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Fisson-track constrains on superposed folding in the Beishan orogenic belt, southernmost Altaids
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文摘

Superposed fold developed in the Hongyanjing Basin, Beishan range, southern most Altaids.

Basin thermal history shows heating and cooling process in end Permian to late Cretaceous.

Apatite fission track results related to end Permian closure of Paleo-Asian Ocean and Mesozoic orogenesis.

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