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腾冲地区地热水分布广泛,经过初步调查,发现它的放射性水文地球化学具有许多特点。目前,有许多资料说明腾冲地热水的形成主要与现代火山作用有关。该区地热水大多分布在现代火山群附近,其出露状态和化学成分具有岩浆期后的某些特征,而与一般地下水成分有明显差别。其热源属玄武岩岩浆热,水源为大气降水。这些水进入地热系统后,被加温
Geothermal water in Tengchong area is widely distributed. After preliminary investigation, it found that radioactive hydrogeochemistry has many characteristics. At present, there is a lot of information that explains the formation of hot water in Tengchong is mainly related to the role of modern volcanoes. Most of the geothermal water in the area is distributed near the modern volcanic group, and the exposed state and chemical composition have certain characteristics after magmatic period, which are obviously different from the general groundwater composition. The heat source is a basalt magmatic heat, water for the precipitation. After the water enters the geothermal system, it is warmed