Geochemical characteristics and origin of geothermal water in the Dezhou hollow;

Finite element numerical simulation of the geothermal water system in the hot spring area in Fuzhou;

Based on the geological and geophysical investigati on in geothermal anomaly area of Fashui hot spring,the distribution conditions o f underground thermal water and the geological\|geophysical characteristics in t he area are analyzed.

The underground thermal water in Zhengzhou City hosted in the fluviolacustrine facies loose beds in the Pliocene, Miocene epoch of Neogene Period, and it belongs to the underground moderate temperature hot water in the zone of subsidence.

In order to investigate the distribution of underground thermal water of the hot spring, we used the direct current prospecting to determine the fracture belt bearing underground thermal water with the near source field electric profiling.

Evolution of thermal groundwater resources under the conditions of exploitation:A preliminary analysis.;

But it has relatively rich thermal groundwater resources.

Long-term exploitation of thermal groundwater in deep-seated aquifers has led to a continual falling in water levels at geothermal wells.

On the basis of analyzing the chemical character of underground hot water, the formation mechanism of the chemical composition and its genesis are discussed in this paper.

Underground hot water occurs widely in the Kunlun, Tianshan and Artai mountains of Xinjiang.