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Characterization of near-source ground motions with earthquake simulations

机译:利用地震模拟表征近源地震动

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摘要

We examine the characteristics of long-period near-source ground motions by conducting a sensitivity study with variations in six earthquake source parameters for both a strike-slip fault (M 7.0-7.1) and a thrust fault (M 6.6-7.0). The directivity of the ruptures creates large displacement and velocity pulses in the forward direction. The dynamic displacements close to the fault are comparable to the average slip. The ground motions exhibit the greatest sensitivity to the fault depth with moderate sensitivity to the rupture speed, peak slip rate, and average slip. For strike-slip faults and thrust faults with surface rupture, the maximum ground displacements and velocities occur in the region where the near-source factor from the 1997 Uniform Building Code is the largest. However, for a buried thrust fault the peak ground motions can occur up-dip from this region.
机译:我们通过对走滑断层(M 7.0-7.1)和逆冲断层(M 6.6-7.0)的六个地震震源参数进行敏感性研究,研究了长周期近源地震动的特征。破裂的方向性在向前方向上产生大的位移和速度脉冲。靠近断层的动态位移可与平均滑移相媲美。地面运动对断层深度表现出最大的敏感性,对破裂速度,峰值滑移率和平均滑移具有中等敏感性。对于带有表面破裂的走滑断层和逆冲断层,最大的地面位移和速度发生在1997年《统一建筑规范》中近源因子最大的区域。但是,对于埋藏的逆冲断层,峰值地面运动可能会从该区域向上倾斜。

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