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Journal Article

Highly metamorphosed altered rocks associated with the Osborne Lake volcanogenic massive sulfide deposit, Snow Lake area, Manitoba Available to Purchase

Calvert C. Bristol, Edgar Froese
Published: 01 December 1989
The Canadian Mineralogist (1989) 27 (4): 593–600.
View PDF for article title, Highly metamorphosed altered rocks associated with the Osborne <span class="search-highlight">Lake</span> volcanogenic massive sulfide deposit, <span class="search-highlight">Snow</span> <span class="search-highlight">Lake</span> <span class="search-highlight">area</span>, Manitoba
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Journal Article

Geology of the copper-zinc deposits of stall lake mines lts., snow lake area, n. manitoba Available to Purchase

C. J. A. Coats, L. A. Clark, R. Buchan, J. J. Brummer
Journal: Economic Geology
Published: 01 December 1970
Economic Geology (1970) 65 (8): 970–984.
DOI: https://doi.org/10.2113/gsecongeo.65.8.970
...C. J. A. Coats; L. A. Clark; R. Buchan; J. J. Brummer Abstract The copper-zinc deposits of Stall Lake Mines Ltd. in the Snow Lake area of Manitoba are interpreted as being of metamorphosed volcanogenic origin. Some of the massive chalcopyrite and sphalerite ores occur in highly elongate, stratiform...
View PDF for article title, Geology of the copper-zinc deposits of stall <span class="search-highlight">lake</span> mines lts., <span class="search-highlight">snow</span> <span class="search-highlight">lake</span> <span class="search-highlight">area</span>, n. manitoba
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Journal Article

Application of chlorite-sulfide-oxide equilibria to metamorphosed massive sulfide ores, Snow Lake area, Manitoba Available to Purchase

L. Taras Bryndzia, Steven D. Scott
Journal: Economic Geology
Published: 01 July 1987
Economic Geology (1987) 82 (4): 963–970.
DOI: https://doi.org/10.2113/gsecongeo.82.4.963
...L. Taras Bryndzia; Steven D. Scott Abstract The Stall Lake and Anderson Lake massive Cu-Zn sulfide deposits, situated in the Snow Lake area of northern Manitoba, occur in hydrothermally altered felsic volcanic rocks which have been subjected to amphibolite-grade metamorphism. Mineral assemblages...
View PDF for article title, Application of chlorite-sulfide-oxide equilibria to metamorphosed massive sulfide ores, <span class="search-highlight">Snow</span> <span class="search-highlight">Lake</span> <span class="search-highlight">area</span>, Manitoba
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Journal Article

Metamorphic zones in the Snow Lake area, Manitoba Available to Purchase

E. Froese, E. Gasparrini
Published: 01 May 1975
The Canadian Mineralogist (1975) 13 (2): 162–167.
View PDF for article title, Metamorphic zones in the <span class="search-highlight">Snow</span> <span class="search-highlight">Lake</span> <span class="search-highlight">area</span>, Manitoba
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Generalized geology of the Reed Lake – Snow Lake area modified from Syme et al. (1995) and Bailes et al. (1994). The Morton Lake fault zone (MLFZ) is interpreted to represent the basal thrust (Syme et al. 1995; Lucas et al. 1996) that separates the Snow Lake area from the central Flin Flon Belt (i.e., Amisk collage). The Snow Lake area is characterized by a structural style and by lithologies that are more comparable to the Kisseynew domain than those observed in the central Flin Flon Belt. The Snow Lake area consist of a series of Kisseynew-type allochthons of volcanic and sedimentary rocks.

