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首页> 外文期刊>Bulletin of the Seismological Society of America >Analysis of horizontal strong-motion attenuation in the great 2008 Wenchuan earthquake
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Analysis of horizontal strong-motion attenuation in the great 2008 Wenchuan earthquake

机译:2008年汶川特大地震水平强震衰减分析

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摘要

A large number of strong-motion records were obtained by the National Strong-Motion Observation Network System (NSMONS) of China for the Wenchuan earthquake. There are 1350 components of strong-motion records from the mainshock at 455 stations. In these stations, 164 stations are located in the range of rupture distance within 400 km and 37 stations are within 100 km. The largest peak ground acceleration is 957.8 Gal from the Wolong station in the hanging wall area with rupture distance of 23 km. The records from 164 stations in the range of rupture distance within 400 km are used in this study to investigate the hanging wall/footwall effects, directivity effects, and attenuation characteristics of ground motions from theWenchuan earthquake. The characteristics of ground motion attenuations are compared in four subareas: hanging wall area, footwall area, forward directivity area, and backward directivity area. The study results show a clear hanging wall/footwall effect in near-fault ground motions within a rupture distance of 40 km, but it appears only in the peak ground acceleration and components at short periods below 1.0 s, and a strong forward directivity effect appears in ground motions over the whole range of rupture distance and period. Furthermore, the fitting attenuation curves of the peak ground acceleration and spectral accelerations of ground motions from the Wenchuan earthquake are compared with the predicted curves by an empirical attenuation model in the hanging wall and footwall areas.
机译:中国国家强震观测网络系统(NSMONS)获得了汶川地震的大量强震记录。 455个台站的主震记录有1350个强震记录组成部分。在这些站中,破裂距离在400 km以内的有164个站,而在100 km以内的有37个站。距挂壁区域卧龙站最大的地面加速度峰值是957.8 Gal,破裂距离为23 km。在这项研究中,使用了164个破裂点在400 km范围内的台站的记录,以调查汶川地震的悬壁/底盘效应,方向性效应以及地震动的衰减特征。在四个子区域中比较了地震动衰减的特征:悬挂壁区域,下盘壁区域,前向指向性区域和后向指向性区域。研究结果表明,在40 km破裂距离内的近断层地面运动中,明显的悬壁/底盘效应明显,但仅出现在峰值地面加速度和1.0 s以下短时间内的分量中,并且出现了强烈的前向指向性效应。在整个破裂距离和破裂周期范围内的地面运动中。此外,通过经验衰减模型,将实测的汶川地震的峰值地面加速度和地震动的频谱加速度的拟合衰减曲线与预测曲线进行比较,并将其与悬壁和底壁区域的衰减曲线进行比较。

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