Geology of the Mt. Osmond area, South Australia
Date
1964
Authors
Yong, C. K.
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Thesis
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Abstract
The area of uniform stratigraphic sequence studied is essentially part of the west limb of a regional anticlinorium. Both the mesoscopic and the macroscopic folds have the same concentric style. Two different explanations are suggested for the apparently odd occurrence of a 30-foot arkosic quartzite band near the top of the northern foothills.
School/Discipline
School of Physical Sciences
Dissertation Note
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1964
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