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

太行山南端岩溶洞穴及其形成环境
引用本文:翁金桃,陈旸,刘新号,郑富盈.太行山南端岩溶洞穴及其形成环境[J].中国岩溶,1991,10(1):63-71.
作者姓名:翁金桃  陈旸  刘新号  郑富盈
作者单位:地矿部岩溶地质研究所,地矿部岩溶地质研究所,河南地矿局水文地质一队,河南地矿局水文地质一队
摘    要:本文对分布于太行山南麓的岩溶洞穴形态进行了阐述和成因研究,首次报导了这些洞穴中发育良好的天锅等溶蚀形态的新资料。不但丰富了对中国区域岩溶的认识,而且也为分析我国北方的古气候和古水文地质环境提供了宝贵资料。

关 键 词:岩溶  溶洞  形成环境  太行山

KARST CAVES AND THEIR THEIR FORMING ENVIRONMENT AT THE SOUTHERN TIP OF TAIHANG MOUNTAIN IN NORTH CHINA
Weng Jintao,Chen Yang,Liu Xinhao and Zheng Fuying.KARST CAVES AND THEIR THEIR FORMING ENVIRONMENT AT THE SOUTHERN TIP OF TAIHANG MOUNTAIN IN NORTH CHINA[J].Carsologica Sinica,1991,10(1):63-71.
Authors:Weng Jintao  Chen Yang  Liu Xinhao and Zheng Fuying
Institution:Institute of Karst Geology,Ministry of Geology and Mineral Resources,Institute of Karst Geology,Ministry of Geology and Mineral Resources,The No.1 Hydrogeology Party, Bureau of Geology and Mineral Resources, Henan province and The No.1 Hydrogeology Party, Bureau of Geology and Mineral Resources, Henan province
Abstract:
Keywords:
本文献已被 维普 等数据库收录!
点击此处可从《中国岩溶》浏览原始摘要信息
点击此处可从《中国岩溶》下载免费的PDF全文
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