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The Centralian Superbasin is a concept connecting Neoproterozoic successions that presently occur in separate structural basins in central Australia into a once-continuous depositional system. The superbasin is thought to have been initiated ∼830Ma, coevally with the breakup of Rodinia, by a mantle plume centred under the central Adelaide Geosyncline, South Australia. The superbasin is thought to...
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