首页 | 本学科首页   官方微博 | 高级检索  
     检索      

黔西南晴隆—贞丰地区岩溶发育规律研究
引用本文:唐琼,徐世光,冯小波,李俊.黔西南晴隆—贞丰地区岩溶发育规律研究[J].河南科学,2014(2):240-244.
作者姓名:唐琼  徐世光  冯小波  李俊
作者单位:[1]昆明理工大学,昆明650093 [2]云南地矿工程勘察集团公司,昆明650011
摘    要:黔西南晴隆—贞丰地区岩溶发育强烈,该地区岩溶以形成时期分为近代岩溶与古岩溶,近代岩溶出露地表而古岩溶大部分深埋地下.通过对该地区地表岩溶与钻孔揭露古岩溶发育特征统计,进而结合该地区地质构造进行深入研究.研究结果认为岩溶发育特征主要是地质构造作用控制:近代岩溶受构造作用影响发育强烈;古岩溶受构造作用影响深埋地下,岩溶发育作用停止.

关 键 词:黔西南  地质构造  岩溶发育规律  近代岩溶  古代岩溶

The Development Law of the Karst from Qinglong to Zhenfeng in Southwest Guizhou
Tang Qiong,Xu Shiguang,Feng Xiaobo,Li Jun.The Development Law of the Karst from Qinglong to Zhenfeng in Southwest Guizhou[J].Henan Science,2014(2):240-244.
Authors:Tang Qiong  Xu Shiguang  Feng Xiaobo  Li Jun
Institution:1. Kunming University of Science and Technology, Kunming 650093, China; 2. Yunnan Geological Mining Engineering Investigation Group Co. Ltd., Kunming 650011, China)
Abstract:The karst from Qinglong to Zhenfeng region,in the southwest of Guizhou,are well developed. According to formation period,it can be divided into modern karst and ancient karst. Modern karst outcropped on the surface and most of the ancient karst buried deep underground. Through statistical analysis of the karst development characteristics of the surface karst and ancient karst revealed by drilling,we can carried out a deep study combined with the geological structure of this area. It is concluded that the main controlling factor of the karst development is geological structure. Modern karst are highly developed by the tectonic events and ancient karst buried deep are suspended.
Keywords:southwest of Guizhou  geological structure  development law of karst  modern karst  ancient karst
本文献已被 CNKI 维普 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号