首页> 外文期刊>Bulletin of the Seismological Society of America >Broadband Ground-Motion Simulation Based on the Relationship between High- and Low-Frequency Acceleration Envelopes: Application to the 2003 M-w 8.3 Tokachi-Oki Earthquake
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Broadband Ground-Motion Simulation Based on the Relationship between High- and Low-Frequency Acceleration Envelopes: Application to the 2003 M-w 8.3 Tokachi-Oki Earthquake

机译:基于高频和低频加速度包络关系的宽带地面运动仿真:在2003年十月8.3级十日大地震中的应用

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摘要

We present a new approach for broadband ground-motion simulation that is a combination of high-frequency (HF, f > 0.5 Hz) and low-frequency (LF, f < 0.5 Hz) ground-motion simulations. In this method, the LF ground motion is first computed by a deterministic approach based on a velocity model and a source model. Then, the HF acceleration envelopes are computed by multiplying the LF envelopes by envelope ratio functions (ERFs), which are defined as the empirical relationships between the characteristics of envelopes of different frequency bands. We apply the method to the 2003 Tokachi-Oki, Japan, earthquake (M-w 8.3). The LF ground motion is computed by a finite-difference method with a 3D velocity model and a finite-fault slip model. Because of the complicated rupture process of the earthquake, the fault is divided into subfaults that can be considered as smaller earthquakes. ERFs are estimated by investigating the ground-motion data of moderate-size aftershocks (5.4 <= M-w <= 6.6) for each station. The HF ground motions are simulated using the LF ground motion and the ERFs. Seismograms of all frequency bands are summed to give a time series of broadband (0.05-16 Hz) ground motion. We find that our method yields realistic broadband ground motion, in terms of the acceleration envelope, velocity waveform, and Fourier amplitude spectrum. Comparing the HF waveforms with those computed by the stochastic Green's function method (SGFM), we find that the performance of our method is better than that of the SGFM under the condition that LF waveforms are appropriately computed. The proposed method has the potential to be used as a practical method for broadband ground-motion prediction incorporating the effects of a 3D velocity model and a finite-source model.
机译:我们提出了一种宽带地面运动模拟的新方法,该方法是高频(HF,f> 0.5 Hz)和低频(LF,f <0.5 Hz)地面运动模拟的组合。在这种方法中,首先通过确定性方法基于速度模型和源模型来计算LF地面运动。然后,通过将LF包络乘以包络率函数(ERF)来计算HF加速度包络,ERF被定义为不同频带包络特性之间的经验关系。我们将该方法应用于2003年日本十胜冲chi地震(M-w 8.3)。 LF地面运动是通过有限差分方法,3D速度模型和有限故障滑动模型来计算的。由于地震破裂过程的复杂性,将断层划分为可以视为较小地震的子断层。通过研究每个站点的中等大小余震(5.4 <= M-w <= 6.6)的地震动数据来估算ERF。使用LF地面运动和ERF模拟HF地面运动。将所有频带的地震图相加,得出宽带(0.05-16 Hz)地面运动的时间序列。我们发现,根据加速度包络,速度波形和傅立叶振幅谱,我们的方法产生了现实的宽带地面运动。将HF波形与通过随机格林函数方法(SGFM)计算出的HF波形进行比较,我们发现在适当计算LF波形的情况下,该方法的性能优于SGFM的性能。所提出的方法有可能被用作结合3D速度模型和有限源模型的影响的宽带地面运动预测的实用方法。

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