摘要
铜陵地区现代岩溶发育深度一般在200m以内，但在特殊地质块段存在着埋藏深度更大的岩溶，它的存在对地下水资源的开采和深埋矿床的开采具有重要意义。该类岩溶按成因可分为岩浆侵入到、断裂构造型和古岩溶。本文就其形成机制和分布特征进行了探讨。
In Tongling area. the modern karst is formed at the depth of 200m, but still deeper karsts are hidden in special sections of the area, which are worth of notice for the mining of groundwater resources and deep-lying deposits. These karsts could be divided into magma intrusive, fault structural and palaeokarst according to their genesis. This paper discusses the formation mechanism and distribution characteristics of these karsts.
出处
《水文地质工程地质》
CAS
CSCD
1997年第1期43-45,共3页
Hydrogeology & Engineering Geology
