Multiple uplift and exhumation history of the Southeastern Tibetan Plateau: Evidence from Low-Temperature Thermochronology
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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.
提供机构:
Limin Wu



