重庆涪陵焦石片区岩溶发育规律及影响因素分析

详细信息

刊出日期: 2012-04-25

Analysis on karst development law and its influencing factors in Jiaoshi area of Chongqing city

Publish Date: 25 April 2012

摘要: 本区岩溶组合形态分为垄岗谷地中山、垄脊槽谷低—中山、岩溶峡谷中山、溶丘谷地低山四种类型。岩溶洞穴主要分布在卷洞河流域、包鸾河流域、乌江干流、长江干流。岩溶发育分布特征受到多个因素的影响,碳酸盐岩岩性组合是其物质基础:区域构造及新构造运动是其影响因素。
- 岩溶 /
- 发育规律 /
- 影响因素
Abstract: There are four karst combination morphology like ridge-hilllock-valley-middle mountain,ridge-spinal-valley- low-middle mountain,karst-conyon-middle mountain,solution platform-valley-low mountain in this area. Karst caverns are distributed mainly in the Reach of Juandong River and Baoluan River,main stream of Wujiang River and Yangtze River. Karst development and distribution are influenced by many factors:carbonate lithology combination is the base, and regional structure and neoteetonics are influencing factors.
- karst /
- developmentlaw /
- influencing factors