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Probabilistic seismic hazard mapping of National Capital Region of India using a modified gridded seismicity model

机译:使用修改的网格震荡模型,印度国家首都地区的概率地震危害映射

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This is the first comprehensive study for a seismic macro-zonation of the National Capital Region of India by using the probabilistic seismic hazard analysis approach. A modified gridded seismicity model is used for this purpose, in which the earthquake occurrence rates obtained using the Gutenberg-Richter's (G-R) relationships for conventional area type seismic sources are distributed non-uniformly among a grid of cells. This provides a more robust approach than the commonly used weighted sum of area sources of homogeneous seismicity and the zone-free smoothed gridded seismicity. Other distinguishing features of the present analysis include: detailed seismotectonic evaluation of the region to identify seven area type seismic sources, compilation of a comprehensive earthquake catalogue for the estimation of seismicity recurrence parameters, selection of the most appropriate ground motion prediction equation by using a database of 71 strong motion accelerograms recorded in the region, and estimation of the compatible distance parameters by associating a fictitious fault rupture plane to each grid cell with appropriate strike and dip angles. Hazards maps are prepared for the hard rock site condition in terms of the peak ground acceleration and the 5%-damping acceleration response spectrum amplitudes for several combinations of natural periods and return periods. A simple empirical approach is also developed to obtain amplification factors for modifying the uniform hazard response spectra for the rock sites to those for the soil sites with a given VS30 value. The hazard estimates from this study are found to be somewhat higher with greater site-to-site variations as compared to those from the earlier studies.
机译:这是利用概率地震危害分析方法对印度国家首都区地震宏观区的第一综合研究。用于这种目的的改进的网格地震性模型,其中使用古代伯格 - 里希特(G-R)关系获得的常规区域型地震源的关系获得的地震发生率在细胞网格中不均匀地分布。这提供了比均匀地震性的常用加权和无均匀地震源的加权和自由般平滑的网格状地震性的更稳健的方法。本分析的其他显着特征包括:区域的详细地震型评估区域以识别七个区域型地震源,编写全面地震目录,用于估计地震性复发参数,选择通过使用数据库选择最合适的地面运动预测方程式在该区域中记录的71个强运动加速度局,并通过将虚拟故障破裂平面与适当的击打和倾角相关联来估计兼容距离参数。在峰接地加速度和5%验证的加速度响应频谱振荡幅度的几个自然时段和返回时期的若干组合,为硬岩位点状况准备了危险地图。还开发了一种简单的经验方法,以获得用于将岩石部位均匀危害响应光谱改变为具有给定VS30值的土壤部位的扩增因子。与早期研究的研究相比,该研究的危险估计与较大的位点对现场变化有所更高。

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