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通过对浙江省武义县溪里地热区区域地质、矿产地质等资料的分析,并结合地热地质调查、钻探及物探等勘查工作,基本查明溪里地热地质特征、热储结构与空间分布,证实溪里地下热水的分布受武义盆地断裂构造控制,且与萤石矿带的成因联系,热水由大气降水沿导水、储水的构造系统深循环形成。
Through the analysis of geology and mineral geology in the geothermal area of Xili in Wuyi County, Zhejiang Province, and combined with the geothermal geological survey, drilling and geophysical prospecting work, the geothermal geological characteristics, thermal storage structure and spatial distribution in Xili Lake are basically ascertained The distribution of underground hot water in the creek is controlled by the fault structure of the Wuyi Basin and is related to the genesis of the fluorite ore zone. Hot water is formed by the deep circulation of the aquifer and aquifer tectonic systems by atmospheric precipitation.