Generalized geology of the Reed Lake – Snow Lake area modified from Syme et... Available to Purchase

Published: 10 February 2000
Fig. 2. Generalized geology of the Reed Lake – Snow Lake area modified from Syme et al. ( 1995 ) and Bailes et al. ( 1994 ). The Morton Lake fault zone (MLFZ) is interpreted to represent the basal thrust ( Syme et al. 1995 ; Lucas et al. 1996 ) that separates the Snow Lake area from the central
Image
Regional geology of the Snow Lake area, created using CorelDRAW version 18. Structural domains (A–E) are shown by the red dashed lines and are represented on Figure 13. The regional data for the map was compiled from Froese and Moore (1980), Kraus and Williams (1999), Beaumont-Smith and Gagné (2008), and Gagné (2009b). The base map was from Gagné and Beaumont-Smith (2010), courtesy of the Manitoba Geological Survey. Alm, almandine; Bt, biotite; Sil, sillimanite. [Colour online.]

Regional geology of the Snow Lake area, created using CorelDRAW version 18.... Available to Purchase

Published: 05 November 2020
Fig. 4. Regional geology of the Snow Lake area, created using CorelDRAW version 18. Structural domains (A–E) are shown by the red dashed lines and are represented on Figure 13 . The regional data for the map was compiled from Froese and Moore (1980) , Kraus and Williams (1999) , Beaumont
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Physical attributes and correlation of units in the Snow Lake area. Available to Purchase

Published: 05 November 2020
Table 1. Physical attributes and correlation of units in the Snow Lake area.
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Interpreted structural geological map of the Snow Lake area showing the location of regional faults and folds. North–south and northeast–southwest cross section illustrated in Fig. 21 are represented by solid black lines. BLF, Birch Lake Fault; MRT, McLeod Road Thrust Fault; SLF, Snow Lake Fault. The map was created using CorelDRAW version 18. The base map was modified after Natmap Shield Margin Project Working Group (1998), which contains information licensed under the Open Government Licence – Canada. [Colour online.]

Interpreted structural geological map of the Snow Lake area showing the loc... Available to Purchase

Published: 05 November 2020
Fig. 16. Interpreted structural geological map of the Snow Lake area showing the location of regional faults and folds. North–south and northeast–southwest cross section illustrated in Fig. 21 are represented by solid black lines. BLF, Birch Lake Fault; MRT, McLeod Road Thrust Fault; SLF, Snow
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Geologic map of the Snow Lake area showing the locations of all whole-rock samples analyzed for oxygen isotopes and the regional oxygen isotope zoning, based on Taylor and Timbal (1998). Note that high-temperature alteration from beneath the Chisel Lake Gabbro is projected to the surface.

Geologic map of the Snow Lake area showing the locations of all whole-rock ... Available to Purchase

Published: 01 June 2016
Fig. 11 Geologic map of the Snow Lake area showing the locations of all whole-rock samples analyzed for oxygen isotopes and the regional oxygen isotope zoning, based on Taylor and Timbal (1998) . Note that high-temperature alteration from beneath the Chisel Lake Gabbro is projected
Journal Article

Pressure and temperature conditions of metamorphism in the vicinity of three massive sulfide deposits, Flin Flon – Snow Lake belt, Manitoba Free

Pradeep K. Aggarwal, Bruce E. Nesbitt
Published: 01 November 1987
Canadian Journal of Earth Sciences (1987) 24 (11): 2305–2315.
DOI: https://doi.org/10.1139/e87-215
... of 475 ± 75 °C at 2.6 ± 1.2 kbar pressure (1 kbar = 0.1 kPa). The Snow Lake area to the west, in the vicinity of the Anderson Lake deposit, has been metamorphosed to sillimanite grade. In the staurolite–biotite–sillimanite zone, the temperature and pressure conditions were 580 ± 25 °C and 5.25 + 0.75...
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Simplified geology of the central and eastern portions of the Flin Flon domain showing major tectonostratigraphic assemblages and plutons, and locations of mined VMS deposits. F = Flin Flon, S = Snow Lake. The Snow Lake area is characterized by a structural style and rock types that are more comparable to the Kisseynew domain than those in the Amisk Collage of the central Flin Flon belt. The Snow Lake area consists of a series of Kisseynew-type allochthons of 1.89 Ga volcanic and 1.85 to 1.83 Ga sedimentary rocks soled by the Morton Lake fault zone (MF; Syme et al., 1995). The red rectangle shows the area depicted in Figure 4a and b.

