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Petrology, Geochemistry and Geochronology of a pluton in Thelon Tectonic Zone, Northwest Territories

dc.contributor.advisorMcNutt, R. M.
dc.contributor.authorNewman, Richard
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-06-14T19:42:26Z
dc.date.available2016-06-14T19:42:26Z
dc.date.issued1986-04
dc.description.abstract<p> The Thelon Tectonic Zone is a major structural, metamorphic and lithological feature of the Precambrian Shield in the Northwest Territories. Situated within this Zone is a 30 square kilometre plutonic body. Rubidium- Strontium whole rock geochronology yields an age range of 1650 - 2200 Ma for the emplacement of this pluton. Field and petrographic evidence indicates that the pluton has suffered post-emplacement deformation, representative of a late Proterozoic metamorphic event. Major and trace element geochemistry suggests that this high Ca, ferrogranodiorite-tonalite intrusive body is associated with a subduction-related, continental margin tectonic environment. </p>en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19540
dc.language.isoenen_US
dc.subjectPetrologyen_US
dc.subjectGeochemistryen_US
dc.subjectGeochronologyen_US
dc.subjectplutonen_US
dc.subjectTectonic Zoneen_US
dc.subjectThelon Tectonicen_US
dc.titlePetrology, Geochemistry and Geochronology of a pluton in Thelon Tectonic Zone, Northwest Territoriesen_US

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