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本文根据西藏高原地热活动与温泉分布和各种地球物理场的特征,进行了综合分析与研究,给出了地壳深部要素的统一解释。说明了西藏高原水热分布及其活动原因是由于地壳介质中温度很高,地壳中存在着物质的熔融或部分熔融所致。水热显示是受深部地壳构造与物质运移所制约,其热能是由印度板块与欧亚板块碰撞过程中所产生的热量和岩浆上涌所提供的。
Based on the characteristics of geothermal activity and distribution of hot springs in Tibet Plateau and various geophysical fields, the paper makes a comprehensive analysis and research and gives a unified explanation of the deep elements in the crust. It shows that the hydrothermal distribution and its activities in the Tibetan plateau are due to the high temperature in the crustal medium and the melting of the crust or the partial melting of the crust. Hydrothermal display is constrained by the deep crustal structure and material movement, the thermal energy is provided by the heat and magmatic upwelling produced during the collision between the Indian and Eurasian plates.