Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/115218
Type: Thesis
Title: Geology of the Delamere area, South Australia
Author: Leslie, W. C.
Issue Date: 1962
School/Discipline: School of Physical Sciences
Abstract: In Stockyard Creek near Delamere there is a tilted sedimentary sequence with a stratigraphic thickness greater than 5500 feet. This is a portion of the sediments of the Adelaide Geosyncline. The finding of Lower Cambrian fossils (hyolithids) in two formations of the Delamere Marble, has allowed relative dating of the sequence which is given as Upper Proterozoic and Lower Cambrian age. The base of the Cambrian has been taken as the lowest known occurrence of the hyolithids. A description of the geology of the area and a detailed account of the lithology of the Stockyard Creek section is given, and where possible, by using lithological similarity and fossil evidence the sequence has been correlated with the type areas.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1962
Where: Adelaide Geosyncline, Stansbury Basin, Kanmantoo Trough, Fleurieu Peninsula, South Australia
Keywords: Honours; Geology; Neoproterozoic; Cambrian; stratigraphy; palaeontology; 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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