摘要
本文运用基础地质资料、差异应力及磁组构,对仙女山断裂的北延问题作一分析。最后得出:仙女山断裂消失于荒口北一带而没有穿过长江。
This paper analyzed the northward extension probtern of Xiannushan fault on the basis of basic geologic data, differential stress and magnetic fabrics. It is concluded that Xiannushan fault deoes out near the north of Huangkou and does not extes nd across the Yangtze river.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1991年第5期13-17,共5页
Hydrogeology & Engineering Geology
