山东聊城市唐庄地热水热储模式研究  

Research on thermal reservoir model of geothermal water in Tangzhuang of Liaocheng in Shandong

作　　者：袁凤凯 李建华[2] 胡亚召[3] 

机构地区：[1]四川省核工业地质调查院 [2]四川省核工业地质局二八一大队 [3]四川省地质工程勘察院

出　　处：《山西建筑》2010年第26期170-172,共3页Shanxi Architecture

摘　　要：针对聊城市唐庄地区地热井地热水热储模式进行了分析,通过分析得出该区地热水很多水化学指标都达到了矿水浓度,具有重要的开采价值,并指出该区地热水主要热储层为新近系馆陶组中粗砂岩、砾状粗砂岩等地层,盖层为第四系和新近系明化镇组黏性土、砂性土、砂层等地层。The paper analyzes the geothermal and the thermal reservoir model of the geothermal water in Tangzhuang of Liaocheng, indicates the chemical indexes of the geothermal water of the region meet the mineral water＇s density, so it has the exploitation value, and introduces the main thermal reservoir lay of the thermal water are mainly medium-sized sandstone and gravel sandstone of the neogene guantao formation, and the cap rock is the quaternary and neogene Minghuazhen formation clay, sandstone and sand layer.

关 键 词：地热水 热储模式 热储层 盖层 

分 类 号：TU833[建筑科学—供热、供燃气、通风及空调工程]