太原地区间互状灰岩块断型水文地质结构研究  

STUDR ON BLOCK-TYPE HYDROGEOLOGICAL STRUCTURE OF INTERSTRATIFIED LIMESTONE

作　　者：何宇彬[1] 徐超[1] 

机构地区：[1]同济大学

出　　处：《中国岩溶》1993年第1期55-66,共12页Carsologica Sinica

摘　　要：大原是我国能源基地,水资源紧张。该基地地质结构复杂,喀斯特水埋藏很深,迳流与排泄条件非常复杂,某些水文地质问题,例如水文地质结构模型;喀斯特水的深部迳流问题;关于西、东边山的潜流侧排问题;兰村与枣沟水源地之间的水力联系问题;奥灰水水资源的潜力问题,一直是学术界争论的焦点。 笔者认为,上述诸多问题的核心是对水文地质结构模型的认识,它是一项具有应用性的基础理论研究。随着对这一问题认识的深入,其它问题也就迎刃而解了。Taiyuan city is a coal energy base of China, one of the cities which is deficient in water resources. The geological structure of Taiyuan area is complicated.Karst water is buried much deeply, which makes the condition of runoff and drainage very complex. Some hydrogeological problems have been the points in dispute. They are: 1.Hydrogeological structural model. 2.The problem of deep runoff of karst water. 3.The lateral drainage of western and eastern marginal belts. 4.The hydraulic connection between Liancun and Zaogou water source bases. 5.The potentiality of karst water resources. The authors think that the main point of above issues is still the cognition about the hydrogeological structural model which is a fundamental theoretical study with applicabity. Along with the further cognition to this problem, the other issues can be readily solved.

关 键 词：水文地质 结构 洞隙水 灰岩块 

分 类 号：P641.136[天文地球—地质矿产勘探]