A model of two-layer anisotropy media is used to simulate the crust and the upper mantle respect-tively, and elastic wave fields are calculated in four coupling conditions between the two layers.

 
  • 用几种不同情况下的两层各向异性模型,模拟了全波场,著重分析了不同深度观测点上的前切波分裂特徵。
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