摘要
通过对浙江省横店镇忠信堂地热区域地质、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,基本查明忠信堂地热地质特征、热储结构与空间分布,证实忠信堂地下热水的分布受断裂构造控制,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。
Based on the analysis of the geological and mineral data of Zhongxintang geothermal area in Hengdian Town, Zhejiang Province, and combined with geothermal geological survey, drilling and geophysical exploration, the geothermal geological characteristics, thermal reservoir structure and spatial distribution of Zhongxintang geothermal area are basically figured out. It is confirmed that the distribution of geothermal water in Zhongxintang is controlled by fault structure and related to the genesis of fluorite ore belt, and hot water is formed by deep circulation of atmospheric precipitation along the structural system of water diversion and storage.
出处
《科技创新与应用》
2019年第24期87-89,共3页
Technology Innovation and Application
关键词
忠信堂
地热
热储
Zhongxintang
geothermal
thermal storage