |
2.17244 | 42C13SE0080 | 42C13SE0080 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Schreiber-Hemlo
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Amphibolite
Dec 07, 2005 (D McKay) - The occurrence is underlain primarily by a southeasterly-trending sequence of mafic metavolcanic rocks which comprise a portion of the north limb of the Schreiber-Hemlo greenstone belt. Thin units of felsic metavolcanic (?) and metasedimentary rocks occur locally within the mafic metavolcanic sequence. The supracrustal rocks in this area are locally strongly foliated (105 degrees/65 degrees SW) and mineral assemblages indicate they have experienced lower amphibolite facies-grade regional metamorphism. In the vicinity of the occurrence, the supracrustal sequence is approximately 3.5 km wide and is bounded to the north and south by granodioritic rocks of the Dotted Lake Batholith. The metavolcanic and metasedimentary rocks in the vicinity of the occurrence have been intruded locally by narrow felsic dikes. A large (60 m wide), north-northeasterly-trending diabase dike is located approximately 250 m west of the occurrence. An elongate (6.5 km long by 300 m wide) body of amphibolitic metagabbro is located approximately 650 m to the north, and the White Lake Fault, a regional-scale northeast-trending structure, is located approximately 800 m to the southeast. In the vicinity of the occurrence, 4 narrow (up to 30 cm wide) ,sulphide-bearing graphitic shear zones occur within the mafic metavolcanic sequence. These shear zones are subparallel to one another, occur within a 10 m wide area, strike approximately 098 degrees and dip 70 degrees to the south. The widest shear zone has been trenched and can be traced from the shore of Spruce Bay inland for approximately 6 m. The shear zones contain up to 5% sulphides.
Rock Type | Rank | Composition | Texture | Relationship | Schist-Unsubdivided | 1 | Q-Fel-Hb Schist | Sheared | Host |
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Siltstone | 2 | Near |
Dec 07, 2005 (D McKay) - The mafic metavolcanic rocks are typically dark green, fine- to medium-grained, moderately to locally strongly foliated, q-fel-hb schists and gneisses. The metasedimentary rocks are fine-grained clastic units that occur as thin (up to 1.5 m wide) beds intercalated within the metavolcanic rocks.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Sphalerite | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore | ||||
3 | Pyrite | Economic | Ore | ||||
4 | Bornite | Economic | Ore | ||||
5 | Magnetite | Economic | Ore | ||||
1 | Graphite | Economic | Gangue |
Dec 07, 2005 (D McKay) - The shear zones contain up to 5% fine- to medium-grained pyrite, chalcopyrite and sphalerite as disseminated grains, fracture-fillings, and coatings along fracture planes. Sulphides also occur within the mafic metavolcanic rocks proximal to the shear zones. Grab samples collected from the occurrence by D.B. McKay in 1992 returned assay values that varied from nil to trace Au, nil Ag, 411 to 567 ppm Cu, 24 to 111 ppm Pb and 1880 to 4040 ppm Zn.
Mar 13, 2019 (Therese Pettigrew) - The Point Zone, located at NAD83 UTM Zone 16 596462 m E, 5405185 m N, assayed up to 0.368% Zn from mafic to ultramafic flows intruded by mafic-ultramafic dykes. The Post Zone, located at NAD83 UTM Zone 16 596497 m E, 5405010 m N, assayed up to 0.853% Zn from a sulphide-bearing BIF intercalated with ferruginous siltstone (Muir, 2000). Homestake reported that a sample collected from the Post Zone assayed 8560 ppm Zn, 547 ppm Cu, 297 ppm Ni, and 18 ppm Mo from a magnetite ironstone that contains 2-5% disseminated and blebby pyrite, bornite, chalcopyrite, and sphalerite (Assessment file 42C13SE2002).
Rank | Classification |
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1 | Hydrothermal |
Rank | Characteristic |
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1 | Disseminated |
2 | Sheared |
Map - Geophysical Series, White Lake, Thunder Bay District, Ontario
Publication Number: Map 2168G Scale: 1:63,360 Date: 1963
Author: Geological Survey of Canada
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/116493
MonoMap - Geology of the Black River area, District of Thunder Bay
Publication Number: R072 Date: 1968
Author: Milne V.G.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Manitouwadge-Wawa sheet, geological compilation series, Algoma, Cochrane, Sudbury and Thunder Bay districts
Publication Number: M2220 Scale: 1:253,440 Date: 1972
Author: Milne V.G., Giblin P.E., Bennett G., Thurston P.C., Wolfe W.J., Giguere J.F., Leahy E.J., Rupert R.J.
Publisher Name: Ontario Division of Mines
Location:
Book - National Geochemical Reconnaissance Release NGR 35-1978, Regional Lake Sediment and Water Geochemical Reconnaissance Data, Ontario Eastern Shore, Lake Superior
Publication Number: OF 555 Date: 1979
Author: Hornbrook, E.H.W., Coker, W.B., Lynch, J.J.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129524
Map - White Lake sheet, Thunder Bay District
Publication Number: M2147 Scale: 1:31,680 Date: 1968
Author: Milne V.G.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geological series, Precambrian geology, Lumby Lake area, western part, Kenora District
Publication Number: P2828 Scale: 1:15,840 Date: 1985
Author: Jackson M.C., Chevalier P.
Publisher Name: Ontario Geological Survey
Location:
Book - Regional Lake Sediment and Water Geochemical Reconnaissance Data, Northwestern Ontario
Publication Number: OF 2362 Date: 1979
Author: Friske, P.W.B., Hornbrook, E.H.W., Lynch, J.J., McCurdy, M.W., Gross, H.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/132202
Map - Geological Compilation of the Eastern Half of the Schreiber-Hemlo Greenstone Belt
Publication Number: M2614 Scale: 1:50,000 Date: 2000
Author: Muir T.L.
Publisher Name: Ontario Geological Survey
Location:
File - Schreiber-Hemlo Resident Geologist Mineral Deposit Files
Publication Number: Min Dep Date:
Author:
Publisher Name:
Location: Thunder Bay RGP
Compend - Report of Activities 1992, Resident Geologists
Publication Number: MP161 Page: 149-151 Date: 1993
Author: Fenwick K.G., Pitts A.E., Newsome J.W.
Publisher Name: Ontario Geological Survey
Location:
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