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A petrographic study of the granite wash in the clear hills area, Alberta.

“Granite wash” refers to partly reworked residual material overlying the basement and underlying marine strata. Its distribution is irregular and its age varies from place to place. Recent oil discoveries have made the Granite Wash economically interesting. Representative samples from a cored wall, Gulf Clear Rills 14-10, on the northern flank of the Peace River high, were subjected to detailed petrographic examination. Only the lowest few feet of core, if any, were found to be basement, consisting of tectonized granitoid gneiss. The rock types studied indicate no mineralogical variations in the source rock, only variations in degree of crushing and hence grain size.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111372
Date January 1957
CreatorsZwartendyk, Jan.
ContributorsStearn, C. (Supervisor)
PublisherMcGill University
Source SetsLibrary and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada
LanguageEnglish
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation
Formatapplication/pdf
CoverageMaster of Science. (Department of Earth Sciences.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: NNNNNNNNN, Theses scanned by McGill Library.

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