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anisotropy 各向异性岩石的一种特性,当沿着不同轴向进行测量时,显示不同的响应或测量值。微观各向异性指的是垂直于层面所测的特性不同于平行层面所测的特性。这是因为片状的矿物颗粒和孔隙趋于使其取向平行于层面。宏观各向异性指的是薄层和裂缝面造成的变化,二者的特性明显地不同于所测量的其余部分的特性。
An anisotropy A characteristic of anisotropic rock that shows different responses or measurements when measured along different axes. Micro-anisotropy refers to the fact that the measured characteristic perpendicular to the plane differs from the measured plane parallelism. This is because flaky mineral particles and pores tend to be oriented parallel to the layer. Macroscopic anisotropy refers to the changes caused by thin layers and fracture surfaces, the properties of which differ significantly from those of the rest of the measured properties.