Macroscopic deviations from isotropy occur due to bedding, schistosity and also sometimes fracturing.

与各向同性相差很大的情况往往产理，片理，某些候则由断所成。

Through the bedding distribution statistical analysis, studies the palaeocurrent during sedimentation.

通过对理分布统计分析，研究了沉积古水流方向。