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The 4–10km-thick Bangemall Supergroup, comprising the Edmund and Collier Groups, was deposited between 1620 and 1070Ma in response to intracratonic extensional reactivation of the Paleoproterozoic compressional Capricorn Orogen. The supergroup can be further divided into six depositional packages bounded by unconformities or major marine flooding surfaces. U–Pb dating of over 1200 detrital zircon...
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