首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Envelope synthesis of short‐period seismograms in 3‐D random media for a point shear dislocation source based on the forward scattering approximation: Application to small strike‐slip earthquakes in southwestern Japan
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Envelope synthesis of short‐period seismograms in 3‐D random media for a point shear dislocation source based on the forward scattering approximation: Application to small strike‐slip earthquakes in southwestern Japan

机译:基于正向散射近似的点剪切位错源在3D随机介质中短周期地震图的包络合成:在日本西南部小型走滑地震中的应用

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摘要

Even though high‐frequency seismograms of local earthquakes are complex because of the excitation of scattered waves caused by random lithospheric heterogeneities, their envelopes are well reproduced by the forward scattering approximation on the basis of stochastic characterization of random media. We present a method to synthesize three‐component vector wave envelopes for a point shear dislocation source by way of the stochastic raypath method using the Markov approximation for the parabolic wave equation. Because of multiple forward scattering, the directionality of the synthesized envelope shows a smoothed quadrant pattern compared to the original radiation pattern; the scattered or diffracted energy appears even in the direction of the null axis and on the nodal planes. The quadrant pattern becomes smooth as hypocentral distance increases. To examine the availability of the synthesized envelope, we analyze seismograms of two small strike‐slip earthquakes that occurred in southwestern Japan. First, we estimate the statistical parameters characterizing the randomness and the intrinsic absorptions in frequencies 2–4, 4–8, and 8–16 Hz assuming a von Karman‐type random medium, and then we examine the directionality of the envelope. The maximum energy density of the envelope shows a quadrant pattern for both P and S waves with a 45 degree shift. The directionality appears in the frequencies up to 16 Hz and at distances up to 200 km. The directionality also appears on the S wave envelope duration. The observed directionality is well explained by the synthesized envelope, but it is still difficult to explain the partition of energy into three components by the synthesized envelopes.
机译:尽管由于随机岩石圈非均质性引起的散射波的激发,局部地震的高频地震图很复杂,但在随机介质随机表征的基础上,通过正向散射近似可以很好地再现其包络。我们提出了一种利用抛物线波动方程的马尔可夫近似的随机射线路径法合成点剪切位错源的三分量矢量波包络的方法。由于存在多个前向散射,因此与原始辐射图相比,合成包络的方向性显示出平滑的象限图。甚至在零轴方向和节点平面上也会出现散射或衍射能量。象限模式随着中心距的增加而变得平滑。为了检查合成包层的可用性,我们分析了日本西南部发生的两次小型走滑地震的地震图。首先,假设冯·卡曼型随机介质,我们估计表征2–4、4–8和8–16 Hz频率的随机性和固有吸收的统计参数,然后检查包络的方向性。包络线的最大能量密度对于P波和S波均显示45度偏移的象限模式。方向性出现在高达16 Hz的频率和200 km的距离内。方向性也出现在S波包络持续时间上。合成包络很好地解释了观察到的方向性,但是仍然难以解释合成包络将能量分为三个分量的情况。

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