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Site Specific Ground Response Study of Deep Indo-Gangetic Basin Using Representative Regional Ground Motions

机译:利用代表性的区域地震动研究印度-恒河盆地深处的场地特定地面响应

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Massive damages due to repeated earthquake are evidenced since ancient times when compared to any other natural hazard. Such damages are not directly due to earthquakes but due to site effects and induced effects such as liquefaction. Earthquakes cannot be predicted precisely, but catastrophic damages and human loss due to earthquakes can be minimized by estimating earthquake hazard parameters. India is experiencing earthquake damages since 1200 AD, though very limited attempt have been made to estimate seismic hazard parameters on regional scale. Present study focuses on estimating spectral character of deep soils of Lucknow located close to Himalayan seismic belt. A detailed deterministic hazard analysis has been carried out at bedrock level. Subsurface stratums of study area have been investigated using Standard penetration tests and shear wave velocity profiling, which were used for seismic site classification. Site specific response analysis has been carried out using representative ground motions and local subsurface details.
机译:与任何其他自然灾害相比,自古以来就证明了由于反复地震造成的巨大破坏。这样的破坏不是直接由于地震引起的,而是由于场地效应和诸如液化的诱发效应。无法精确预测地震,但是可以通过估计地震危险参数来最大程度地减少由于地震造成的灾难性破坏和人员伤亡。自公元1200年以来,印度一直遭受地震破坏,尽管在区域范围内估计地震灾害参数的尝试非常有限。目前的研究侧重于估计位于喜马拉雅地震带附近的勒克瑙深层土壤的光谱特征。在基岩层进行了详细的确定性危害分析。研究区域的地下地层已使用标准渗透试验和剪切波速度剖面进行了调查,这些地震剖面被用于地震现场分类。已经使用代表性的地面运动和局部地下细节进行了针对特定地点的响应分析。

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