摘要
分析青藏高原几条地球物理研究剖面，并对其地表大地热流和岩石圈温度场进行计算．结果表明：青藏高原温度场分布具南北分带、东西分块的特征．进一步论述了青藏高原东西部的地质构造差异、热差异及其地球动力学意义．
Using geological and geophysical results, heat flow values and temperature distribution were calculated along the four geophysical profiles in Qinghai - Tibet plateau. The temperature distribution shows such a characteristic that the temperature in different terrain is apparently different. The temper-attire is apparently different even in the same terrain from east to west. These differences, combined with tectonic difference, are meaningful to geodynamic process of the Qinghai - Tibet plateau.
出处
《地球物理学进展》
CSCD
2001年第3期12-20,共9页
Progress in Geophysics
基金
中国科学院项目(KZ951-A1-204)
国家自然科学基金项目(49604055)联合支持.
