1 edition of Flin Flon volcanic belt found in the catalog.
Flin Flon volcanic belt
by Geological Association of Canada, Winnipeg Section in Winnipeg
Written in English
|Statement||by E. C. Syme ... [et al.].|
|Series||Field trip guidebook -- trip 6, Field trip guidebook (Geological Association of Canada-Mineralogical Association of Canada) -- trip 6|
|Contributions||Syme, E.C., Geological Association of Canada., Mineralogical Association of Canada.|
|The Physical Object|
|Pagination||iv, 91 p. :|
|Number of Pages||91|
Volcanism of Western Canada: Mackenzie Large Igneous Province, Volcanism of Alberta, Volcanism of British Columbia, Volcanism of Manitoba: : Source: Wikipedia: Libros en idiomas extranjerosFormat: Tapa blanda. About the City of Flin Flon Located north of the 54th parallel and km northwest of Winnipeg, the City of Flin Flon is a unique northern-urban community and trading area. The city was built on old volcanic belt which gives the region a beautiful .
Geology of the area: The Flin Flon-Snow Lake Greenstone Belt is a Precambrian greenstone belt formed by volcanic ically, it’s a bimodal-mafic classification of a volanogenic massive sulfide (VMS) ore deposit. (Yeah, I had to read that a couple of times, too). and hydrothermal history of the western Paleoproterozoic Flin Flon volcanic belt with respect to formation of volcanogenic massive sulphide (VMS) deposits; and 2) assist the development of exploration strategies that support the discovery of new VMS deposits (Galley and Bailes, ).
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Porphyritic intrusions and related mineralization in the Flin Flon volcanic belt [D. Baldwin] on *FREE* shipping on qualifying : D.
Baldwin. Get this from a library. Flin Flon volcanic belt: geology and ore deposits at Flin Flon and Snow Lake, Manitoba.
[E C Syme; Geological Association of Canada.; Mineralogical Association of Canada.;]. Located north of the 55th parallel of latitude, the City of Flin Flon is part of the Precambrian Amisk Volcanic Belt that was an element of the Trans-Hudson Origen. This belt was formed millions of years ago by underwater volcanic eruptions, these intense eruptions and multiple episodes of glaciations left us the present unique landscape, and is the source of the vast mineral.
Porphyritic intrusions and related mineralization in the Flin Flon volcanic belt. [Winnipeg]: Manitoba Dept. of Energy and Mines, Mineral Resources Division, (OCoLC) Material Type: Government publication, State or province government publication: Document Type: Book: All Authors / Contributors: D A Baldwin.
The Flin Flon-Glennie Complex or Flin Flon Greenstone Belt, extends over a km interval on the southern margin of the Trans-Hudson orogen in northern Manitoba and Saskatchewan, hosts clusters of volcanic hosted massive sulphide (VHMS) copper-zinc-gold deposits surrounding Flin Flon, Snow Lake - km to the east of Flin Flon, Hanson Lake - 60 km west of Flin Flon and Sherridon.
Buy Porphyritic intrusions and related mineralization in the Flin Flon volcanic belt (Economic geology report) by D. A Baldwin (ISBN:) from Amazon's Book Store. Author: D. A Baldwin. U–Pb geochronology of late Neoarchean tonalites in the Flin Flon Belt, Trans-Hudson Orogen: surprise at surface. Lithological and structural mapping in the east Wekusko Lake area of the Flin Flon Belt, Trans-Hudson Orogen, suggested an intimate relationship between magmatism, fluvial sedimentation, and initiation of fold and thrust belt by: INTRODUCTION The east Amisk area of Saskatchewan comprises a small portion of the Pro- terozoic Flin Flon-Snow Lake volcanic belt of east-central Saskatchewan and west-central Manitoba.
The area differs from much of the western portion of the belt in that pillowed basalts and mafic/ultramafic intrusions predominate over felsic volcanics and : G.R. Parslow.
Flin Flon (pop. 5, in census; 4, in Manitoba and in Saskatchewan) is a mining city in is located on a correction line on the Manitoba and Saskatchewan border, with the majority of the city located within Manitoba.
