中国岩溶2011，Vol.30Issue(2)：145-155,11.
桂南红层岩溶及其发育控制因素探讨
Karst features and the controlling factors of redbeds in South Guangxi
刘功余1
作者信息
- 1. 中铁四院集团南宁勘察设计院有限公司,广西南宁530003
- 折叠
摘要
Abstract
The redbed karst morphs in southern Guangxi mainly include gentle hills, underground caverns, karst springs and subterranean rivers as well as karst windows. In 50m depth range under the ground, the caves are mostly non-filled cave of 0. 5 to 3 m high and the number of caves decrease with depth. The types of karst springs include rising spring and descending spring with big variation in spring flow. There is no subterranean river being found in the aquifers formed only with the redbed yet. The development and the morph features of the redbed karst in south Guangxi are related to lithology and geo-structure as well hydro-geologic conditions. The redbed karst in the area mainly develops in the calcareous conglomerate that formed on the margin of the redbed basin. The group structure of redbeds can be divided into single-bed and inter-bed type. The karst develops stronger in the single-bed type but the karst develops along bedding plane in inter-bed type. Usually ,the redbed caves is more developed near the contact zone of soluble rock and non-soluble rock layers; the redbed karst is much stronger and the cave is bigger near the fracture zone of fault or valley.关键词
红层/红层岩溶/控制因素/桂南地区Key words
redbed/ redbed karst/ controlling factors/ South Guangxi分类
天文与地球科学引用本文复制引用
刘功余..桂南红层岩溶及其发育控制因素探讨[J].中国岩溶,2011,30(2):145-155,11.
