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Selbaie Deposits

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Journal Article
Published: 01 July 2000
Exploration and Mining Geology (2000) 9 (3-4): 189–214.
...MEHMET F. TANER Abstract “Les Mines Selbaie” is a large, generally low-grade, polymetallic (Zn, Cu, Ag, Au) “giant” volcanic-associated ore deposit in the Harricana-Turgeon belt, which is part of the northern Abitibi Subprovince of Quebec. Economically recoverable mineralization occurred in three...
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Journal Article
Journal: Economic Geology
Published: 01 October 1993
Economic Geology (1993) 88 (6): 1460–1482.
...John E. Larson; Richard W. Hutchinson Abstract The Selbaie deposits of western Quebec are hosted in calc-alkalic pyroclastic rocks of the Abitibi subprovince. Rocks range upward from subaqueous debris flows through pumiceous tuff to densely welded ignimbrite; they form an intracaldera sequence over...
Image
Simplified geology of the Selbaie deposits area, showing sub-surface location of undifferentiated sedimentary rocks [zone of volcano-tectonic subsidence (see Fig. 4)] with distribution of stromatolite-bearing carbonates (mostly in blocks), massive pyrite-carbonate and chert (ch) zones and location of a probable synvolcanic fault, related to Lens 2 of the A2 Zone (see Fig. 10).
Published: 01 July 2000
Fig. 9. Simplified geology of the Selbaie deposits area, showing sub-surface location of undifferentiated sedimentary rocks [zone of volcano-tectonic subsidence (see Fig. 4 )] with distribution of stromatolite-bearing carbonates (mostly in blocks), massive pyrite-carbonate and chert (ch) zones
Image
Regional geology of the Harricana-Turgeon belt (after Remick, 1969; Lacroix, 1994; Lacroix and Sawyer, 1995) and locations of main volcanic centers and ore deposits, including the polymetallic Selbaie deposits and the stromatolite occurrence at Joutel. I3 is a maficultramafic sill lying south of Selbaie.
Published: 01 July 2000
Fig. 2. Regional geology of the Harricana-Turgeon belt (after Remick, 1969; Lacroix, 1994; Lacroix and Sawyer, 1995 ) and locations of main volcanic centers and ore deposits, including the polymetallic Selbaie deposits and the stromatolite occurrence at Joutel. I3 is a maficultramafic sill
Image
Schematic diagram summarizing the lateral and vertical sequences of alteration facies relative to mineralization at the Selbaie deposit. Abbreviations as in Fig. 3.
Published: 13 February 2007
Fig. 5. Schematic diagram summarizing the lateral and vertical sequences of alteration facies relative to mineralization at the Selbaie deposit. Abbreviations as in Fig.  3 .
Journal Article
Published: 13 February 2007
Canadian Journal of Earth Sciences (2006) 43 (12): 1877–1885.
...Fig. 5. Schematic diagram summarizing the lateral and vertical sequences of alteration facies relative to mineralization at the Selbaie deposit. Abbreviations as in Fig.  3 . ...
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Journal Article
Journal: Economic Geology
Published: 01 October 1993
Economic Geology (1993) 88 (6): 1341–1358.
... N /Yb N = 1-4: Noranda camp (excluding the Horne deposit) and Val d'Or camp). Group III is host to only one known deposit, the Selbaie mine, which is unusual in that much of its mineralization cuts stratigraphy. The Selbaie mine sequence contains calc-alkalic andesite-rhyolite with relatively low...
Journal Article
Journal: Economic Geology
Published: 01 May 1996
Economic Geology (1996) 91 (3): 563–575.
...C. Tucker Barrie; T. E. Krogh Abstract The Selbaie mine is a large tonnage, low-grade Cu-Zn-Ag-Au deposit with both stratiform and epithermal characteristics. Mineralization comprises lower grade, disseminated Zn-Ag ore and pyritic siliceous sinter of the A1 zone at the surface; and higher grade Cu...
Journal Article
Journal: Economic Geology
Published: 01 May 2002
Economic Geology (2002) 97 (3): 629–642.
... Lake, Mattabi, Lyon Lake, Kamiskotia, South Bay and Selbaie—all from the Superior province of Canada ( Fig. 1 ), and the younger deposits include felsic volcanic rocks from the Bathurst camp, Canada; San Nicolas, Mexico; and Kuroko, Japan. Felsic metavolcanic rocks (the so-called "sericite...
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Journal Article
Journal: Economic Geology
Published: 01 November 2008
Economic Geology (2008) 103 (7): 1531–1562.
... belt. Although considered less prospective, some districts dominated by FII rhyolites, such as Val-d’Or and Selbaie, have collectively produced in excess of 100 million metric tons (Mt) of ore. Deposits in these districts mainly consist of sulfide veins and disseminated ore with low Cu and Zn grades...
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Journal Article
Published: 01 November 1986
Canadian Journal of Earth Sciences (1986) 23 (11): 1724–1741.
... an older till and of three dates obtained from intertill (below the surficial till) nonglacial sediments in the Timmins and Matheson areas in Ontario and the Selbaie mine area in Quebec, the oldest west-southwest (230–270°) striae are tentatively associated with the west-southwest flow that deposited...
Journal Article
Published: 02 April 2000
Canadian Journal of Earth Sciences (2000) 37 (2-3): 503–516.
..., and Selbaie). Systematic compressional wave velocity and density measurements in deep boreholes have established that lithological contacts were the main impedance contrast imaged, although reflections from faults and deformation zones have also been observed. The strongest reflections are attributed to mafic...
