The seismic reflection method can provide more detailed and more information about underground geological structure than refraction method.
对于地下复杂的地质构造，地震反射波法比折射波法能够提供更多更详细的地下信息。
Therefore, this method is suitable for the data processing of refraction and wide angle reflection profiles.
因此，适宜于折射及宽角度反射地震测深剖面的资料处理。
The reflection and the refraction of the pulse electromagnetic waves at a dielectric interface were calculated and analyzed based on the FDTD method and PML technique.
利用FDTD法和PML技术计算分析了平面分界面对脉冲波的反射和折射，充分而形象地描绘平面界面对脉冲波反射的时域过程。
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