摘要
本文运用磁组构及显微构造方法对仙女山断裂构造变形进行分析,进而为仙女山断裂的延仲发展问题提供了理论参考依据。
Xiannushan fault is a regional active structure in the west of Hubei Province. The paper analyses the structural deformation of Xiannushan fault with microstructure and a new method,magnetic fabrics, and then affords theoretical proofs to the extension and development of Xiannushan fault.
出处
《地壳形变与地震》
CSCD
1992年第2期68-73,共6页
Crustal Deformation and Earthquake
关键词
磁组构
仙女山
断裂
三峡工程
库首
magnetic fabrics, microstrueture, Xiannushan fault, extension.
