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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/19833
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DC FieldValueLanguage
dc.contributor.advisorMcNutt, R. H.-
dc.contributor.authorMcMaster, Glenn-
dc.date.accessioned2016-07-18T19:51:10Z-
dc.date.available2016-07-18T19:51:10Z-
dc.date.issued1975-04-
dc.identifier.urihttp://hdl.handle.net/11375/19833-
dc.description.abstract<p> A gabbroic intrusion within the Wabigoon Greenstone Belt, southeast of Dryden Ontario, was studied and mapped. Petrographic examination of the sill was carried out and geochemical whole rock data was obtained using X.R.F. methods. </p> The Gabbro Lake Sill was injected into a mafic pile and subsequently underwent fractional crystallization and differentiation. The sill exhibits good phase layering resulting in its division into six basic units: Chilled Margin Gabbro Diabasic Gabbro Leucocratic Gabbro Pyroxenitic Gabbro Pegmatitic Gabbro Sheared Gabbro </p> <p> These units are evident in thin section and are distinguishable both modally and textUrally. In most cases, variations in the chemistry and norms reflect the units mapped in the field. </p> <p> Many features of the sill are analogous to other intrusions, and comparisons have been drawn and theories incorporated to explain these features in the Gabbro Lake Sill. </p>en_US
dc.language.isoenen_US
dc.subjectPetrographyen_US
dc.subjectGeochemistryen_US
dc.subjectGabbro Lake Sillen_US
dc.subjectNorthwest Ontarioen_US
dc.titlePetrography and Geochemistry of the Gabbro Lake Sill, Superior Province, Northwest Ontarioen_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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