Simplified geology of the central and eastern portions of the Flin Flon dom... Available to Purchase

Published: 01 June 2016
Fig. 2 Simplified geology of the central and eastern portions of the Flin Flon domain showing major tectonostratigraphic assemblages and plutons, and locations of mined VMS deposits. F = Flin Flon, S = Snow Lake. The Snow Lake area is characterized by a structural style and rock types
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Schematic cross section showing a series of allocthons in the Reed Lake – Snow Lake area (bottom left to upper right in Fig. 2). The 1.89 Ga panels of volcanic rocks are seperated by thrust faults and panels of 1.84 Ga Burntwood Group sedimentary rocks. The allocthons of volcanic and younger sedimentary rocks are cut by late successor arc 1.84–1.83 Ga granite plutons. VMS mines are restricted to arc assemblages, with seven of the 10 mines in the Snow Lake area located in an allocthon composed of Snow Lake arc assemblage rocks.

Schematic cross section showing a series of allocthons in the Reed Lake – S... Available to Purchase

Published: 10 February 2000
Fig. 3. Schematic cross section showing a series of allocthons in the Reed Lake – Snow Lake area (bottom left to upper right in Fig.  2 ). The 1.89 Ga panels of volcanic rocks are seperated by thrust faults and panels of 1.84 Ga Burntwood Group sedimentary rocks. The allocthons of volcanic
Book Chapter

Supplementary References for Annotated Bibliographies of Mineral Deposits in the Western Hemisphere Available to Purchase

Author(s)
JOHN D. RIDGE
Book: Annotated Bibliographies of Mineral Deposits in the Western Hemisphere
Series: GSA Memoirs
Publisher: Geological Society of America
Published: 01 January 1972
DOI: 10.1130/MEM131-S-p1
..., Preliminary compilation of the geology of the Snow Lake-Flin Flon-Sherridon area, Manitoba: Man. Dept. Mines and Nat. Res. Geol. Paper 1-71, 27 p. Snow Lake, MANITOBA Coats, C.J.A., and others, 1970, Geology of the copper-zinc deposits of Stall Lakes Mines Ltd., Snow Lake area, N. Manitoba: Econ. Geol...
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Canada Britannia (Howe Sound), BRITISH COLUMBIA Brown, A. S., 1972, Britannia: 24th Int. Geol. Cong. Field Excur. A09–C09, p. 7–14 Rossland, BRITISH COLUMBIA Fyles, J. T., and others, 1973, The age of sulfide mineralization at Rossland, British Columbia: Econ. Geol., v. 68, no. 1, p. 23–33 Sullivan, BRITISH COLUMBIA Morris, H. C., and Staff, Sullivan Mine, 1972, An outline of the geology of the Sullivan mine, Kimberley, British Columbia: 24th Int. Geol. Cong. Field Excur. A24–C24, p. 26–34, 36 Flin Flon-Sherritt Gordon (General), MANITOBA Bailes, A. H., 1971, Preliminary compilation of the geology of the Snow Lake-Flin Flon-Sherridon area, Manitoba: Man. Dept. Mines and Nat. Res. Geol. Paper 1-71, 27 p. Snow Lake, MANITOBA Coats, C.J.A., and others, 1970, Geology of the copper-zinc deposits of Stall Lakes Mines Ltd., Snow Lake area, N. Manitoba: Econ. Geol., v. 65, p. 970-984 Batimerst-Newoastie, NEW BRUNSWICK Lusk, J., 1972, Examination of volcanic-exhalative and biogenic origins for sulfur in the stratiform massive sulfide deposits of New Brunswick: Econ. Geol., v. 67, p. 169–183 McAllister, A. L., and Lamarche, R. Y., 1972, The Bathurst-Newcastle area: 24th Int. Geol. Cong. Field Excur. A58, p. 50–76; see also p. 1–14 Stumpfl, E. F., and others, 1971, Tectonics, volcanism and mineralization in New Brunswick, Canada—Some new aspects, in Takéuchi, Y., Editor, IAGOD Volume, IMA-IAGOD Meetings 1970, Papers and Pr.: Soc. Min. Geols. Japan, Spec. Issue no. 3, p. 86–92 Great Bear Lake, NORTHWEST TERRITORIES Badham, J.P.N., and others,

