我们展示了基于合成数据接收函数估测BPD成功应用于近地表厚度为5，7，10和15公里的薄层内的地壳模型。
We demonstrate successful application of BPD based RF estimation from synthetic data for a crustal model with a near‐surface thin layer of thickness 5, 7, 10, and 15 km.
这种深部构造信息也有可能通过地壳的动力变形和深部地球化学反应传递到地表。
The deep structural informations are also probably transmitted through mechanical deformations and deep geochemical reactions to the earth's surface.
地震震源处，其温度和压力与地壳浅处及地表不同，温、压越高，共轭破裂角越大。
The temperature and pressure at the focus is different from the shallow of the crust and the ground. The higher temperature and pressures, the larger conjugate rupture angle.
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