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The Neoproterozoic Danzhou Group, composed of siliciclastic sedimentary rocks interbedded with minor carbonate and volcanic rocks in the southeastern Yangtze Block, South China, is thought to be related to the breakup of Rodinia. Detrital zircon ages constrain the deposition of the Danzhou Group at ~770Ma and ~730Ma. The Danzhou Group contains dominant Neoproterozoic detrital zircon grains (~740–900Ma)...
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