摘要
圆梁山隧道毛坝向斜段核部及两翼的可溶岩地层中发育分布有大量的典型岩溶现象 ,本文详尽讨论了岩溶洼地、槽谷、巨型组合槽谷和地下溶洞等大型岩溶形态的基本特征、形成机制、受控因素 。
A lot of typical Karst phenomena develop in the soluble stratum at the core of the Maoba syncline and its two wings. This paper discusses the character of many big Karstic features conformation such as Karst depression,trough and gigantic combination trough and underground Karst cave as well as their forming mechanism and factors controlling them. It is concluded that lithologic character and structure control their developing and distribution.
出处
《地质灾害与环境保护》
2001年第1期43-47,共5页
Journal of Geological Hazards and Environment Preservation
