节点文献

鄂西清江下游古岩溶角砾岩特征及形成环境

THE CHARACTERISTICS AND THE FORMATION ENVIRONMENT OF PALEOKARST BRECCIAS IN THE LOWER REACHES OF QINGJIANG RIVER, WESTERN HUBEI

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 沈继方王增银王良忱徐瑞春徐胜友

【Author】 Shen Jifang Wang Zengyin Wang Liangchen(China University of Geosciences, Wuhan)Xu Ruichen(General Survey Team, Changjiang Water Conservancy Coramitte)Xu Shengyou(Institute of Karst Geology MGMR)

【机构】 中国地质大学长江水利委员会勘测总队地矿部岩溶地质研究所 武汉武汉武汉

【摘要】 本文将现代沉积学的概念与理论运用于清江流域古岩溶角砾岩的分类和描述;据其岩石学和矿物学特征,分析地下水沉积作用,确立形成环境与形成机制;结合其时空分布与区域地质格局的关联及样品测试,探讨了形成时代区域古水文地质条件的演变和岩溶发育期。

【Abstract】 By introducing the conception and theory of mordern sedimentology. the authors discribed and classified the paleokarst breccias distributed in the lower reaches of Qingjiang River(western Hubei Province). The sedimentation by under ground water flows was analysed on the basis of the petrologic and mineralogic characteristics of these breccias, and their forming condition and mechanism were consequently established. Joining with the studies about the correlations between their distribution in time and space and regional geologic setting, and with the analysis of samples, the evolution of the regional paleohydrogeological conditions and the karst development in their forming period are discussed.

  • 【文献出处】 中国岩溶 ,Carsologica Sinica , 编辑部邮箱 ,1993年01期
  • 【被引频次】14
  • 【下载频次】312
节点文献中: 

本文链接的文献网络图示:

本文的引文网络