The studies of magnetic fabric of rocks (and susceptibility anisotropy) may be successfully applied to the analysis of geologic structures.
岩石磁化组构(即磁化率各向异性)的研究，可能成功地用于地质结构分析。
Fault rocks with a random fabric include fault breccia, fault gouge, pseudotachylyte and cataclastic rocks.
具有紊乱组构的断层岩包括断层角砾岩、断层泥、假玄武玻璃以及碎裂岩。
The fabric analysis of Cpx and Opx in peridotite indicates that the Bixiling ultra_basic rocks has experienced the ductile deformation, resulting in the LPO fabric.
对橄榄岩中单斜辉石和斜方辉石的组构分析表明，碧溪岭地区超基性岩经历了塑性变形，形成了LPO组构；
应用推荐