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Shebandowan Mine

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Journal Article
Published: 01 November 1978
The Canadian Mineralogist (1978) 16 (4): 659–663.
Series: Reviews in Economic Geology
Published: 01 January 2011
DOI: 10.5382/Rev.17.03
EISBN: 9781629490243
... by Stott et al. ( 2007 ), showing the location of the Abitibi greenstone belt (1), and the Shebandowan greenstone belt (2). The Superior province is shown as the shaded gray in the inset (after Stott and Mueller, 2009 ). F ig . 2. Distribution of major nickel discoveries, mining operations...
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Journal Article
Journal: Economic Geology
Published: 01 June 2013
Economic Geology (2013) 108 (4): 895–907.
... is hosted in ultramafic rocks at the base of, or just below, the sill (e.g., past-producing Maskwa-Dumbarton mines). In this study, we report a U-Pb age (chemical abrasion-thermal ionization mass spectrometry) for a leucogabbro from the Chrome property of 2743.0 ± 0.5 Ma (n = 8 single grains of zircon...
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Journal Article
Published: 02 February 2015
Canadian Journal of Earth Sciences (2015) 52 (3): 196–214.
... Shebandowan Ni–Cu mine (8.34 Mt at 2.00% Ni, 1.2% Cu, 3.96 g/t of platinum group elements (PGE); Morton 1982 ; Lavigne et al. 1990 ). A substantial, differentiated gabbroic complex has also been dated at ca. 2720 Ma ( Corfu and Stott 1998 ) and is associated with several base metal showings (e.g., Farrow...
Journal Article
Published: 20 February 2004
Canadian Journal of Earth Sciences (2004) 41 (2): 217–235.
... and Wawa subprovinces, south of the Beardmore–Geraldton Belt. Gold mineralization at the Leitch and MacLeod-Cockshutt mines, the two richest past-producing gold mines in the Beardmore–Geraldton Belt, is associated with D3 shear zones and folds, overprinting regional F2 folds. The plunge of the ore zones...
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Journal Article
Published: 01 April 2000
Canadian Journal of Earth Sciences (2000) 37 (1): 1–15.
... characteristics of the Midway sequence are generally similar to those of the Timiskaming Group and Timiskaming-type rocks in Canada, and more specifically to those of the Shebandowan Group in the Thunder Bay district. This similarity implies that the latest Archean tectonic and magmatic history of the western...
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Journal Article
Journal: Economic Geology
Published: 01 August 2014
Economic Geology (2014) 109 (5): 1291–1313.
...), Pick Lake (1.3 Mt at 16.5% Zn, 0.9% Cu), and Zenith (0.16 Mt at 16.5% Zn) Zn-rich volcanogenic massive sulfide (VMS) orebodies (e.g., Severin et al., 1991 ) and several Au prospects in the Big Duck Lake area (e.g., MacDonald, 2003 ). Exploration and mining activities prompted and facilitated academic...
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Journal Article
Published: 24 January 2007
Canadian Journal of Earth Sciences (2006) 43 (11): 1751–1753.
... program. Initial interpretation of KIM distribution in the Lac de Gras region was of a regional-scale dispersal plume characterized by relatively long distance dispersal (high erosion length scale) from the initial discoveries in the Ekati and Diavik Mine areas (see Ward and others 1996 ). In the authors...
Journal Article
Published: 01 January 2003
Exploration and Mining Geology (2003) 12 (1-4): 37–47.
... in the following. Prior to the development of the mines, Atikokan was a small CNR hamlet with a population of about 300. There was no proper provincial highway to Atikokan. The nearest road was Highway No. 11, which extended west from Thunder Bay to Shebandowan, 136 km east of Atikokan (Fig. 1...
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Image
Simplified geology of the Bird River Belt showing the location of the Bird ...
Published: 01 June 2013
, National Ledin, Poplar Bay [Wards]), each of which contains chromitite layers in the ultramafic portions of the sill (except Wards, stratiform chromitite hosted in gabbro). Associated Ni-Cu-(PGE) deposits that occur along the base of the sill (Dumbarton, Maskwa, Ore Fault) and the Tanco rare element mine
Journal Article
Published: 08 August 2007
Canadian Journal of Earth Sciences (2007) 44 (8): 1041–1053.
