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岩石标本磁各向异性的统计检验准则适用X~2检验。矿区岩石的磁组构与岩石组构及有限应变形态组构具有相同的极密优选组构特征。磁面理平行于矿区第一期劈理,也平行于应变椭球最大拉长轴面;磁线理与拉长线理近于平行。磁化率椭球与应变椭球具有共轴性,二者的两半轴比存在函数关系。
The rock magnetic anisotropy statistical test criteria apply X ~ 2 test. The magnetic fabric of the rock in the mining area has the same extremely dense structural features as the rock and finite strain morphologies. Magnetic field parallel to the first phase of the mine cleavage, but also parallel to the maximum elongation of the elastic axis of the plane; magnetism and the extension of nearly parallelism. The magnetic susceptibility ellipsoid and the strain ellipsoid are coaxial, and the two half-axes have a functional relationship.