Mineralogical and geochemical investigation of the cordierite-anthophyllite rocks at Star Lake, near Sherridon, Manitoba

dc.contributor.authorLeroux, Marc V.en_US
dc.date.accessioned2012-05-23T21:02:07Z
dc.date.available2012-05-23T21:02:07Z
dc.date.issued1989en_US
dc.degree.disciplineGeological Sciencesen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractThe Sherridon Group, a stratigraphic unit of the Kisseynew gneiss belt, near Sherridon, Manitoba is typically dominated by quartz-rich gneisses. Discontinuous lenses of cordierite-anthophyllite rocks, the focus of the present study, occur within these quartz-biotite gneiss units. These cordierite-anthophyllite gneisses are extremely coarse-grained in places, and are spatially associated with barren (Star Lake) and sulfide-mineralized zones (Sherridon; Elken Lake). The present chemical composition of the Star Lake-Elken Lake gneisses indicates hydrothermal alteration of a basaltic progenitor producing chlorite-rich alteration pipes. This alteration involves a depletion in alkali and alkaline earth elements with an apparent enrichment in Al and Mg as a function of constant summation. These chemical modifications are the result of reactions between heated seawater and basaltic rocks of the crust. A modern analogue of the Sherridon Group environment might be the shelf and slope deposits of modern island arcs.en_US
dc.format.extentxiv, 177 [i.e. 202] leaves :en_US
dc.identifierocm72751300en_US
dc.identifier.urihttp://hdl.handle.net/1993/7189
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.titleMineralogical and geochemical investigation of the cordierite-anthophyllite rocks at Star Lake, near Sherridon, Manitobaen_US
dc.typemaster thesisen_US
local.subject.manitobayesen_US
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