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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/19549
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DC FieldValueLanguage
dc.contributor.advisorMcNutt, R.H.-
dc.contributor.authorPrevec, Stephen-
dc.date.accessioned2016-06-15T15:44:38Z-
dc.date.available2016-06-15T15:44:38Z-
dc.date.issued1985-04-
dc.identifier.urihttp://hdl.handle.net/11375/19549-
dc.description.abstract<p> The northwestern Melville Peninsula in the area of 69°34'N/84°50'W consists of Precambrian Shield rocks that have suffered multiple metamorphic events, including a high grade metamorphic event in the late Archean, ranging from upper amphibolite to granulite grade locally. The oldest unit present is a tonalite-granodiorite-granite suite showing both foliation and lineation and a somewhat migmatic texture. This biotite-hornblende orthogneiss has produced a Rb-Sr whole rock age date of 2.55 +/- 0.2 Ga. Field relationships indicate that this is a metamorphically induced age rather than an emplacement age. A coarse grained granitic pegmatite associated with the orthogneiss has produced a Rb-Sr isochron indicating an age of 1.83 +/- 0.06 Ga. Petrographic and field evidence indicate that this represents the emplacement age of the pegmatite. </p>en_US
dc.language.isoenen_US
dc.subjectPetrologyen_US
dc.subjectgeochemistryen_US
dc.subjectgeochronologyen_US
dc.subjectPrecambrian rocksen_US
dc.subjectMelville Peninsulaen_US
dc.subjectNorthwest Territoriesen_US
dc.titlePetrology, geochemistry, and geochronology of some Precambrian rocks of the north-western Melville Peninsula, Northwest Territoriesen_US
dc.contributor.departmentGeologyen_US
dc.description.degreetypeThesisen_US
dc.description.degreeBachelor of Science (BSc)en_US
Appears in Collections:Bachelor theses

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