山东省定陶县城区地热资源分析及开发利用  

Development and Utilization of the Geothermal Resources in Dingtao County Area,Shandong Province

作　　者：冯超臣[1] 马龙[1] 张旭[1] 

机构地区：[1]山东省鲁南地质工程勘察院,山东兖州272100

出　　处：《城市地质》2012年第4期28-31,共4页Urban Geology

摘　　要：定陶县城区地处鲁西南黄泛平原,为第四系和新近系松散层覆盖。区域断裂构造发育,可利用的热储层为新近系明华镇组和奥陶系。奥陶系热储层具有较好的开发利用价值,本文分析了该区热储层地质条件、地温场特征和地热水质,并对其开发利用与保护提出了建议。The town area of Dingtao County is located in the southwest of the Yellow River flood plain area, which surface is covered by the very thick unconsolidated sediments of Quaternary and Neogene systems. The regional faults are well-developed for forming the geothermal conditions. The favorable geothermal reservoirs occur in the Neogene Minghuazhen Fm. and Ordovician System, of which the Ordovician reservoir has the good value to develop and utilize. For the Ordovician heat reservoir, the geothermal geological conditions, geothermal field characteristics and water quality characteristics are analyzed in this paper. Otherwise the measurements of development and protection are put forward for the future.

关 键 词：地热资源 热储层 模型 开发利用 

分 类 号：P314[天文地球—固体地球物理学]