...., www.landore.com/junior-lake.htm , accessed 9 July 2007) and the Shebandowan Mine in the Shebandowan belt, west of Thunder Bay (8.64 million tonnes mined, grading 1.92% Ni, 0.98% Cu, 2.62 g/t Pt + Pd; Resident Geologist’s Files, Thunder Bay South District, Thunder Bay). In the Obonga Lake belt, the Core Zone...
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Journal Article
Published: 01 November 2010
Geochemistry: Exploration, Environment, Analysis (2010) 10 (4): 391–399.
...Peter J. Barnett; Stuart Averill Abstract ABSTRACT Till sampling near the Lac des Iles Pd mine north of Thunder Bay, Ontario, Canada has led to the identification of heavy mineral dispersal trains in till as unique as the local Pd deposits. The till at Lac des Iles was deposited by ice actively...
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Journal Article
Published: 01 November 2007
The Journal of Geology (2007) 115 (6): 655–674.
... Ma from a porphyry stock (Davis 2002 ) Fault-bounded; unconformity with turbidite deposits; composed of conglomerate, sandstone, siltstone, mudstone, felsic volcaniclastic rocks, and porphyry stocks Rocheleau 1980 ; Diop et al. 2006 Wawa Subprovince:  Shebandowan Basin U-Pb zircon...
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Journal Article
Published: 01 May 2011
Geochemistry: Exploration, Environment, Analysis (2011) 11 (2): 145–159.
... ; Cook & Fletcher 1993 ; Bajc & Hall 2000 ; Searcy 2001 ; Barnett 2007 ) and even fewer that also document Ni–Cu–PGE indicator mineral signatures. To address this knowledge gap, the Geological Survey of Canada (GSC) in collaboration with the Canadian Mining Industry Research Organization...
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Journal Article
Journal: Economic Geology
Published: 01 May 2010
Economic Geology (2010) 105 (3): 669–688.
... press release, Mengold resources citing production and Ni and Cu grades of Shebandowan from 1971–1998, along with Pd/Ni and Pt/Ni ratios for the adjacent Shebandowan West deposit, which have been extended to Shebandowan; Langmuir 1 and 2: Tons mined and Ni grade from Inspiration Mining website (March 5...
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Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 51–67.
.... Plutons intruded into an actively deforming crust and were probably also the heat source for regional metamorphism. The most likely environment was a tectonically active, Timiskaming-type sedimentary basin. Similarly aged basins are found in the Timmins area to the east and the Shebandowan greenstone belt...
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Journal Article
Published: 31 March 2003
Canadian Journal of Earth Sciences (2003) 40 (3): 395–430.
... plane. The four HGD shafts, from west to east, are Williams mine main (B zone), Williams mine A zone (defunct), Golden Giant mine, and David Bell mine. Primary features in mafic volcanic flows are rarely preserved but may include variably deformed plagioclase phenocrysts, varioles...
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Journal Article
Published: 01 April 2000
The Canadian Mineralogist (2000) 38 (2): 287–317.
... event. Major greenstone belts subjected to low-grade metamorphism include the Mishibishu, Michipicoten and Gamitagama belts in the east, and the Shebandowan and Vermillion belts in the west. All exhibit a metamorphic zonation similar to that observed in other granite–greenstone subprovinces...
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Journal Article
Published: 01 November 2011
Geochemistry: Exploration, Environment, Analysis (2011) 11 (4): 279–291.
... to avoid surface sediment potentially containing wind-blown mineral contamination from mining or drilling activity. A few surveys were conducted in humid tropical rather than arid regions and utilized gravel samples from active streams. All of the samples were supplied by mining companies conducting...
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Journal Article
Published: 01 September 2006
Canadian Journal of Earth Sciences (2006) 43 (7): 749–765.
... . Corfu F, Stott G.M. 1998 . Shebandowan greenstone belt, western Superior Province: U–Pb ages, tectonic implications, and correlations . Geological Society of America Bulletin , 110 : 1467 – 1484 . Corfu F. Jackson S.L. Sutcliffe R.H. 1991 . U–Pb ages and tectonic...
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