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Stochastic finite-fault method controlled by the fault rupture process and its application to the Ms 7.0 Lushan Earthquake

机译:断裂过程控制的随机有限故障方法及其在庐山7.0级地震中的应用

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Fast and precise estimation of strong ground motion is important for seismic hazard responses and engineering purposes. Stochastic finite-fault methods are effective ground-motion time-series simulation methods using stochastic models of point-source spectra and considering physical parameters on finite faults. We propose two main modifications of current stochastic finite-fault methods to control the simulations. We replace the predetermined time function with different source time functions for each subfault to improve low-frequency results including the envelopes of accelerations and velocities. We replace the uniform stress drop with a distribution of non-uniform stress drops to reduce the dependence of simulated results on a single stress drop. The two modifications are applied to simulate ground motions of the 2013 Ms 7.0 Lushan earthquake. The simulation results agree with the observations in terms of acceleration, velocity, and pseudo-spectral acceleration (PSA). Damage estimates based on the simulated PSA also agree with the post-earthquake disaster investigation.
机译:快速准确地估计强烈的地面运动对于地震灾害响应和工程目的很重要。随机有限故障方法是一种有效的地面运动时间序列仿真方法,它使用点源谱的随机模型并考虑了有限断层的物理参数。我们提出了对当前随机有限故障方法的两个主要修改,以控制仿真。对于每个子故障,我们用不同的源时间函数替换预定的时间函数,以改善低频结果,包括加速度和速度的包络。我们将非均匀应力降的分布替换为均匀应力降,以减少模拟结果对单个应力降的依赖性。这两项修改被应用于模拟2013年芦山7.0级地震的地震动。仿真结果与加速度,速度和伪谱加速度(PSA)方面的观察结果一致。基于模拟PSA的损失估算也与震后灾难调查一致。

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