2 edition of Exploration history review of the Schist Lake area, Manitoba 63K/12 found in the catalog.
Exploration history review of the Schist Lake area, Manitoba 63K/12
Manitoba. Mineral Resources Division.
by Dept. of Mines, Resources & Environmental Management in [Winnipeg]
Written in English
Bibliography: p. 46-47.
|Statement||[edited by J. D. Bamburak].|
|Series||MRD open file report ; 77/6|
|Contributions||Bamburak, J. D.|
|LC Classifications||TN270 .M314 1977|
|The Physical Object|
|Pagination||iv, 55 p. :|
|Number of Pages||55|
|LC Control Number||79306683|
The annual mining & exploration review An official publication of the Manitoba-Saskatchewan Prospectors and Developers Association There is currently exploration in Snow Lake area for gold. HISTORY. The Snow Lake area has a long exploration and mining history. Exploration in the Chisel Basin has been active since The Chisel Basin area is a large geologically controlled area and has hosted producing mines for nearly 50 years.
Manitoba ⓘ Atik Lake Banded Iron Deposit Bernier, Louis R., , Vanadiferous Zincian-Chromian Hercynite in a Metamorphosed Basalt-Hosted Alteration Zone, Atik Lake, Manitoba, Canadian Mineralogist () v. ;. Ten zones of gold-arsenopyrite mineralization have been identified in the Squall Lake area through previous exploration programs from to These zones occur within a m stratigraphic interval above the staurolite schist unit and are aligned over a 10 km strike length along the northwest flank of the McLeod Lake Synform.
Closure of Public Lane (Schist Lake) By-law No. 6/ / 21 Oct 2 Nov Community Councils Election Regulation: 71/ A: 6 Apr 18 Apr Community Employees Benefits Program By-law No. 18/ 73/ 30 Mar 14 Apr Community Records Retention Regulation: 68/ 6 Apr 18 Apr Conflict of Interest. Silurian succession from North Africa – Sedimentology and thermal history for a new era of hydrocarbon exploration: Hocine: Djouder: Sedimentary model of a Permian-Triassic salt giant in the Peruvian fold-and-thrust belt: Emilio: Carrillo: Exploring in Asia for Oil and Gas in Naturally Fractured and Weathered Basement.
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Exploration History Review of the Schist Lake Area, Manitoba; 63K/12 Edited by J.D. Bamburak NOTE: This report was superseded by the Mineral Inventory Cards Database and OF Open File Report 77/5. The deposit is located east of White Lake, and near the northeast arm of Schist Lake.
E.A. Mortimer first staked the deposit as Byng () on Ap On Octohe transferred one-half interest to G.V. Armer. The claim was allowed to lapse on. Martins, T., Linnen, R.L., Fedikow, M.A.F. and Singh, J. Whole-rock and mineral geochemistry as exploration tools for rare-element pegmatite in Manitoba: examples from the Cat Lake–Winnipeg River and Wekusko Lake pegmatite fields (parts of NTS 52L6, 63J13); in Report of ActivitiesManitoba Growth, Enterprise and Trade, Manitoba.
Till composition of a sampling transect in the Lynn Lake area, northwest Manitoba (parts of NTS 64B12, 64C9, 11, 12, 14–16, 64F3, 4) By T.J.
Hodder and M.S. Gauthier. Open File OF Gravity gradiometer survey of the Creighton area, Saskatchewan and Manitoba, parts of NTS L/8 and K/5. Athapapuskow Lake area, west-central Manitoba (parts of NTS 63K12, 13); in Report of ActivitiesManitoba Growth, Enterprise and Trade, Manitoba Geological Survey, p.
– Summary The Athapapuskow Lake area is part of a tectonic collage situated in the Flin Flon greenstone belt, Exploration history review of the Schist Lake area.
The Namew Lake Fe-Ni-Cu sulfide deposit, 60 km south of Flin Flon, Manitoba, is hosted by an undifferentiated metapyroxenite sill enclosed within Early Proterozoic orthogneisses and covered by. Source Map: OGSP FINGER LAKE SHEET. Sources Map Scale: Access Description: km North of Red Lake and 70 km SE of the Manitoba-Ontario boundry.
Sandy Lake settlement is 7 km north, served by regular airline flights. Exploration and Mining History.
