CAJ | 학술논문

眉县汤峪地热田位于秦岭山地与汾渭地堑的接触地带，属于典型的断裂裂隙型地热田。笔者基于物探和水文地球化学方面工作对该区进行了系统研究。结果表明：汤峪地热田内主要分布着东西向和近南北向的两组断层构造。这两组构造也成为研究区内主要的导（控）水和导（控）热构造，控制着地热田的分布。地热田内热储层为断层破碎带和裂隙发育地段，具有良好的储水储热性能。地热水由研究区以南的秦岭山区得到补给，补给水源以大气降水为主，补给水径流向地下渗透，经热源加热后成为地热流体。热水在区内断层交汇处上涌，最终形成地热田。
미현탕욕지열전위우진령산지여분위지참적접촉지대，속우전형적단렬렬극형지열전。필자기우물탐화수문지구화학방면공작대해구진행료계통연구。결과표명：탕욕지열전내주요분포착동서향화근남북향적량조단층구조。저량조구조야성위연구구내주요적도（공）수화도（공）열구조，공제착지열전적분포。지열전내열저층위단층파쇄대화렬극발육지단，구유량호적저수저열성능。지열수유연구구이남적진령산구득도보급，보급수원이대기강수위주，보급수경류향지하삼투，경열원가열후성위지열류체。열수재구내단층교회처상용，최종형성지열전。
Tangyu geothermal field in Mei Country is located in the contact area of Qinling Mountains and Fen-wei graben, belongs to typical fracture type. Based on geophysical prospecting and hydrogeochemical study, we made conclusions:there are two groups of fault structure zones in the geothermal field mainly with east-west di-rection and south-north direction. The two groups of faults have become the most important faults in the study ar-ea. They control not only the water and heat but also the distribution of geothermal field. The heat reservoir of Tangyu geothermal field is faults and fractured zone which can restore a lot of water and heat. The supply area of hot water is in the south of Qinling Mountains. Feed water run down to the underground, then to be the geother-mal fluid after heat source heating. When the hot water encounters faults, it begins to move towards the land sur-face.