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dc.contributor.author Michalkow, Albert en_US
dc.date.accessioned 2011-06-06T18:11:08Z
dc.date.available 2011-06-06T18:11:08Z
dc.date.issued 1954 en_US
dc.identifier ocm72793745 en_US
dc.identifier.uri http://hdl.handle.net/1993/4619
dc.description.abstract A layered series of granitic, sedimentary and altered volcanic rocks occurs in the Lily Pond Area of Southeastern Manitoba. The sedimentary and volcanic rocks are bands or sheets conformably enclosed within and between quartz diorite, granodiorites and quartz monzonite bands or sheets which are structurally concordant to a central domed quartz diorite mass. Field work and a petrographic study of specimens of the rocks showed that the granitic rocks could be instrusive crystallization differentiation fractions from a common parent basaltic melt. The liquid fractions were emplaced as upward and westward moving sheets which intruded a volcanic-sedimentary complex and left parts of this complex as remnant bands within the instrusive series. en_US
dc.format.extent 96 p. en_US
dc.format.extent 39307269 bytes
dc.format.mimetype application/pdf
dc.language en en_US
dc.language.iso en_US
dc.rights The reproduction of this thesis has been made available by authority of the copyright owner solely for the purpose of private study and research, and may only be reproduced and copied as permitted by copyright laws or with express written authorization from the copyright owner. en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title Structural geology and petrology of the Lily Pond area, Manitoba en_US
dc.type info:eu-repo/semantics/masterThesis
dc.degree.discipline Geology en_US


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