Preferred orientation of rock fabric elements is usually recognized by projecting and plotting contours.
以往采用投影作图法确定岩石组构要素优选方位。
According to geologic structural location, features of occurrence, rock fabric and geochemical index of basalt in Ruqi clough of Helan Mountain, it can be regarded as continental rift basalt.
根据贺兰山汝箕沟玄武岩的地质构造位置、产状特征、岩石组构和地球化学指标等，将其划归为大陆裂谷玄武岩系列，它代表了典型的陆内拉张环境。
For touch, select an object with "a notable texture or temperature, like a rock, a piece of fabric, or an instant ice pack."
触觉上，选择一些具有“纹理或温度，如岩石，一块织布或一个紧急的冰敷袋子。”
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.
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 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.
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 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.
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。
An analysis of the rock magnetic fabric can be used to study the fabric characteristics of the rocks and structural deformation.
岩石磁组构分析可用来研究岩石的组构特征及构造变形。
Fabric analysis studys vectorial quality of natural rock and unit in space by statistical method and illustrates or probes the produced condition and metastatic history during tectonic movement.
岩组分析是利用统计的方法研究天然岩石及其组成单元在空间向量性质，以阐明或探讨岩石形成时的条件及其在构造运动中的变形历史。
Can rock magnetic fabric reveal strain?
岩石磁组构可以揭示应变吗？
As a product of geological history, rock and soil media process their special compositions and fabric structures so that their engineering behavior is very complicated.
岩土体是地质历史的产物，有着特定的物质组分和结构构造，从而表现出复杂的工程力学性质。
The shapes and fabric of the inclusion, as well as the strong exchange of the chemical compositions between the enclave and the host rock indicate the magma mingling.
包体的形态、结构 构造以及与寄主岩 石强烈地成分交换等均是岩浆混合作用的标志。
The shapes and fabric of the inclusion, as well as the strong exchange of the chemical compositions between the enclave and the host rock indicate the magma mingling.
包体的形态、结构 构造以及与寄主岩 石强烈地成分交换等均是岩浆混合作用的标志。
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