| 陕西渭北东部区新生代伸展构造网络系统对奥灰水的控制作用 |
| |
| 引用本文： | 陈昌彦,王思敬,王贵荣,黄克兴. 陕西渭北东部区新生代伸展构造网络系统对奥灰水的控制作用[J]. 地质力学学报, 1996, 2(4): 21-30 |
| |
| 作者姓名： | 陈昌彦 王思敬 王贵荣 黄克兴 |
| |
| 作者单位： | 1. 中国科学院地质研究所工程地质力学开放研究实验室; |
| |
| 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。
|
| 关 键 词： | 控水构造网络系统 三维控制 奥灰水 |
CENOZOIC EXTENSIONAL TECTONIC SYSTEM CONTROL OF THE UNDERGROUND WATER IN ORDOVICIAN LIMESTONE IN EAST WEIBEI, SHAANXI PROVINCE |
| |
| Chen Changyan,Wang Sijing,Wang Guirong and Hang Kexing. CENOZOIC EXTENSIONAL TECTONIC SYSTEM CONTROL OF THE UNDERGROUND WATER IN ORDOVICIAN LIMESTONE IN EAST WEIBEI, SHAANXI PROVINCE[J]. Journal of Geomechanics, 1996, 2(4): 21-30 |
| |
| Authors: | Chen Changyan Wang Sijing Wang Guirong Hang Kexing |
| |
| Affiliation: | 1. Institute of Geology, Chinese Academy of Science;2. Department of Geology Xi'an Mining Institute |
| |
| 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. |
| |
| Keywords: | structural network extensional tectonic system the underground water in Ordovician limestone |
| 本文献已被 维普 等数据库收录！ |
| 点击此处可从《地质力学学报》浏览原始摘要信息 |
|
点击此处可从《地质力学学报》下载全文 |
