CENOZOIC EXTENSIONAL TECTONIC SYSTEM CONTROL OF THE UNDERGROUND WATER IN ORDOVICIAN LIMESTONE IN EAST WEIBEI, SHAANXI PROVINCE
-
摘要: 本文以新活动论构造观和系统论为指导,建立了渭北东部区新生代伸展构造系统模式,并以岩体结构控制论为基础,系统地讨论了本区构造网络系统对奥陶系灰岩的空间分布、奥陶系灰岩地下水水文地质单元的边界条件、奥灰水单元的补、径、排特征及其富集等方面的控制作用以及宏观指导意义。最后,系统地提出了导水构造网络系统控水的实质。Abstract: From the tectonic view point of a new mobilist and systematist, the model of Cenozoic extensional tectonic system distributed in east Weibei(eastern part of the northern Weihe River area, Shaanxi) is established in this paper. And the structural network control of the distribution of ordovician limestone, the hydrogeologic unit boundary and the movement of the underground water in the Ordovician limestone is discussed at some length with the texture and structure of the rockmass as a basis.
点击查看大图
计量
- 文章访问数: 113
- HTML全文浏览量: 32
- PDF下载量: 10
- 被引次数: 0