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首页> 外文期刊>Geophysical Research Letters >Rupture dynamics and ground motions from earthquakes in 2-D heterogeneous media
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Rupture dynamics and ground motions from earthquakes in 2-D heterogeneous media

机译:二维异质介质中地震的破裂动力学和地震动

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摘要

We perform 2-D simulations of earthquakes on rough faults in media with random heterogeneities (with von Karman distribution) to study the effects of geometric and material heterogeneity on the rupture process and resulting high-frequency ground motions in the near-fault region (out to approximate to 20km). Variations in slip and rupture velocity can arise from material heterogeneity alone but are dominantly controlled by fault roughness. Scattering effects become appreciable beyond approximate to 3km from the fault. Near-fault scattering extends the duration of incoherent, high-frequency ground motions and, at least in our 2-D simulations, elevates root-mean-square accelerations (i.e., Arias intensity) with negligible reduction in peak velocities. We also demonstrate that near-fault scattering typically occurs in the power law tail of the power spectral density function, quantified by the Hurst exponent and another parameter combining standard deviation and correlation length.
机译:我们对具有随机异质性的介质(具有von Karman分布)的粗糙断层进行地震的二维模拟,以研究几何和材料异质性对破裂过程的影响以及近断层区域中高频地震动的影响。约20公里)。滑移和破裂速度的变化可能仅由材料异质性引起,但主要受断层粗糙度控制。在距断层约3 km处,散射效应变得明显。近断层散射延长了不连贯的高频地面运动的持续时间,并且至少在我们的二维模拟中,它提高了均方根加速度(即Arias强度),而峰值速度的减小可忽略不计。我们还证明了近故障散射通常发生在功率谱密度函数的幂律尾部,由赫斯特指数和结合标准偏差和相关长度的另一个参数来量化。

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