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Syntectonic granite in the southern margin of the Palaeoproterozoic Capricorn Orogen, Western Australia

โœ Scribed by Occhipinti, S. A.; Sheppard, S.; Nelson, D. R.; Myers, J. S.; Tyler, I. M.


Book ID
126744762
Publisher
Taylor and Francis Group
Year
1998
Tongue
English
Weight
393 KB
Volume
45
Category
Article
ISSN
0812-0099

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The Palaeoproterozoic Capricorn Formation near Ashburton Downs in northwestern Australia formed during the latter stages of the convergence of the Pilbara and Yilgarn Cratons. Palaeocurrent and facies analyses show that the southwesterly derived sediments were deposited in terrestrial environments a