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RB 2008/00003 The Corunna Conglomerate, Gawler Craton: a review of the sedimentology and new U-Pb zircon geochronology.
The Corunna Conglomerate is a sequence of unmetamorphosed fluvial to shallow marine sediments, comprising conglomerates, sandstones and siltstones, which were deposited in active fault grabens in the eastern Gawler Craton. It is found on the...-
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Published: 01 Apr 2008
