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首页> 外文期刊>Seismological research letters >Broadband (0-5 Hz) Fully Deterministic 3D Ground-Motion Simulations of a Magnitude 7.0 Hayward Fault Earthquake: Comparison with Empirical Ground-Motion Models and 3D Path and Site Effects from Source Normalized Intensities
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Broadband (0-5 Hz) Fully Deterministic 3D Ground-Motion Simulations of a Magnitude 7.0 Hayward Fault Earthquake: Comparison with Empirical Ground-Motion Models and 3D Path and Site Effects from Source Normalized Intensities

机译:宽带(0-5 Hz)完全确定的3D地面运动模拟7.0 Hayward故障地震:与经验地面运动模型和3D路径和站点效应的比较来自源标准化强度

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摘要

We report on high-performance computing (HPC) fully deterministic simulation of ground motions for a moment magnitude (Mw) 7.0 scenario earthquake on the Hayward fault resolved to 5 Hz using the SW4 finite-difference code. We computed motions obeying physics-based 3D wave propagation at a regional scale with an Mw 7.0 kinematic rupture model generated following Graves and Pitarka (2016). Both plane-layered (1D) and 3D Earth models were considered, with 3D subsurface material properties and topography interpolated from a model of the U. S. Geological Survey (USGS). The resulting ground-motion intensities cover a broader frequency range than typically considered in regional-scale simulations, including higher frequencies relevant for engineering analysis of structures. Median intensities for sites across the domain are within the reported between-event uncertainties (t) of groundmotion models (GMMs) across spectral periods 0.2-10 s (frequencies 0.1-5 Hz). The within-event standard deviation. of ground-motion intensity measurement residuals range 0.2-0.5 natural log units with values consistently larger for the 3D model. Source-normalized ratios of intensities (3D/1D) reveal patterns of path and site effects that are correlated with known geologic structure. These results demonstrate that earthquake simulations with fully deterministic wave propagation in 3D Earth models on HPC platforms produce broadband ground motions with median and within-event aleatory variability consistent with empirical models. Systematic intensity variations for the 3D model caused by path and site effects suggest that these epistemic effects can be estimated and removed to reduce variation in site-specific hazard estimates. This study motivates future work to evaluate the validity of the USGS 3D model and investigate the development of path and site corrections by running more scenarios.
机译:我们报告了高性能计算(HPC)的地面动作的完全确定性模拟了片刻幅度(MW)7.0场景地震,使用SW4有限差分码解决了5 Hz。我们计算了遵守基于物理的3D波传播的动作,以坟墓和Pitarka(2016)产生的MW 7.0运动破裂模型。考虑了平面层(1D)和3D地球模型,3D地下材料特性和地形从美国地质调查(USGS)的模型内插。由此产生的地运动强度覆盖比在区域规模模拟中通常考虑的更广泛的频率范围,包括对结构的工程分析相关的频率。跨越域中的站点的中位强度在谱间隔0.2-10s(频率0.1-5Hz)之间报道的地图模型(GMMS)之间的报告 - 事件不确定性(T)之间。内部事件标准偏差。地面运动强度测量残差范围为0.2-0.5自然日志单位,对于3D模型始终较大。源标准化的强度比(3D / 1D)揭示了与已知地质结构相关的路径和现场效果的模式。这些结果表明,HPC平台上的3D地球模型中具有完全确定性波传播的地震模拟产生了与实证模型一致的中位数和内在的综利变异性的宽带接地运动。由路径和现场效果引起的3D模型的系统强度变化表明这些认知效果可以估计和去除,以减少特定于特特异性危险估计的变化。本研究激励未来的工作来评估USGS 3D模型的有效性,并通过运行更多场景来调查路径和站点更正的开发。

著录项

  • 来源
    《Seismological research letters》 |2019年第3期|共17页
  • 作者单位

    Lawrence Livermore Natl Lab Atmospher Earth &

    Energy Div &

    Geophys Monitoring 7000 East Ave L-046 Livermore CA 94551 USA;

    Lawrence Livermore Natl Lab Ctr Appl Sci Comp 7000 East Ave L-561 Livermore CA 94551 USA;

    Lawrence Livermore Natl Lab Atmospher Earth &

    Energy Div &

    Geophys Monitoring 7000 East Ave L-046 Livermore CA 94551 USA;

    Univ Nevada 1644 North Virginia St Reno MS 0258 Reno NV 89577 USA;

    Lawrence Livermore Natl Lab Ctr Appl Sci Comp 7000 East Ave L-561 Livermore CA 94551 USA;

    Univ Calif Berkeley Dept Civil &

    Enviornm Engn 455 Davis Hall Berkeley CA 94720 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地震学;
  • 关键词

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