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.
出处
《城市地质》
2012年第4期28-31,共4页
Urban Geology
关键词
地热资源
热储层
模型
开发利用
Dingtao county area
Geothermal resources
Geothermal reservoir
Model
Exploitationand utilization
