摘要
绥阳双河洞是发育在早古生代白云岩体内的多层多支，并彼此有水力联系的复杂洞群，根据贵州洞穴协会实测，洞长达３５．２ｋｍ。文章在实地考察的基础上，分析主要洞道的分布与特征，研究了洞穴发育与硫酸盐岩及含ＳＯ地下水的密切关系，并探讨了石膏源及洞穴发育演化的过程。
Shuanghe cave system is located in Suiyang County,N.GuiXhou.It is a complicated cave sys-tem developed in the dolomitic rocks of Early Paleozoic and consisting of many levels and branch-es hydrologically connected with each other.The total length of the cave passages surveyedamounts to 35 km,that might be said to be the longest in Guizhou.Based on the cave explorationand mapping as vvell as field work in the cave district the distribution and characteristics of themain cave passages are discussed.The interrelation between sulfate minerals,SObearinggroundwater and the mechanism of the cave formation is also emphasized.
出处
《中国岩溶》
CAS
CSCD
北大核心
1994年第3期247-255,共9页
Carsologica Sinica
关键词
洞穴发育
石膏
白云岩
双河洞系
ave development,gypsum,dolomite,Suiyang County of Guizhou.
