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Research on the relationship between geothermal field and the tectonic in Himalayas and its surrounding regions

机译:喜马拉雅山地区与周边地区的地热场与构造关系研究

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In this article, based on the terrestrial heat flow data, the terrestrial heat flow map in the area, geothermal gradient map and different depth geothermal contour map of study area within the Territory of China, I explored respectively the relationship between geothermal field and tectonic, geologic structures by analyzing respectively the corresponding relationships between the structural diagram and terrestrial heat flow diagram, temperature contour map, geothermal gradient map in study area. The main conclusions are as follows. Geothermal field has been restricted by the India plate and Eurasian plate collision. So the study area as a whole is a geothermal abnormal area. Features of regional geological structure control the geothermal (low distribution. Geothermal abrupt changing occurs between different tectonic units.
机译:在本文的基础上,基于地面热流数据,地区的地面热流图,地热梯度图和中国境内的研究区域的不同深度地热轮廓图,我探讨了地热场和构造之间的关系,通过分析结构图和地面热流图,温度等高图,研究区域地热梯度图之间的相应关系。主要结论如下。地热领域受到印度板材和欧亚平板碰撞的限制。因此,研究区域整体是地热异常区域。区域地质结构的特点控制地热(低分布。不同构造单元之间发生地热突变变化。

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