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Validation of 3-D basin structure models for long-period ground motion simulation in the Osaka basin, western Japan

机译:在日本西部大阪盆地进行长周期地震动模拟的3-D盆地结构模型的验证

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摘要

We studied the applicability of two types of existing three-dimensional (3-D) basin velocity structure models of the Osaka basin, western Japan for long-period ground motion simulations. We synthesized long-period (3–20 s) ground motions in the Osaka basin during a M6.5 earthquake that occurred near the hypothetical Tonankai earthquake source area, approximately 200 km from Osaka. The simulations were performed using a 3-D finite-difference method with nonuniform staggered grids using the two basin velocity structure models. To study the ground motion characteristics inside the basin, we evaluated the wave field inside the basin using the transfer functions derived from the synthetics at the basin and a reference rock site outside the basin. The synthetic waveforms at the basin site were obtained by a convolution of the calculated transfer function and the observed waveform at the reference rock site.
机译:我们研究了日本西部大阪盆地两类现有的三维(3-D)盆地速度结构模型在长期地面运动模拟中的适用性。我们合成了在假想的Tonankai地震震源区附近发生的M6.5地震期间,大阪盆地中长周期(3– 20 s)的地震动,距大阪市约200 km。使用两个盆地速度结构模型,使用具有非均匀交错网格的3-D有限差分方法进行了模拟。为了研究盆地内部的地震动特征,我们使用从盆地合成物和盆地外部的参考岩石场得到的传递函数评估了盆地内部的波场。通过计算传递函数和参考岩石现场观测波形的卷积获得盆地现场的合成波形。

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