Multiple uplift and exhumation of the Southeastern Tibetan Plateau: Evidence from Low-Temperature Thermochronology
Published: 30 November 2022| Version 2 | DOI: 10.17632/7nvfzhywpp.2
Contributor:
Limin WuDescription
In order to reveal the dynamic mechanism and timing of the growth of the Tibetan Plateau, we present apatite fission track thermochronological data and inverse thermal modeling results for the Mesozoic granitic and dioritic rocks in the southeastern (SE) Tibetan Plateau.
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Institutions
University of the Chinese Academy of Sciences
Categories
Apatite, Fission-Track Thermochronology