Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/115253
Type: Thesis
Title: The structural geology of the Rapid Bay – Second Valley area, South Australia
Author: Kirk, A. C.
Issue Date: 1963
School/Discipline: School of Physical Sciences
Abstract: The area is structurally homogeneous with respect to a single fold axis. The style of folding is recumbent, with the axial plane dipping gently to the east. It is postulated that the anticlines close \to the south, in accord with the regional anticlinorium. Extensive thrust faulting has accompanied this folding. There is some evidence for a second, minor period of deformation superposed on the first. The pressure exerted during the intense folding of the area is thought to be the dominant cause of metamorphism, with only relatively low temperatures involved. The rocks contain low grade mineral assemblages, and are assigned to the quartz m- albite – epidote – biotite subfacies of the greenschist facies.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1963
Where: Adelaide Geosyncline, Stansbury Basin, Kanmantoo Trough, Fleurieu Peninsula, South Australia
Keywords: Honours; Geology;Neoproterozoic; Cambrian; stratigraphy; structure; metamorphism; Adelaide Geosyncline
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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