The geothermal field m our study area is jointly controlled by faults, lithology, caprock buried depth and hydrology, has a relatively high geothermal gradient which ascends southwards.

• 研究区地温场的展布主要受构造断裂、地层岩性、盖层埋深、水文地质条件等控制，地温温度较高，自北向南地温总体呈增高趋势。