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In the Jiangnan orogen, a clear angular unconformity between the Precambrian basement sequences and the overlying Neoproterozoic sedimentary strata (e.g. the Danzhou/Banxi Group, younger than ca. 800Ma) marks the collisional orogenesis (the Jinning orogeny) between the Yangtze and Cathaysia Blocks. In contrast to the upright, open folds in the Danzhou/Banxi Group, the basement sequences were deformed...
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