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dc.contributor.author Solonyka, Edward Richard en_US
dc.date.accessioned 2012-05-15T15:54:49Z
dc.date.available 2012-05-15T15:54:49Z
dc.date.issued 1974 en_US
dc.identifier ocm72805471 en_US
dc.identifier.uri http://hdl.handle.net/1993/6188
dc.description.abstract The Mink Narrows copper deposit of Copper Reef Mines (1973) Ltd., is one of several massive sulphide deposits in the Flin Flon region, northern Manitoba. It outcrops on a small reef off the north shore of Lake Athapapsukow, 14 miles southeast of Flin Flon. The vertical sheet-like deposit occurs in the basic metavolcanic rocks of the Amisk Group and is approximately parallel to the contact of a nearby grandodioritic intrusion. The host rocks have been recrystallized and later affected by minor retrograde metamorphism. Adjacent to the intrusion, the metavolcanics have been fractured. An alteration zone of sericite, chlorite, carbonate and quartz is associated with the deposit. Pyrite, pyrrhotite, chalcopyrite and sphalerite, are the major metallic minerals within the deposit and are present as both massive and disseminated sulphides. Consistent zonation of copper and zinc is not present within the deposit, however zoning occurs in several of the hole intersections. Metamorphism of the sulphides is indicated by their recrystallization, replacement and cataclastic features. Two main genetic possibilities exist for the deposit, either emplacement by hydrothermal fluids from the granodiorite intrusion, or by activities related to the volcanism. en_US
dc.format.extent vii, 69 leaves. en_US
dc.language en en_US
dc.rights en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title Mink Narrows copper deposit, Lake Athapapuskow, Manitoba en_US
dc.type info:eu-repo/semantics/masterThesis
dc.type master thesis en_US
dc.degree.discipline Earth Sciences en_US


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