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Late Pleistocene shortening rate on the northern margin of the Yanqi Basin, southeastern Tian Shan, NW China
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文摘

Active structures penetrated and deformed the intermontane basin across the Tian Shan.

Quantifying slip rates of faults on the margins of intermontane basin, Tian Shan.

Strong earthquake are controlled by active faults distributed across the Tian Shan.

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