Multiple uplift and exhumation of the Southeastern Tibetan Plateau: Evidence from Low-Temperature Thermochronology

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.

为揭示青藏高原生长的动力学机制与演化时序，本研究针对青藏高原东南部（SE）的中生代花岗岩与闪长岩，提供了磷灰石裂变径迹热年代学（apatite fission track thermochronological）数据及反演热模拟结果。