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dc.contributor.author Stott, D. F. en_US
dc.date.accessioned 2011-06-06T18:13:23Z
dc.date.available 2011-06-06T18:13:23Z
dc.date.issued 1954 en_US
dc.identifier ocm72805841 en_US
dc.identifier.uri http://hdl.handle.net/1993/4670
dc.description.abstract The Jurassic system extends from the Williston basin into Manitoba where it unconformably lies on Paleozoic rocks and below Cretaceous sediments. It is divided into four formations, which are from the base upward; Amaranth, Piper, Rierdon, and Swift. An assemblage of gypsiferous red beds, anhydrite, and dolomite are included in the Amaranth formation. The remainder of the Middle Jurassic shales, argillaceous and oolitic limestones is placed in the Piper formation. The Upper Jurassic strata consist of the Rierdon formation which contains varicoloured shales and thin bands of limestone and the Swift formation which contains sand and shale beds. Depositional conditions and correlation problems related to the basal red beds, to the division between Middle and Upper Jurassic sediments, and to the upper limit of the Jurassic system are discussed. en_US
dc.format.extent 131 p. : en_US
dc.format.extent 33352983 bytes
dc.format.mimetype application/pdf
dc.language en en_US
dc.language.iso en_US
dc.rights The reproduction of this thesis has been made available by authority of the copyright owner solely for the purpose of private study and research, and may only be reproduced and copied as permitted by copyright laws or with express written authorization from the copyright owner. en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title The Jurassic stratigraphy of Manitoba en_US
dc.type info:eu-repo/semantics/masterThesis
dc.degree.discipline Geology en_US


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