山东省聊城市城区地下热水地质特征  

Geological Characteristics of Subsurface Thermal Waters in Liaocheng City in Shandong Province

作　　者：李庆朝[1] 孙淑杰[2] 郭晓丽[1] 

机构地区：[1]聊城大学环境与规划学院,山东聊城252059 [2]青岛广播电视大学,山东青岛266200

出　　处：《聊城大学学报（自然科学版）》2008年第2期85-89,共5页Journal of Liaocheng University:Natural Science Edition

基　　金：山东省软科学项目(B2006105)

摘　　要：聊城市城区具有丰富的地下热水资源,主要赋存于上第三系馆陶组和奥陶系地层中.根据聊城市地质条件及地热资源开发利用情况,对地热地质环境进行了分析.指出该区域地热资源地热成矿地质条件有利,热储层埋藏较浅,水量大、水温较高,可在采暖、洗浴、工业、医疗、养殖、农业等方面进行应用.Geothermal resources is rich in Liaocheng city, which mainly occurs in the tertiary Guantao group and Ordovician limestone. Based on conditions of Liaocheng geology and geothermal resource exploitation, geothermal geological environmental effects were analyzed. It has advantage in geothermal resource ore geology conditions, Geothermal layer deposits compare shallow, water yield is large, water temperature is compare high, It can used in many ways, such as heating, bath, industry, medical treatment, agriculture.

关 键 词：地热资源 地下热水特征 山东聊城 

分 类 号：S274[农业科学—农业水土工程]