摘要
分析了龙门地热田勘查、开发现状,并对地热田成因进行了探讨,认为龙门地热田热储为寒武系灰岩,盖层为第四系黏土层,第三系、石炭系、二叠系及三叠系地层中的泥岩和砂质泥岩层,热源来自地下深部岩浆侵入体,控热构造为草店断层及魏湾断层。
Analysed geothermal field exploration, developing status quo of Longmen geothermal field, the causes of geothermal fields were also explored,It was thought that geothermal reservoir of Longmen geothermal field is the Cambrian limestone, cap rocks are shale and sandy shale of the Quaternary, Tertiary, Carboniferous, Permian and Triassic strata, heat is from magma intrusion in deep underground, and thermal control structures are Caodian fault and Weiwan fault.
出处
《中州煤炭》
2014年第2期102-104,共3页
Zhongzhou Coal
关键词
龙门地热田
控热构造
热储结构
水化学特征
Longmen geothermal field
thermal control structure
geothermal reservoir structure
hydrochemical characteristics
