Abstract:Wenquantang hot spring is one of the most important hot spring in Weihai city. Combining with geochemical and geological survey methods, the forming model of Wenquantang hot spring has been analyzed. In this paper, hydrochemistry test and hydrogen and oxygen isotopes test have been carried out by collecting hot spring water samples. Through analyzing water quality type and recharge source of hot spring water, water cycle depth has been estimated, and combining with geothermal geological conditions, the geothermal genetic mechanism has been further enriched. As showed by Piper diagram of water chemistry, the hot spring water belongs to NaCl type. As showed by water rock interaction analysis, hot spring water has the characteristics of shallow water, and the stable isotope values of hydrogen and oxygen are distributed near the atmospheric precipitation line in eastern China. It is speculated that the hot spring water is mainly affected by shallow water, such as atmospheric precipitation, surface water and groundwater. According to the elevation effect of 2H isotope, the recharge elevation of the hot spring is calculated to be 225~265m. According to landform characteristics of the surrounding area, the mountain in the south is about 240m, so it is determined that the mountain in the south is the main supply source. It is regarded that the atmospheric precipitation converges into the basin from the mountain in the south of Wenquantang hot spring. The atmospheric precipitation, surface water and groundwater exchange heat in the deep through the fault fracture zone to form hot spring water, then migrate to the surface to form hot spring. Through analysis of genetic model, it will provide scientific basis for the evaluation and development of hot spring resources, and some references for the research and development of other hot springs in Weihai area.