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Triassic Braided Gravelly River Deposits at Pt. Lepreau, New Brunswick

dc.contributor.advisorMiddleton, G. V.
dc.contributor.authorLoosemore, Gary J.
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-06-08T18:37:36Z
dc.date.available2016-06-08T18:37:36Z
dc.date.issued1984-04
dc.description.abstract<p> A detailed section of the Duck Cove Member (Nadon, 1981) of the Triassic Lepreau Formation of Southern New Brunswick is measured.</p> <p> The section consists of a complex sequence of conglomerates and sandstones with a minor occurrence of mudstones and breccia. A description of the facies is provided and an interpretation is based on observations of ancient and marine braided stream deposits of Miall (1978) and Allen (1983). The Markov chain analysis is used to describe the vertical succession of facies.</p> <p> Paleoflow indicators suggest a flow towards the south or southeast. However this conclusion is based on limited availability of data.</p>en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19485
dc.language.isoen_USen_US
dc.subjecttriassic, braided, gravelly, river, deposits, formation, sandstones, mudstones, brecciaen_US
dc.titleTriassic Braided Gravelly River Deposits at Pt. Lepreau, New Brunswicken_US
dc.typeThesisen_US

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