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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/18760
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DC FieldValueLanguage
dc.contributor.advisorMcNutt, R. H.-
dc.contributor.authorLeriche, Peter-
dc.date.accessioned2016-06-27T18:17:36Z-
dc.date.available2016-01-25T19:02:43Z-
dc.date.available2016-06-27T18:17:36Z-
dc.date.issued1980-04-
dc.identifier.urihttp://hdl.handle.net/11375/18760-
dc.description.abstract<p> The thesis pluton is part of the Saanich granodiorite batholithic complex on south-east Vancouver Island. The pluton is 11 Km by 2 Km, elliptical and trends NW-SE. </p> <p> Petrographically its mineral composition is that of a granodiorite. Alteration is fairly intense as shown by plagioclase and potassium feldspar altering to sericite, as well as biotite and hornblende altering to chlorite. Deformation textures were observed in the form of strained quartz and bent cleavage in biotite. </p> <p> From chemical analyses it was found that the granodiorite represents part of a fractionation process along a calc-alkaline trend. The magma was derived from partial melting of the lower crust. </p>en_US
dc.language.isoenen_US
dc.subjectpetrologyen_US
dc.subjectgeochemistryen_US
dc.subjectplutonen_US
dc.subjectgranodioriteen_US
dc.titlePetrology and Geochemistry of a Pluton of the Saanich Granodiorite Complex, Helmcken Land District, Vancouver Island, B. C.en_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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