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dc.contributor.author Marr, John Munro en_US
dc.date.accessioned 2012-05-14T18:05:06Z
dc.date.available 2012-05-14T18:05:06Z
dc.date.issued 1970 en_US
dc.identifier ocm72793280 en_US
dc.identifier.uri http://hdl.handle.net/1993/5831
dc.description.abstract The Northern Granitic Rocks comprise a group of leucocratIc to mesocratic, plutonIc rocks which occur immediately to the north of the Rice Lake Greenstone Belt. An area of two hundred square miles has been mapped at a scale of 1:50,000 and several hundred samples have been studied to provide data on mineralogy, texture, specific gravity and chemical composition. This appears to be a group of truly igneous rocks which are intrusive into the rocks of the Rice Lake Greenstone Belt. Compositional variation exists from an area of homogeneous trondhjemite, characterised by a high silica content and a high soda to potash ratio west of Wallace Lake, to more mafic, hornblende-bearing quartz diorites and diorites east of Wallace Lake. Both field relationships and mineralogical characteristics suggest that the Northern Granitic Rocks are synkinematic intrusions. This suite of rocks bears a strong resemblance to the other quartz diorite plutons in the area and to granitic intrusions bordering greenstone belts in many shield areas of the world. en_US
dc.format.extent ix, 93 leaves : en_US
dc.language en en_US
dc.rights en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title Petrology of the "northern granitic rocks" : Wanipigow River area, southeast Manitoba en_US
dc.type info:eu-repo/semantics/masterThesis
dc.degree.discipline Earth Sciences en_US


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