论文部分内容阅读
在江西省进行了大地热流测量,并对江西境内的水热系统进行了系统的同位素和地球化学研究。结果表明江西地下热水属于中、低温对流型地热系统,它们与深部有岩浆热源的高温地热系统有明显区别。同时证明同位素和地球化学技术对地热资源勘查十分有效。
The geothermal heat flow measurement was carried out in Jiangxi Province, and the systematic isotope and geochemical study of the hydrothermal system in Jiangxi Province was carried out. The results show that the underground hot water in Jiangxi belongs to the medium and low temperature convective geothermal systems, which are obviously different from the high temperature geothermal systems with the magma source in the deep part. At the same time, it is proved that isotope and geochemical techniques are very effective for geothermal exploration.