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The Ghost River and related formations between the Athabaska and Smoky Rivers, Alberta.

Note: Missing page 28. / In spite of the many studies of the various Paleozoic systems in the Rocky Mountains, no one has dealt satisfactorily with the beds immediately below the known Upper Devonian strata. Several factors are involved. The beds are not so resistant as those above and they are usually found at the base of fault blocks. Thus the sections are talus covered and incomplete due to faulting. Fossils are rare and there is no adequate means of correlation between widely spaced sections.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.109680
Date January 1954
CreatorsMacLean, Donald. W.
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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