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.
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释义
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。
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