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中国西藏高原地热活动强烈,喜马拉雅地带是一条走向近东西向延伸的地热带。这里没有近代火山活动,但却具有水热爆炸、间歇喷泉、沸泉和种类繁多的热泉及温泉等典型的近代火山活动地带的特色。 根据喜马拉雅地热带的分布,水热地球化学与其活动特征、地质构造与地球物理场背景等说明这种地热活动具有板块边缘的特征,它是印度板块早期俯冲与两大陆板块近期持续碰撞与挤压作用下的结果。反映了大陆板块碰撞挤压过渡带的水热活动标志。
Geothermal activity in the Tibetan plateau in China is intense. The Himalayan zone is a geothermal zone that extends toward the east and west. There is no modern volcanic activity, but features typical modern volcanic activity such as hydrothermal explosions, intermittent fountains, boiling springs and a wide variety of hot springs and hot springs. According to the distribution of Himalayan geothermal belt, hydrothermal geochemistry and its activity characteristics, geological structure and geophysical field background shows that this geothermal activity has the characteristics of the plate edge, which is the Indian Plate early subduction and the recent collision between the two continental plates and crush Under the effect of the results. Reflects the continental plate collision squeeze transition zone hydrothermal activity signs.