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临江市老三队地热水形成条件及成因探讨
引用本文:蔡卫东,张敏,初海丰.临江市老三队地热水形成条件及成因探讨[J].吉林地质,2003,22(3):52-56.
作者姓名:蔡卫东  张敏  初海丰
作者单位:1. 吉林省地质调查院,吉林,长春,130061
2. 长春市实验中学,吉林,长春,130056
摘    要:介绍了临江市老三队地热水的自然地理概况和区域地质水文地质概况,分析了它的物理化学特征,含水岩组,补、径、排条件以及热储层、隔热盖层、地热水源等,最后探讨了其形成条件及成因。

关 键 词:地热水  热储层  地温场  地热水成因
文章编号:1001-2427(2003)03-0052-05
修稿时间:2003年6月20日

The geothermal water forming conditions of the Laosandui,Linjiang area, and its origin
CAI Wei-dong,ZHANG Min,CHU Hai-feng.The geothermal water forming conditions of the Laosandui,Linjiang area, and its origin[J].Jilin Geology,2003,22(3):52-56.
Authors:CAI Wei-dong  ZHANG Min  CHU Hai-feng
Institution:CAI Wei-dong~1,ZHANG Min~1,CHU Hai-feng~2
Abstract:The physicogeographical situation of geothermal water of the Laosandui, Linjiang area and the regional geological, hydrogeological situation are introduced. Its physicochemical characteristics, aquifer component, recharge, runoff, discharge condition, thermal reservoir strata, insulating caprock, as well as geothermal field sources are analyzed, finally, its forming conditions and origin are discussed in this paper.
Keywords:geothermal water  thermal reservoir strata  geothermal field  origin of geothermal water
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