摘要
在简述桐麻岭背斜地质环境的基础上 ,较详细地论述了背斜区 ,特别是核部岩溶发育分布特征以及岩溶发育深度 ;岩溶水的发育分布与补给、迳流。
Based on the brief geologic condition of Tongmaling anticline, the paper particularly discusses the developing and distributing character of Karst and Karst developed depth in anticline region, especially in its core. It also discusses the character of karst water’s recharge, runoff and outflow.
出处
《地质灾害与环境保护》
2001年第1期51-53,共3页
Journal of Geological Hazards and Environment Preservation