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Journal Article
Published: 28 January 2010
Canadian Journal of Earth Sciences (2010) 47 (5): 741–760.
...). The Selbaie mine (47.3 Mt) is a polymetallic deposit within a caldera environment that has been in production for 23 years. At the mine, mineralization occurs in veins that cut the local strata at a high angle ( Bouillon 1990 ). Two high-resolution MCS profiles (29-1, 29-2) were acquired by Lithoprobe at Les...
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Image
Multielement plot normalized to primitive mantle (Sun and McDonough, 1989) for FII felsic volcanic samples from various districts. A. Val-d’Or district: gray envelope includes samples R-10 to R-12, R-15 to -18, R-20, and R-116 away from VMS. B. Val-d’Or district: plots of rhyolite samples directly associated with VMS deposits. C. External North Volcanic zone area: gray envelope includes samples R-23, R-25, R-26, R-28 to -31, R-42, and R-43. D. Selbaie district. E. Hunter district: gray envelope includes samples R-55 to -66, excluding R-61 away from VMS. F. Hunter district: plots of rhyolite samples directly associated with VMS deposits. G. Gemini-Turgeon area: gray envelope includes samples R-121 to -123. H. Other rhyolite samples with FII signatures.
Published: 01 November 2008
samples directly associated with VMS deposits. C. External North Volcanic zone area: gray envelope includes samples R-23, R-25, R-26, R-28 to -31, R-42, and R-43. D. Selbaie district. E. Hunter district: gray envelope includes samples R-55 to -66, excluding R-61 away from VMS. F. Hunter district: plots
Image
Fig. 2. Th/Yb versus Ta /Yb diagram from Gorton and Schandl, 2000 (revised after Pearce, 1982, 1983) is divided into three tectonic fields: oceanic arcs, active continental margins (ACM) and within-plate volcanic zones (WPVZ). The within-plate basalts (WPB) and midocean ridge basalts (MORB) represent zones previously defined by Pearce (1982, 1983). Data sets shown by the symbols include the kuroko deposits, Japan (Appendix), Mattabi (Davis et al., 1985) and Lyon Lake mines, Ontario (Appendix), Kamiskotia mines, Ontario (Barrie and Pattison, 1999), Winston Lake, Ontario (Gorton and Schandl, 1995; Appendix), San Nicolas, Mexico (Gorton and Schandl, 2000), Selbaie, Quebec (Larson and Hutchinson, 1993), Bathurst deposits, New Brunswick (Lentz, 1996), South Bay mine, Ontario (Lesher et al., 1986), Askja volcano, Iceland (MacDonald et al., 1987), Narrow Lake volcanic rocks, Ontario (Noble, 1989), Geco mine, Ontario (Schandl et al., 1995), Geco gray gneiss (Schandl et al., 1995), Kidd Creek mine, Ontario (Schandl et al., 1999), and Noranda mines, Quebec (Ujike and Goodwin, 1987).
Published: 01 May 2002
and Schandl, 1995 ; Appendix ), San Nicolas, Mexico ( Gorton and Schandl, 2000 ), Selbaie, Quebec ( Larson and Hutchinson, 1993 ), Bathurst deposits, New Brunswick ( Lentz, 1996 ), South Bay mine, Ontario ( Lesher et al., 1986 ), Askja volcano, Iceland ( MacDonald et al., 1987 ), Narrow Lake volcanic rocks
Journal Article
Journal: Geophysics
Published: 01 January 2000
Geophysics (2000) 65 (6): 1882–1889.
...) and modal abundances of common sulfide minerals using simple mixing relations. Most sulfides have significantly higher impedances than silicate rocks, implying that seismic reflection techniques can be used directly for base metals exploration, provided the deposits meet the geometric constraints required...
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Journal Article
Journal: Economic Geology
Published: 01 August 2004
Economic Geology (2004) 99 (5): 1003–1013.
...T. R. Hart; H. L. Gibson; C. M. Lesher Abstract Volcanogenic massive Cu-Zn-(Pb) sulfide (VMS) deposits occur primarily in subaqueous rift-related environments (e.g., oceanic, fore-arc, arc, back-arc, continental margin, or continental), are hosted primarily by bimodal, mafic-felsic volcanic...
FIGURES
Journal Article
Journal: Geophysics
Published: 01 January 2000
Geophysics (2000) 65 (6): 1871–1881.
.... Seismic reflection methods have been applied within a variety of geological environments in various mining camps in Canada, e.g., low-grade greenstone belts of the Archean Abitibi subprovince (Selbaie area, Perron et al., 1997 ; Matagami area, Milkereit et al., 1992a ; Ansil mine, Perron and Calvert...
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Image
Published: 01 August 2004
F ig . 2. Chondrite-normalized plots, showing the shift with age from predominantly FIII to FII felsic volcanic rocks associated with VMS deposits, except for FIII rhyolites hosting younger, larger tonnage deposits (e.g. Kidd Creek, Neves Corvo, United Verde, Eskay Creek). Normalizing factors from
Journal Article
Journal: The Leading Edge
Published: 01 March 2000
The Leading Edge (2000) 19 (3): 270–274.
... this money is unclear, but it could have significantly subsidized Selco's exploration expenditures. Selco used INPUT for massive sulfide exploration work in Canada. The first discovery was the South Bay deposit in 1967 and the second was Selbaie in 1974. In the latter case, the deposit had been detected...
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