山东省曹县城区地热资源地质条件综合研究  

A Study on the Geological Condition of Geothermal Resources in Caoxian of Shandong Province

作　　者：马龙[1] 冯超臣[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：《地下水》2014年第4期30-32,共3页Ground water

基　　金：山东省曹县城区地热资源普查项目(SDCX-2007)

摘　　要：曹县城区地处鲁西南黄泛平原地区,该区地表被巨厚的第四系和新近系松散层覆盖,区域断裂构造十分发育,地热成矿地质条件有利。可被利用的热储层主要有2个,分别为新近纪明华镇组热储和奥陶纪热储,二个热储层地热资源各具特点。对该区可利用热储层地热资源地质条件进行了分析研究,为下一步曹县城区地热资源的开发利用提供参考性地质依据。Caoxian City, it is located in the southwest of Yellow River floodplain and is an area with rich geothermal re-sources. Attributing to the thick Quaternary and Neogene unconsolidated formation, faults developed well in this region and provide good conditions for geothermal resources mineralization. Available geothermal resources in this region are the quaterna-ry geothermal reservoir located in Minghua town and an Ordovician geothermal reservoir. In this paper, geological conditions of the two geothermal reservoirs are analyzed to provide reference for further exploration and utilization of geothermal resourced in Caoxian.

关 键 词：曹县城区 地热资源 断裂构造 热储层 地温场 

分 类 号：P314[天文地球—固体地球物理学]