Residents thus travel Country: Canada. The past-producing Flin Flon mine, which closed inwas the largest deposit in the Flin Flon Camp, with an historic production of million tonnes (Syme and Bailes, ). The Callinan deposit, 2 km north in stratigraphically equivalent rocks to those of the Flin Flon.
The Flin Flon Belt (Trans-Hudson Orogen, Manitoba and Saskatchewan) is the largest Paleoproterozoic volcanic-hosted massive sulphide (VMS) district in the world, with million tonnes (Mt) of Zn-Cu-(Au-Ag) sulphide ore in 25 past or presently producing mines and Mt in subeconomic by: Rockcliff is a Canadian resource exploration company focused on the discovery, advancement and consolidation of a portfolio of the highest grade, undeveloped metal deposits in the Flin Flon Snow Lake Greenstone Belt.
Overview ofthe Flin Flon belt Historically, the stratigraphy of the Flin Flon belt has been described in terms of two stratigraphic groups, Amisk Group volcanic rocks and Missi Group continental sedimentary rocks (Bruce, ; Harrison, ).
The Flin Flon belt in the area between the Sturgeon-weirRiver (Saskatchewan) and Reed Lake (Manitoba. Located north of the 54th parallel of latitude, the City of Flin Flon was built on old volcanic belt which gives the region a beautiful rocky landscape like no other.
This belt was formed millions of years ago by underwater volcanic eruptions, these intense eruptions and multiple episodes of glaciations left us the present unique landscape, and is the source of the vast mineral deposits in Flin Flon.
Flin Flon is part of a Precambrian volcanic back-arc, the Amisk Volcanic Belt, which was formed billion years ago by underwater volcanic eruptions. These intense eruptions paired with several episodes of glaciation left us our unique, present-day landscape.
The property hosts the Talbot copper, gold, silver deposit covering just over four thousand hectares representing a geological environment similar to that of present and past producing base metal mines associated with bi-modal volcanic rocks in the Flin Flon Snow Lake Greenstone Belt.
Nine new projects have been initiated under the auspices of the Flin Flon Targeted Geoscience Initiative (TGI). These projects are designed to increase understanding of the volcanic and hydrothermal events influencing the setting of volcanogenic massive sulphide (VMS) deposits in the central Paleoproterozoic Flin Flon Belt.
The Flin Flon greenstone belt is one of the largest Proterozoic volcanic-hosted massive sulfide (VMS) districts in the world, containing 27 Cu-Zn- (Au) deposits from which more than million tonnes of ore have been mined. Most of mined VMS deposits in the Flin Flon belt are associated with juvenile arc volcanic rocks providing a powerful focus for future explorations.
Vol Is November Articles Interlayered Eclogites, Blueschists and Epidote Amphibolites from NE Oman: a Record of Protolith Compositional Control and Limited Fluid Infiltration. volcanic belt to the south, to the more homogeneous graph itic garnet-bioti te±silli mani te wackes characteristic of the Kisseynew Gneisses to the east (Ashton, ).
Garnet-andalusite and garnet-staurolite-sillimanite wackes, believed to be low-grade equivalents of the Kisseynew wackes, occur in the Flin Flon volcanic belt in the vicinity.2.
Geological setting. The Flin Flon greenstone belt, which lies within the central part of the Trans-Hudson orogen, is one of the world's largest volcanogenic massive sulphide (VMS) districts, having produced by over Mt of sulphide ore across 29 deposits (Bailes et al., ).The Lalor VMS deposit occurs within the Snow Lake volcanic arc assemblage on the eastern side of the Cited by: 5.found: Baldwin, D.
A. Porphyritic intrusions and related mineralization in the Flin Flon volcanic belt, t.p. (Flin Flon) found: NLC 2/21/84 (AACR 2: Flin Flon (Man.)) found: GeoNames, algorithmically matched, (ppl; 54°46ʹ06ʺN °51ʹ54ʺW).