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首页> 外文期刊>Bulletin of the Seismological Society of America >2.5D SH wave propagation in heterogeneous crustal wave guides using the phase screen method
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2.5D SH wave propagation in heterogeneous crustal wave guides using the phase screen method

机译:使用相位屏蔽方法在异质地波波导中传播2.5D SH波

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摘要

One-way approximations for regional phases slice the half-space crustal wave guide into a number of slabs perpendicular to the propagation direction; the Moho discontinuity can be easily treated as a perturbation from the crustal background. The advantage of one-way propagation methods is their great saving of computing time and memory compared to full-waveform numerical methods, especially for 3D simulations. In this article, we present general 2.5D SH formulas for the thin-slab method and a generalized screen propagator (GSP) for simulating SH wave propagation in the heterogeneous half-space crustal wave guide. Comparisons of numerical results with a finite-difference (FD) algorithm for a standard flat crustal model show excellent agreement, demonstrating the validity and accuracy of the 2.5D GSP for the half-space problem. We then compare the curves of energy attenuation calculated by the 2D and 2.5D formulas. The comparison shows that the energy attenuation of the 2.5D case is about 1.5-3 times greater than that of the 2D case when the trapped mode is formed. The SH screen propagator is also used to simulate two laterally unvarying (in the y direction) crustal models, showing the path effects on regional wave propagation.
机译:区域相位的单向近似将半空间地壳波导切成与传播方向垂直的许多平板。莫霍面的不连续性很容易被视为来自地壳背景的扰动。单向传播方法的优点是,与全波形数值方法相比,它们可以节省大量的计算时间和内存,尤其是对于3D模拟而言。在本文中,我们为薄板方法提供了通用的2.5D SH公式以及用于模拟SH波在异质半空间地壳波导中传播的通用筛网传播器(GSP)。对于标准平面地壳模型,使用有限差分(FD)算法进行的数值结果比较显示出极好的一致性,证明了2.5D GSP用于半空间问题的有效性和准确性。然后,我们比较2D和2.5D公式计算出的能量衰减曲线。比较表明,在形成陷波模式时,2.5D情况的能量衰减约为2D情况的1.5-3倍。 SH屏幕传播器还用于模拟两个横向不变的(沿y方向)地壳模型,显示路径对区域波传播的影响。

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