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Site response estimation using strong motion network: A step towards microzonation of the Sikkim Himalayas

机译:使用强运动网络进行站点响应估计:迈向锡金喜马拉雅山的微区化

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Site response in the Sikkim Himalayas is studied using digital accelerograms recorded by a seven-station-strong-motion network, established to monitor the earthquakes in the region in an effort to microzone the area. Depending on the criterion that signal-to-noise ratio must be greater than or equal to 3, out of more than fifty earthquakes recorded during it-lay-August 1999, only fifteen events are chosen for the non-reference-receiver-function-type estimate of the site amplification factors, Site response curves (with +/- 2 standard deviation uncertainty) at all the seven sites and the contour maps at central frequencies 1, 3, 5,7, 9 and 11 Hz show station to station variation of the site factors at different frequencies, reflecting the changes in geologic/geotectonic/soil conditions. The nonlinearity of the site factor is also observed due to its strong frequency dependence. Results of this investigation reveal the significance of site response studies in the microzonation for seismic hazard assessment. [References: 25]
机译:锡金喜马拉雅山脉的现场响应是通过使用由七个站点组成的强运动网络记录的数字加速度图来研究的,该网络建立来监视该地区的地震,以便对该区域进行微区划。根据信噪比必须大于或等于3的标准,在1999年8月其记录的50多次地震中,非参考接收器功能仅选择了15个事件,站点放大因子的类型估计,所有七个站点的站点响应曲线(具有+/- 2标准偏差不确定性)和中心频率1、3、5、7、9和11 Hz的等高线图显示了站点间的变化不同频率下的站点因子,反映了地质/大地构造/土壤条件的变化。由于其强烈的频率依赖性,还可以观察到站点因子的非线性。这项调查的结果揭示了场地响应研究在微区划中对地震危险性评估的重要性。 [参考:25]

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