摘要
讨论岩石磁各向异性的基本理论和作为一种有效手段在构造地质学分析中的应用,指出分析过程中存在的问题和可能的解决方法。
The paper has interpreted the basic theory of magnetic unisotropy in rock,the present situation of its application as a effective means in the structural geology analysis and the method for solving the problems existing in the analysis.
出处
《云南地质》
2013年第1期106-109,共4页
Yunnan Geology
关键词
磁化率各向异性
磁组构
构造变形分析
岩石形变
Unisotropy of Magnetic Susceptibility
Magnetic Fabric
Analysis of Structural Deformation
Rock Deformation
