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Seismic Zonation of the Delhi Region for Bedrock Ground Motion

机译:德里地区地震对基岩地面运动的影响

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An endeavor is made to compute peak ground horizontal accelerations at bedrock level in the Delhi region due to the seismogenic sources present around Delhi. The entire area is divided into six seismogenic sources for which seismic hazard analysis is carried out using the complete and extreme part of the seismicity data. Maximum likelihood estimates of hazard parameters viz., seismic activity rate λ, b value and maximum probable earthquake M_(max) are made for each zone. The return periods and the probabilities of occurrence of various magnitudes for return periods of 50, 100 and 1000 years are also computed for each zone. The peak ground acceleration (PGA) values for 20% exceedance in 50 years are then computed for the Delhi region from each zone. The maximum PGA value considering all the zones is 0.34 g, which is due to the Mathura fault zone. The seismogenic zones V and VI, i.e., Mathura fault zone and the Sohna fault zone are observed to the contributing maximum PGA values in the Delhi region governing he isoaccelrration contours computed for the region. The seismic zonation map for the PGA values at the bedrock level is obtained for the Delhi region. This can be used directly as input for the microzonation of ground motion at the surface by incorporating the local site conditions.
机译:由于德里附近存在地震源,因此人们努力计算德里地区基岩水平的峰值地面水平加速度。整个区域分为六个地震源,利用地震活动数据的完整和极端部分对其进行地震危险性分析。对每个区域进行危险参数的最大似然估计,即地震活动率λ,b值和最大可能地震M_(max)。还为每个区域计算了50年,100年和1000年的回归期和各种幅度的出现概率。然后,从每个区域计算德里地区50年内超过20%的峰值地面加速度(PGA)值。考虑到所有区域的最大PGA值为0.34 g,这是由于Mathura断层带造成的。在德里地区,观察到了震源区V和VI,即Mathura断层带和Sohna断层带对PGA贡献最大的最大值,从而控制了该区域的等加速度轮廓。获得了德里地区PGA值在基岩水平的地震分区图。通过结合当地的现场条件,可以将其直接用作地面运动微区划的输入。

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