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This page is a summary of: Sichuan Basin and beyond: Eastward foreland growth of the Tibetan Plateau from an integration of Late Cretaceous-Cenozoic fission track and (U-Th)/He ages of the eastern Tibetan Plateau, Qinling, and Daba Shan, Journal of Geophysical Research Solid Earth, June 2017, Wiley,
DOI: 10.1002/2016jb013751.
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