Strong variability in the thermal structure of Tibetan Lithosphere
收藏NIAID Data Ecosystem2026-03-13 收录
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We present a model of ‘thermal lithospheric thickness’ (the depth where the geotherm reaches a temperature of 1300°C) and surface heat flow in Tibet and adjacent regions based on the new thermal-isostasy method.
创建时间:
2022-02-02