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Correlation of this study’s sequence of deformation events, with those of p... Available to Purchase

Published: 05 November 2020
Table 2. Correlation of this study’s sequence of deformation events, with those of previous authors in the Snow Lake area.
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Geological map of the Snow Lake – File Lake – Wekusko lakes area, including isograds from authors cited in Kraus and Menard (1997). Geochronological results refer to age of emplacement of granitic rocks (from Gordon et al. 1990; Bailes et al. 1991; David et al. 1996). Faults: BCSZ, Berry Creek shear zone; BeLF, Beltz Lake fault; BLF, Birch Lake fault; CBF, Crowduck Bay fault; LLF, Loonhead Lake fault; MLF, Morton Lake fault; MRF, McLeod Road fault; RLF, Roberts Lake fault; SLF, Snow Lake fault. Plutons (P), plutonic complexes (C), and gneiss domes (GD): BLC, Batty Lake; BLP, Bujarski Lake; HLGD, Herblet Lake; HLP, Ham Lake; NBP, Nelson Bay; PLGD, Pulver Lake; RiLP, Richard Lake; RLC, Rex Lake; RLP, Reed Lake; SLGD, Squall Lake; SLP, Sneath Lake; TLP, Tramping Lake; WLP, Wekusko Lake. Mineral abbreviations after Kretz (1983).

Geological map of the Snow Lake – File Lake – Wekusko lakes area, including... Available to Purchase

Published: 10 February 2000
Fig. 2. Geological map of the Snow Lake – File Lake – Wekusko lakes area, including isograds from authors cited in Kraus and Menard ( 1997 ). Geochronological results refer to age of emplacement of granitic rocks (from Gordon et al. 1990 ; Bailes et al. 1991 ; David et al. 1996 ). Faults: BCSZ
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Geological and proportional symbol map of the Chisel Lake area of the Snow Lake greenstone belt, Manitoba, showing: (a) Cu/Zn ratio in the &lt;0.063 mm fraction of till; and (b) Zn/Cu ratios in the &lt;0.063 mm fraction of till (modified from Kaszycki et al. 1996). Note locations of past producing VMS deposits shown in triangles.

Geological and proportional symbol map of the Chisel Lake area of the Snow ... Available to Purchase

Published: 28 August 2015
Fig. 14. Geological and proportional symbol map of the Chisel Lake area of the Snow Lake greenstone belt, Manitoba, showing: ( a ) Cu/Zn ratio in the <0.063 mm fraction of till; and ( b ) Zn/Cu ratios in the <0.063 mm fraction of till (modified from Kaszycki et al . 1996 ). Note locations
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Simplified geological map of the Threehouse synform area at Snow Lake (SL). The letters A–E refer to structural domains. ABA, Anderson Bay anticline. Faults: ABSZ, Anderson Bay shear zone; BCSZ, Berry Creek shear zone; BSZ, Bartlett shear zone; SL, town of Snow Lake. Abbreviations of the granitoid plutons as in Fig. 2. Additional structural data were taken from Harrison (1949) and Froese and Moore (1980). A three-dimensional view of this area is given in Fig. 6.

Simplified geological map of the Threehouse synform area at Snow Lake (SL).... Available to Purchase

Published: 10 February 2000
Fig. 3. Simplified geological map of the Threehouse synform area at Snow Lake (SL). The letters A–E refer to structural domains. ABA, Anderson Bay anticline. Faults: ABSZ, Anderson Bay shear zone; BCSZ, Berry Creek shear zone; BSZ, Bartlett shear zone; SL, town of Snow Lake. Abbreviations
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Lithotectonic domains of part of the Trans-Hudson Orogen and location of the Snow Lake area at the southern margin of the Kisseynew Domain (after Hoffman 1988). CL, Cleunion Lake; KL, Kississing Lake; SFKD, southern flank of Kisseynew Domain; SLFZ Setting Lake fault zone; SR, Sasagiu Rapids; Th, Thompson. Inset map: RH, Rae–Hearne; S, Superior craton; THO, Trans-Hudson Orogen.

