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Spectral attenuation models in the Sikkim Himalaya from the observed and simulated strong motion events in the region

机译:锡金喜马拉雅山的光谱衰减模型,来自该地区观测和模拟的强运动事件

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摘要

Strong motion recordings by the Sikkim Strong Motion Array (SSMA) of 80 events with good signal-to-background noise ratio (>= 3) for magnitude between 3 to 5.6, have enabled estimation of source model and site response, and also the simulation of spectral acceleration for moderate-to-large earthquakes with 6 <= M_w <= 8.3. A combined simulated and recorded data set have ultimately been utilized for deriving the spectral attenuation laws incorporating the local site conditions, namely, topographic effect and site response, with and without shear wave velocity in addition to the normal earthquake parameters, viz. moment magnitude (M_w) and source-to-site distance (r). The spectral attenuation laws developed in this study have been found to be appropriate for predicting free-field horizontal Peak Ground Acceleration (PGA) for earthquakes of 3 <= M_w <= 8.3 and for the sites with distances up to 100 km from the source in the Sikkim Himalaya. The estimated spectral acceleration through these attenuation laws mimic the mean spectral acceleration simulated using Brune's source model.
机译:锡金强运动阵列(SSMA)进行的强运动记录具有80个事件,信噪比(> = 3)良好,幅度在3到5.6之间,可以估算源模型和站点响应,还可以进行仿真6 <= M_w <= 8.3的中到大地震的频谱加速度分布图。最终将组合的模拟和记录数据集用于推导包含局部场地条件(即地形效应和场地响应)的频谱衰减定律,除了正常地震参数外,还有和没有剪切波速度。矩量级(M_w)和源到站点距离(r)。已经发现,在这项研究中开发的频谱衰减定律适用于预测3 <= M_w <= 8.3地震以及距震源最远100 km的站点的自由场水平峰值地面加速度(PGA)。锡金喜马拉雅山。通过这些衰减定律估计的光谱加速度模仿了使用Brune源模型模拟的平均光谱加速度。

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