摘要
The first set of terrestrial heat flow data on the Qing-Zang (Qinghai-Xizang) Plateau was obtained in the Yamzho and Puma lakes in 1982 (the average values are 146 mW/m^2 and 91 mW/m^2 respectively). On this basis a multi-layered abnormal crust and upper mantle thermal structure model was successively summarized. Furthermore, the mechanism of the thermo-tectonic evolution of the uplift of the Qing-Zang Plateau
基金
Project supported by the National Natural Science Foundation of China
