神堂沟地热田形成与地质构造的关系  

On the Relation between the Formation of Shentanggou Geothermal Field and Geological Structure

作　　者：侯玉新[1] 慕秀琴 

机构地区：[1]山西煤田水文地质229队,山西太原030006

出　　处：《中国煤田地质》2004年第6期22-23,35,共3页Coal Geology of China

摘　　要：地热田的形成往往与地质构造有着千丝万缕的联系,神堂沟即是如此。笔者从地温场及水化学场的演变出发,揭示了地质构造F1断层、Fa边山断裂带及冶峪向斜的控温作用,它们共同贡献形成的集水“凹槽”是热水田存在的主导因素,而上覆第四系黄土盖层的保温隔热性能为其提供了保证,使神堂沟地热田在众多的边山断裂热水点中脱颖而出。There must have countless ties between the formation of a geothermal field and geological structures, thus the Shentanggou geothermal field also cannot be an exception. From the transmutation of geothermal field and hydrochemical field, the author revealed the temperature control function of F1 fault, Fa Bianshan fracture zone and Yeyu syncline. They worked together to form a catchment ″trough″ and it is a main reason the geothermal field existing, and the overlying Quaternary loess plays as a thermal insulation layer, all of these factors make the Shentanggou geothermal field becomes eminent among the numerous geothermal water outcrops in Bianshan fracture zone.

关 键 词：地质构造 控温作用 神堂沟地热田 

分 类 号：P341.2[天文地球—水文科学]