岩石内部磁性矿物分布排列方式的特点。
磁组构是指磁化率的各向异性。
The magnetic fabric means the anisotropy of the susceptibility.
本文讨论了喀喇昆仑断裂带的磁组构特征。
This paper deals with the characteristics of magnetic fabrics of the Karakoram fault belt.
岩石磁组构分析可用来研究岩石的组构特征及构造变形。
An analysis of the rock magnetic fabric can be used to study the fabric characteristics of the rocks and structural deformation.
应用推荐