• 磁组构是指磁化率的各向异性。

    The magnetic fabric means the anisotropy of the susceptibility.

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  • 磁组构是一种灵敏的应变指示计。

    Magnetic fabric is a sensitive strain indicator.

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  • 岩石磁组构可以揭示应变吗?

    Can rock magnetic fabric reveal strain?

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  • 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.

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  • 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.

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  • 本文研究了典型韧性变形断裂和弱变形区的岩石磁组构特征。

    The paper studies magnetic fabric characteristic of faults developed in the typical ductility and weak deformation areas.

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  • 对龙门山褶皱冲断带北段前锋带至四川盆地边缘的川西北地区进行了磁组构研究。

    An investigation of magnetic fabrics has been carried out in northwestern Sichuan from the front zone in the northern segment of the Longmen fold-thrust belt to the margin of the Sichuan basin.

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  • 岩石磁组构反映的应力状态总体为以NE向挤压为主,与轴向NW的背斜构造发育相一致。

    The stress state reflected by the rock magnetic fabric is mainly manifested by NE compression, which is consistent with the arrangement of the anticlines with axes running NW.

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  • 实例研究证实,磁组构学方法对于岩浆动力学,特别是岩体构造应力的属性分析非常有效。

    This attempt demonstrates that the method of magnetic fabric is effective in the field of magma dynamics, especially for reconstruction of the stress a granite body experienced.

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  • 矿区的磁线理、磁面理等磁组构研究表明,磁组构能与岩组研究一样,解决岩石变形的应力场问题。

    The magnetic lineation and magnetic foliation study of the ore area show that the magnetic fabric study can proclaim the stress field of rock deformation as the petrofabric analysis.

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  • 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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  • 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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