Lithotectonic domains of part of the Trans-Hudson Orogen and location of th... Available to Purchase

Published: 10 February 2000
Fig. 1. Lithotectonic domains of part of the Trans-Hudson Orogen and location of the Snow Lake area at the southern margin of the Kisseynew Domain (after Hoffman 1988 ). CL, Cleunion Lake; KL, Kississing Lake; SFKD, southern flank of Kisseynew Domain; SLFZ Setting Lake fault zone; SR, Sasagiu
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Regional geologic maps. a) Simplified domain map of the Saskatchewan-Manitoba portion of the Trans-Hudson orogen (THO) and location of the Archean cratons modified after Lucas et al. (1993). The Flin Flon-Glennie Complex includes the Glennie domain, Hanson Lake block (HL), and Flin Flon domain. The location of the field study area is indicated by a yellow rectangle. The location of gold deposits discussed in the text are numbered and represented by red circles: 1 = New Britannia mine, 2 = Puffy Lake mine, 3 = Tartan Lake deposit, 4 = Santoy deposits, 5 = Seabee mine, 6 = Komis mine, 7 = Burnt Timber mine, 8 = Lynn Lake area deposits. Inset of Canada showing the location of domain map. Mb = Manitoba, Sk = Saskatcehewan. b) Regional geology of the Flin Flon-Glennie Complex (excluding the Glennie domain) modified after Syme et al. (1999). Abbreviations: HLGD = Herblet Lake gneiss dome, PLGD = Pulver Lake gneiss dome. Snow Lake area is highlighted by the black box.

Regional geologic maps. a) Simplified domain map of the Saskatchewan-Manito... Available to Purchase

Published: 01 March 2024
, PLGD = Pulver Lake gneiss dome. Snow Lake area is highlighted by the black box.
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A. Plan view of the 1.89 Ga Anderson sequence, Chisel sequence, and Snow Creek sequence components of the Snow Lake arc assemblage. Arrows show facing direction of supracrustal rocks. Also shown are ca. 1.84 to 1.83 Ga successor arc sedimentary and intrusive rocks, ca. 1.84 Ga thrust faults (red, teeth), and ca. 1.78 Ga normal faults (solid black lines). Colored circles and ellipses show distribution of VMS deposits (red are Cu rich, magenta are Zn rich): A = Anderson Lake, B = Bomber, C = Chisel Lake, CK = Cook Lake, CN = Chisel North, G = Ghost Lake, Jn = Joannie zone, L = Lost Lake, La = Lalor Lake, Li = Linda, M = Morgan Lake, P = Photo Lake, Pn = Pen zone, Pt = Pot Lake, R = Rod, Ra = Ram zone, Rd = Raindrop, S = Stall Lake. The barren sulfide “horizon” (locally known as the Foot-Mud horizon) is a sulfide-bearing, fine-grained, volcaniclastic unit located at the contact between the Anderson (primitive arc) and Chisel (mature arc) sequences. B. Simplified geologic map of the Snow Lake area. Letters indicate informal names of units (identified in legend). The designation “p-arc” after the unit name in the legend indicates that it belongs to the primitive arc (Anderson sequence) and “m-arc” indicates that it is part of the mature arc (Chisel sequence). VMS deposit names and designations are the same as those given in the caption for A.

A. Plan view of the 1.89 Ga Anderson sequence, Chisel sequence, and Snow Cr... Available to Purchase

Published: 01 June 2016
between the Anderson (primitive arc) and Chisel (mature arc) sequences. B. Simplified geologic map of the Snow Lake area. Letters indicate informal names of units (identified in legend). The designation “p-arc” after the unit name in the legend indicates that it belongs to the primitive arc (Anderson