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On the use of ground-motion simulations within ShakeMap methodology: application to the 2008 Iwate-Miyagi Nairiku (Japan) and 1980 Irpinia (Italy) earthquakes

机译:关于在shakemap方法中使用地面运动模拟:应用于2008 Iwate-miyagi Nairiku(日本)和1980年Irpinia(意大利)地震

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摘要

ShakeMap package uses empirical Ground Motion Prediction Equations (GMPEs) to estimate the ground motion where recorded data are not available. Recorded and estimated values are then interpolated in order to produce a shaking map associated with the seismic event of interest. The ShakeMap approach better works in regions with dense stations coverage, where the observed ground motions adequately constrain the interpolation. In poorly instrumented regions, the ground motion estimate mainly relies on the GMPE, that account only for average characteristics of source and wave propagation processes.In this study we investigated the improvement of ShakeMap in the near fault area when including synthetic estimates. We focus on the 2008, Mw 7.0, Iwate-Miyagi Nairiku (Japan) earthquake as a case study because recorded by a huge number of stations. As first we calculated the shakemaps to be used as reference maps and then removed several subsets of stations from the original data-set, replacing them with: (i) the estimations of the ground motion obtained by using a specific GMPE valid for that area, using simple source information such as the earthquake magnitude and fault geometry; (ii) the peak values from synthetic time-histories computed with a hybrid deterministic-stochastic method for extended fault, using the rupture fault model obtained from the kinematic source inversion of strong-motion records.We evaluate the deviations from the reference map and the sensitivity to the number of sites where recordings are not available. Our results show that shakemaps are more and more reliable as the coverage of stations is dense and uniformly distributed in the near-source area. Moreover, the synthetics account for propagation and source properties in a more correct way than GMPE, and largely improve the results. The hybrid maps reach good fitting levels especially when synthetics are used to integrate real data and for particular strong-motion parameters and stations’ distribution.
机译:ShakeMap软件包使用经验性地面运动预测方程(GMPE)来估算没有可用记录数据的地面运动。然后对记录的和估计的值进行插值,以生成与感兴趣的地震事件相关的振动图。 ShakeMap方法可以更好地在覆盖站点密集的区域工作,在该区域观测到的地面运动会充分限制插值。在仪器设备较差的地区,地震动估算主要依赖于GMPE,而GMPE仅考虑了震源和波传播过程的平均特征。在本研究中,我们在包括综合估算的情况下研究了ShakeMap在近断层地区的改进。我们以2008年Mw 7.0级地震(日本岩手-宫城县Nairiku)为重点,因为有大量台站记录了该地震。首先,我们计算了要用作参考图的震动图,然后从原始数据集中删除了多个站点子集,将其替换为:(i)通过使用对该区域有效的特定GMPE获得的地面运动估算,使用简单的源信息,例如地震震级和断层几何形状; (ii)使用从强运动记录的运动学源反演获得的破裂断层模型,使用混合确定性-随机混合方法计算扩展时间断层的合成时间历史的峰值,我们评估与参考图和对没有录音的站点数量的敏感性。我们的结果表明,随着台站覆盖范围密集且在近源区域均匀分布,抖动图越来越可靠。此外,与GMPE相比,合成物以更正确的方式解释了传播和源特性,并大大改善了结果。混合地图达到了良好的拟合水平,尤其是当使用合成来集成真实数据以及特定的强运动参数和测站的分布时。

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