实验证明核磁共振孔隙度与岩石磁化率及岩石比表面有关。
Experiments demonstrate that NMR porosity is related with magnetic susceptibility and specific surface of the rock.
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。
The studies of magnetic fabric of rocks (and susceptibility anisotropy) may be successfully applied to the analysis of geologic structures.
由于磁性矿物受当时磁场作用往往呈定向排列，导致岩石磁化率各向异性，反映了岩石的磁组构特征。
The anisotropy of rock magnetic susceptibility, caused by the oriented arrangement of magnetic minerals effected by then magnetic field, reflects the feature of the rock magnetic fabric.
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