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Finite-element simulations of long-period ground motions: Japanese subduction-zone earthquakes and the 1906 San Francisco earthquake

机译:长周期地面运动的有限元模拟:日本俯冲带地震和1906年旧金山地震

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摘要

Large earthquakes at shallow depths commonly excite long-period ground motions in distant sedimentary basins, thereby inflicting damage upon large-scale structures. For example, the 2003 Tokachi-oki earthquake, Japan, damaged oil tanks in the Yufutsu Basin, located 250 km from the epicenter. Similar long-range effects were also observed during the 2004 earthquake off Kii Peninsula, Japan. In this study, we present the results of simulations of these earthquakes undertaken using the finite element method (FEM) with a voxel mesh. In addition, to examine whether the 1906 San Francisco earthquake excited long-period ground motions in the Los Angeles-area basins, we performed long-period ground motion simulations of most of the California region. The FEM simulations confirmed the importance of path effects for the development of long-period ground motions.
机译:浅深度的大地震通常会激发远处沉积盆地的长期地震动,从而对大型结构造成破坏。例如,2003年日本十胜井地震,距震中250公里的由富津盆地的油箱损坏。在2004年日本纪伊半岛附近的地震中,也观察到了类似的远距离影响。在这项研究中,我们介绍了使用体素网格使用有限元方法(FEM)进行的这些地震的模拟结果。此外,为检查1906年旧金山地震是否激发了洛杉矶地区盆地的长周期地震动,我们对加利福尼亚大部分地区进行了长周期地震动模拟。有限元模拟结果证实了路径效应对于长周期地面运动发展的重要性。

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