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RB 81/00052 Carnot Gneisses, southern-most Eyre Peninsula.
The Carnot Gneisses form an extensive layered sequence that crops out in southernmost Eyre Peninsula. They consist of garnetiferous quartzofeldspathic gneiss, hypersthene gneiss, granitic gneiss and basic granulite. Rb/Sr whole rock studies indicate a...-
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Published: 01 Jul 1981
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RB 97/00057 Gawler Craton excursion guide - September 21-26, 1997.
This 5-day field excursion was mounted by the GSSA to inform government and industry participants about significant newly identified geological features within the central Gawler Craton which are the subjects of ongoing study. The itinerary chosen...-
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Published: 19 Sep 1997
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Ceduna. Annual reports and final report to licence full surrender, for the period 31/8/1996 to 17/7/2000.
Joint venture exploration over an area extending for 40, 35 and 50 km respectively west, north and east of Ceduna targeted Archaean and Proterozoic Yarlbrinda - style Au and Ernest Henry / Olympic Dam style Cu-Au associated with shear zones and...-
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Tungketta Hill. Annual reports and final report to licence full surrender, for the period 7/3/2007 to 9/6/2015.
An area centred ~25km south-east of Elliston on south-western Eyre Peninsula and which abuts the coast of the Great Australian Bight has been explored for possible buried economic occurrences of Archaean igneous intrusive body - related nickel...-
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RB 2016/00019 Neoarchaean to earliest Palaeoproterozoic magmatism in the southern Gawler Craton: petrogenesis of the Minbrie Gneiss and Carpa Granite.
This report presents geochemical constraints on the evolution of the Minbrie Gneiss and Carpa Granite, two magmatic units occurring in the southern Gawler Craton. These two units were previously assigned to the Palaeoproterozoic Lincoln Complex,...-
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Published: 01 Jan 2017
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Bull 055 A geochronological framework for the Gawler Craton, South Australia
This bulletin contains geochronological data and interpretations from the Gawler Craton of South Australia that have been completed by Mark Fanning of The Australian National University, by Geological Survey of South Australia personnel, and by...-
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