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Estimation of Source Parameters of M_w 6.9 Sikkim Earthquake and Modeling of Ground Motions to Determine Causative Fault

机译:M_w 6.9锡金地震震源参数的估计和地动建模以确定原因断层

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摘要

In this study, source parameters of the September 18, 2011 M_w 6.9, Sikkim earthquake were determined using acceleration records. These parameters were then used to generate strong motion at a number of sites using the stochastic finite fault modeling technique to constrain the causative fault plane for this earthquake. The average values of corner frequency, seismic moment, stress drop and source radius were 0.12 Hz, 3.07 × 10~(26) dyne-cm, 115 bars and 9.68 km, respectively. The fault plane solution showed strike-slip movement with two nodal planes oriented along two prominent lineaments in the region, the NEoriented Kanchendzonga and NW-oriented Tista lineaments. The ground motions were estimated considering both the nodal planes as causative faults and the results in terms of the peak ground accelerations (PGA) and Fourier spectra were then compared with the actual recordings. We found that the NW-SE striking nodal plane along the Tista lineament may have been the causative fault for the Sikkim earthquake, as PGA estimates are comparable with the observed recordings. We also observed that the Fourier spectrum is not a good parameter in deciding the causative fault plane.
机译:在这项研究中,使用加速度记录确定了2011年9月18日锡金M_w 6.9级地震的震源参数。然后,使用随机有限断层建模技术将这些参数用于在多个站点产生强运动,以约束该地震的致病性断层。拐角频率,地震矩,应力降和震源半径的平均值分别为0.12 Hz,3.07×10〜(26)达因-厘米,115巴和9.68 km。断层平面解显示走滑运动,其中两个节点平面沿着该地区的两个突出线,朝向NE的Kanchendzonga和西北的Tista线。估计地面运动时将节点面视为致病性断层,然后将有关峰值地面加速度(PGA)和傅立叶谱的结果与实际记录进行了比较。我们发现,沿着Tista台面的NW-SE撞击节点平面可能是锡金地震的致病性断层,因为PGA估算值与观测到的记录相当。我们还观察到,傅立叶频谱不是确定故障平面的好参数。

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