-
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...-
Document
Published: 01 Jul 1981
-
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...-
Document
-
RB 2007/00015 Geochronology of the Gawler Craton, South Australia.
Geochronology enables us to determine the age of rocks and minerals. The variety of isotopic geochronological techniques give complementary information on, for example, the timing of igneous or metamorphic crystallisation, as is often the case for the...-
Document
Published: 01 Sep 2007
-
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,...-
Document
Published: 01 Jan 2017
