Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/119984
Type: Thesis
Title: The Late Precambrian geology of the Wyacca Bluff – Buckaringa Gorge area, Flinders Ranges, South Australia
Author: Miller, R. K.
Issue Date: 1975
School/Discipline: School of Physical Sciences
Abstract: Detailed lithostratigraphic mapping of the Late Precambrian sequence extending from the Tapley Hill Formation in the Umberatana Group, to the A.B.C. Range Quartzite in the Wilpena Group in the Wyacca Bluff - Buckaringa Gorge area, has indicated 18 mappable units. These may be lithologically uniform, or contain several distinct or gradational lithologies, ranging from almost pure carbonates to clastics with only minor carbonate content. Stromatolite growth proliferated during deposition of the Brighton Limestone and the morphology of these stromatolites is described. Minor stromatolite growth occurred during deposition of the upper parts of the Tapley Hill Formation and Etina Limestone Member respectively. Deposition occurred under shallow marine conditions, in environments ranging from below wave base, to supratidal. Comparison with the Hallett Cove - Marino area suggests that similar environments prevailed in both areas, although not necessarily synchronously. The sequence is located on the eastern side of a shallow southerly plunging anticline, which has been truncated on the western side by Wyacca Fault.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1975
Where: Adelaide Geosyncline, Flinders Ranges, South Australia
Keywords: Honours; Geology; Adelaide Geosyncline; Adelaidean; Precambrian; stratigraphy; stromatolites; depositional environments
Description: This item is only available electronically.
Provenance: This 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/legals
Appears in Collections:School of Physical Sciences

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