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|Title:||Developing a tectonic framework for the Southern Curnamona Cu - Au Province : geochemical and radiogenic isotope applications|
|Author:||Rutherford, Lachlan Stuart|
|School/Discipline:||School of Earth and Environmental Sciences|
|Abstract:||"Two independent geochronological techniques specifically targeting post-kinematic or late-stage growth of kyanite, staurolite and late-stage garnet in the southern Curnamona Province has found that these minerals grew during the Delamerian Orogeny (~530-500 Ma). Prograde metamorphism during the Delamerian Orogeny attained kyanite-staurolite-garnet grade (amphibolite-facies). Previous interpretations of an anticlockwise P-T path for the Olarian Orogeny need revising, as these interpretations have been shown in this study to be based on textural relationships spanning ~1100 million years. This highlights the importance of in situ geochronological techniques in defining robust P-T-t paths for a region." --p. 121 of source document.|
|Advisor:||Hand, Martin Phillip|
Barovich, Karin Marie
Foden, John David
|Dissertation Note:||Thesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.|
|Subject:||Metamorphism (Geology) South Australia Olary Region|
Metamorphism (Geology) New South Wales Broken Hill Region.
Geology, Stratigraphic Proterozoic
|Keywords:||geology Australia Curnamona Province, geophysics|
|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 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:||Research Theses|
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