Bailes, A.H. Map 1, Geologic Compilation of the Snow Lake-Flin Flon-Sherridon area, scale, geological map, accompanying Manitoba Mineral Resources Division Paper Buckham, A.F. MapAthapapuskow Lake; scale, geological map, accompanying Geological Survey of Canada Paper Publication - Operation Lingman Lake, P Publication Number: MP Date: Author: Bennet, G.
and Railey, R. Publisher Name: ODM. Book - Technical Report on The Lingman Lake Property, Lingman Lake Area, District of Kenora. Prepared for Signature Resources Ltd. Gold metallogenesis and tectonometamorphic history of selected deposits from the Snow Lake area and the southern flank of the Kisseynew Domain, west-central Manitoba.
T he T Hompson Nickel Belt in northern Manitoba is the second largest Ni-Cu-(PGE) mining camp in Canada, after Sudbury, with a premining resource estimated at million metric tons (Mt) at percent Ni, percent Cu, percent Co, g/t Pt, g/t Pd, g/t Rh, g/t Ru, g/t Ir, and g/t Os (Naldrett, ).It is the second largest camp of komatiite.
Rocks west of the Mandy Road Fault in the Schist Lake–Mandy mines area, approximately 5 km south of Flin Flon, are mainly juvenile tholeiitic, aphyric and pyroxene-plagioclase–phyric basaltic. The Detour Lake deposit is at a faulted contact between mafic volcanic and siliciclastic to volcaniclastic rocks, differing from other orogenic Au deposits in the dominantly greenschist facies Abitibi region, by possessing amphibolite facies assemblages.
Consequently, typical indicator minerals for mineralization, like secondary biotite, may not be useful for locating ore zone, due to the. Geology of the Rice Lake Area, Rice Lake Greenstone Belt, Southeastern Manitoba (Parts of NTS 52L13, 52M4).
Manitoba Science, Technology, Energy and Mines, Manitoba Geological Survey. Examples from the Itapicuru greenstone belt in Bahia, Brazil, a crystalline area near Nantes, France, and the Rice Lake greenstone belt in Manitoba, Canada, demonstrate that mafic and ultramafic.
The purpose of this paper is to review current literature in light of a large recently published dataset (Burnham et al., ) on the geology of Thompson nickel belt and provide new insights into the petrology and geochemistry of the sulfide describe and interpret the textures, mineralogy, mineral chemistry, and whole-rock chemistry of sulfide-bearing rocks in the Thompson.
Source Map: OGSP FINGER LAKE SHEET. Sources Map Scale: Access Description: km North of Red Lake and 70 km SE of the Manitoba-Ontario border.
Sandy Lake settlement is 7 km north, served by regular airline flights. Exploration and Mining History. One important line of evidence for this scenario comes from the hafnium-tungsten isotopic system (review papers by Jacobsen,and Kleine et al., a, b).
Lithophile Hf decays to siderophile W with a half life of 9 m.y., so ratios of Hf to W isotopes in rocks and metals constrain ages of differentiation of core from mantle. Mines and Energy Branches Natural Resources Building 50 Elizabeth Avenue P.O. Box St.
John’s, NL A1B 4J6. Phone: The integrated analysis of seismic rock properties, lithogeochemical data, and mineral compositional data, estimated via scanning electron microscopy-energy dispersive X-ray spectroscopy (SEM-EDS), provides insight into the effects of hydrothermal alteration on seismic reflectivity in the footwall of the Lalor volcanogenic massive sulfide (VMS) deposit, Manitoba, Canada.
STOCKWELL, C. H.,Rice Lake-Gold Lake area, southeastern M a n i t o b a, Canadian Mines and Geology Branch, Memoir79 pp.
W00DBRIDGE, D. E.,The hydraulic compressedair power plant at the Victoria m i n e, Engineering and Mining J o .Full text of "Record of North American geology for to inclusive [, and ]" See other formats.The increasing demand for green technology and battery metals necessitates a review of geological exploration techniques for Li–Cs–Ta (LCT) pegmatites, which is applicable to the work of mining companies.
This paper reviews the main controls of LCT pegmatite genesis relevant to mineral exploration programs and presents a workflow of grassroots exploration techniques, supported by .