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dc.contributor.advisorAitken, J. D.
dc.contributor.authorPoulton, Terence Patrick
dc.coverage.spatial2000001265en
dc.date.accessioned2005-07-19T20:56:12Z
dc.date.available2005-07-19T20:56:12Z
dc.date.issued1970
dc.identifier82481544en
dc.identifier.citationPoulton, T. P. (1970). Stratigraphy and sedimentology, Horsethief Creek Formation, northern Dogtooth Mountains, British Columbia (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/12690en_US
dc.identifier.other82481544en
dc.identifier.urihttp://hdl.handle.net/1880/14537
dc.descriptionBibliography: p. 92-97.en
dc.description.abstractIn the northern Dogtooth Mountains, the exposed Precambrian rocks are represented by the Horsethief Creek Formation, 700o+ ft. thick, contorted and faulted, consisting of four members in the following upward sequence: Feldspathic Grit Member, Lower Slate Member, Limestone Member, and Upper Shale Member. The Feldspathic Grit Member is interpreted as mainly delta-front elastic deposits and is recognized over the total study area. Available evidence suggests the sediments were derived from the east. The Lower Slate Member is mainly slate, interpreted as marine, with upper parts probably equivalent in age to parts of the Limestone Member. The Limestone Member consists of carbonate and elastic rocks varying from supratidal to probably "deeper" water deposits. Slumped units and close lateral relationship of shallow and "deeper" water deposits suggest minor penecontemporaneous tectonism. The Upper Shale Member is mainly dolomitic elastic rocks, and is recognizable with certainty only in eastern parts of the area. At Rogers Pass, and in areas where metamorphic minerals higher in grade than chlorite occur, identification of the members is hazardous. Locally, garnetiferous rocks occur, but most of the area contains rocks probably representing the biotite zone. The sequence of members is recognizable in homotaxial rocks throughout the southern Canadian Cordillera. Local absence of this sequence may be due to facies changes, and/or erosion at the sub-Cambrian unconformity. The base of the Cambrian Hamill Group is sharply defined in some places and apparently gradational in others.en
dc.format.extent118 leaves : ill. ; 30 cm.en
dc.language.isoeng
dc.relationAdditional Copy: QE 655 P67 1970Gen
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
dc.subject.lcshGeology, Stratigraphic - Pre-Cambrian
dc.subject.lcshGeology - Dogtooth Mountains
dc.subject.lcshStratigraphic correlation
dc.titleStratigraphy and sedimentology, Horsethief Creek Formation, northern Dogtooth Mountains, British Columbia
dc.typemaster thesis
dc.publisher.institutionUniversity of Calgaryen
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/12690
thesis.degree.nameMaster of Science
thesis.degree.nameMS
thesis.degree.nameMSc
thesis.degree.disciplineGeology
thesis.degree.grantorUniversity of Calgary
dc.publisher.placeCalgaryen
ucalgary.thesis.notesPLen
ucalgary.thesis.additionalcopyQE 655 P67 1970Gen
ucalgary.thesis.uarcreleasenoen
ucalgary.item.requestcopytrue


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