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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/138342
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dc.contributor.authorGabrieel, C. M.-
dc.coverage.spatialAdelaide Geosyncline, Flinders Ranges, South Australia-
dc.date.issued1971-
dc.identifier.urihttps://hdl.handle.net/2440/138342-
dc.descriptionThis item is only available electronically.en
dc.description.abstractMapping in the Emu Bore area has disclosed hitherto unmapped Parachilna Formation, Brachina Formation and Billy Creek Formation as well as a diapiric body. The entire Upper Proterozoic to Upper Lower Cambrian sequence is a shallow water one marked by periods of transgression and regression which has resulted in the deposition of limestones and red beds. The Lower Cambrian rocks consist entirely of limestones as opposed to those in the type section in Wilkawillina Gorge where clastic units are included.en
dc.language.isoenen
dc.subjectHonours; Geology; Proterozoic; Cambrian; Flinders Ranges; stratigraphy; environments of deposition; diapirsen
dc.titleThe geology of the Proterozoic and Cambrian of the Emu Bore area, Flinders Ranges, South Australiaen
dc.typeThesisen
dc.contributor.schoolSchool of Physical Sciencesen
dc.provenanceThis electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the author of this thesis and do not wish it to be made publicly available, or you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legalsen
dc.description.dissertationThesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1971-
Appears in Collections:School of Physical Sciences

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