Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/84193
Type: Thesis
Title: Geology of part of the Springton-Cambrai area.
Author: Kaewbaidhoon, S.
Issue Date: 1951
School/Discipline: School of Physical Sciences
Abstract: The report deals with the general geology of part of the East Mount Lofty Ranges on lower part of Cambrai sheet and upper part of Mannum Sheet, which is the result of geological mapping during 1951. The rocks of the area are mainly, schists, quartzites, and marbles of Kanmantoo Series and Palmer Granite. The structure of Kanmantoo Series is pitching north synclinal fold, of which, the east limb was cut off by big fault separating the Mount Lofty Ranges from the Murray Plains. The Palmer Granite intruded the Series about the middle of the area.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1951
Where: Kanmantoo Province, east Mt Lofty fold belt, South Australia
Keywords: Honours; Geology; Kanmantoo Group; stratigraphy; structure; petrology; metamorphism; igneous rocks; granites; mining
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

Files in This Item:
File Description SizeFormat 
01frontGeoHon.pdf597.58 kBAdobe PDFView/Open
02wholeGeoHon.pdf1.21 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.