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浅析吉林市圣德泉地热资源成因
引用本文:陈永城,张璐,杨益国.浅析吉林市圣德泉地热资源成因[J].吉林地质,2012(3):108-110.
作者姓名:陈永城  张璐  杨益国
作者单位:吉林省地质环境检测总站;吉林省地矿信息中心
摘    要:吉林圣德泉生态园观光旅游区地处伊—舒地堑盆地中部,开发利用第三系砂岩-砂砾岩中的地下热水资源。该地区地热成因属于断裂构造和盆地增温复合型。目前大部分开采的地热田埋藏深度为950~2 000 m,储热层厚度200~300 m,日开采量200~300 m3,水温59~62℃,属于低温地下热水。

关 键 词:地热田  储热层  低温地下热水  伊—舒地堑盆地

Genesis of Shengdequan geothermic resources in Jilin City
CHEN Yong-cheng,ZHANG Lu,YANG Yi-guo.Genesis of Shengdequan geothermic resources in Jilin City[J].Jilin Geology,2012(3):108-110.
Authors:CHEN Yong-cheng  ZHANG Lu  YANG Yi-guo
Institution:1.Geological Environment Testing Station of Jilin Province,Changchun 130061,Jilin,China;2.Information Center of Geology Mineral Resources of Jilin Province,Changchun 130061,Jilin,China
Abstract:Jilin Shengdequan ecological park tourism zone is located in the middle part of Yitong-Shulan graben basin,developed and utilized underground hot-water resources of the Tertiary system sandstone gravel rock.The geothermic genesis in the region belongs to compound type of the fracture structure and basin warming.Most of the burial depth of current productive geothermal field is 950~2 000 m,the heat-storage reservoir depth 200 ~ 300 m,daily yield 200 ~ 300 m3,water temperature 59~62℃,which belongs to low temperature geothermal hot water.
Keywords:geothermal field  the heat-storage reservoir  low temperature geothermal hot water  Yitong-Shulan graben basin
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