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Probabilistic assessment of surface level seismic hazard in India using?topographic gradient as a proxy for site condition

机译:使用地形坡度替代场地条件的印度地表地震危险性概率评估

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This paper presents spatial variation of seismic hazard at the surface level for India, covering 6–38° N and 68–98° E. The most recent knowledge on seismic activity in the region has been used to evaluate the hazard incorporating uncertainties associated with the seismicity parameters using different modeling methodologies. Three types of seismic source models, viz. linear sources, gridded seismicity model and areal sources, were considered to model the seismic sources and different sets of ground motion prediction equations were used for different tectonic provinces to characterize the attenuation properties. The hazard estimation at bedrock level has been carried out using probabilistic approach and the results obtained from various methodologies were combined in a logic tree framework. The seismic site characterization of India was done using topographic slope map derived from Digital Elevation Model data. This paper presents estimation of the hazard at surface level, using appropriate site amplification factors corresponding to various site classes based on V S30 values derived from the topographic gradient. Spatial variation of surface level peak horizontal acceleration (PHA) for return periods of 475 years and 2475 years are presented as contour maps. Graphical abstract Display Omitted Highlights ? Peak Ground Acceleration values due to possible future earthquakes. ? Different attenuation relations used to estimate ground motion. ? Seismic site characterization using topographic slope map. ? Surface level peak horizontal acceleration evaluated.
机译:本文介绍了印度地表覆盖6-38°N和68-98°E的印度地表地震危险的空间变化。该地区有关地震活动的最新知识已用于评估与地震相关的不确定性的灾害。使用不同建模方法的地震活动性参数。三种类型的地震源模型,即。考虑使用线性震源,网格化地震活动模型和面震源对震源进行建模,并针对不同构造省份使用了不同的地面运动预测方程组来表征衰减特性。基岩级别的危害估计已使用概率方法进行,并且将从各种方法获得的结果组合到逻辑树框架中。印度的地震现场特征描述是使用从数字高程模型数据得出的地形坡度图完成的。本文根据从地形梯度得出的V S30值,使用与各个工位类别相对应的适当工位放大系数,提出了对地表危害的估算。等高线图表示了475年和2475年回归期的地表水平峰值水平加速度(PHA)的空间变化。图形摘要显示省略的突出显示?由于可能发生的未来地震而导致的地面加速度峰值。 ?用于估计地面运动的不同衰减关系。 ?使用地形坡度图表征地震现场。 ?评估表面水平峰值水平加速度。

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