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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/98389
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dc.contributor.authorPoole, L. E.-
dc.coverage.spatialKanmantoo Trough, Mt Lofty Ranges, South Australia-
dc.date.issued1969-
dc.identifier.urihttp://hdl.handle.net/2440/98389-
dc.descriptionThis item is only available electronically.en
dc.description.abstractThere have been at least two periods of deformation in this area. The (probable) first deformation is the most prominent and has an axial plane schistosity. The second deformation deforms this schistosity and is only generally manifest as crenulations. “Deformation zones” exist throughout the area and can be interpreted as either reverse faults or transposed limbs of folds. It is probable that the major metamorphic phase took place during the first deformation. The ore deposits in the region show a structural and stratigraphic control.en
dc.language.isoenen
dc.subjectHonours; Geology; structure; deformationen
dc.titleThe structural geology of an area south of Kanmantoo, S.A.en
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 Earth and Environmental Sciences, 1969-
Appears in Collections:School of Physical Sciences

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