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INTRODUCTION AND PRELIMINARY ANALYSIS OF STRONG MOTION RECORDINGS FROM THE 12 MAY 2005 Ms8.0 WENCHUAN EARTHQUAKE OF CHINA*

机译:2005年5月12日中国汶川Ms8.0地震强运动记录的介绍和初步分析*

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An Ms8.0 Wenchuan earthquake occurred on the Longmenshan fault belt in Sichuan, China on 12 May 2008.The strong motion recordings of the main shock are obtained from 460 permanent free-field stations and three arrays for topographical effect and structural response observation in the National Strong Motion Observation Network System (NSMONS) of China, and a large numbers of acceleration records from the strong aftershocks occurred were also obtained by permanent free-field stations of the NSMONS and 59 mobile instruments quickly deployed after the main shock. The mobile instruments are specifically deployed to record the strong motions of the strong aftershocks for the purposes of near-fault effect, topographical effect, basin effect and structural response observation. This paper provides a detailed description of the relevant stations and the resultant strong motion measurements of the main shock, and a brief description of the mobile observation. The preliminary analysis of the recordings shows that over 1,400 components of strong motion records are obtained from the main shock. Among the records, there are more than 500 components with peak ground acceleration (PGA) larger than 10 gal, 200 larger than 50 gal, 115 larger than 100 gal, 42 larger than 200 gal, 16 larger than 400 gal, and 7 larger than 600 gal. With the stations of the NSMONS and mobile stations, over 20,000 components of acceleration records were obtained from strong aftershocks. In the aftershock records, the largest PGA has exceeded 800 gal which was recorded in the Qingchuan aftershock on 5 August 2008. Some near-fault properties of recordings are also demonstrated such as large vertical acceleration, rupture directivity effect, fault slip effect, hanging wall effect, basin effect, etc.
机译:2008年5月12日,中国四川龙门山断裂带发生汶川Ms8.0地震。主要地震记录来自460个永久性自由场台站和三个阵列,用于观测该地区的地形影响和结构响应。中国的国家强震观测网络系统(NSMONS),以及由NSMONS的永久性自由场站以及在主震发生后迅速部署的59台移动仪器,也获得了来自强余震发生的大量加速记录。移动仪器专门用于记录强余震的强烈运动,以用于近断层效应,地形效应,盆地效应和结构响应观测。本文提供了有关台站的详细说明以及由此产生的主要冲击的强运动测量结果,以及对移动观测的简要说明。记录的初步分析表明,从主震中获得了1,400多个强运动记录的成分。在记录中,有超过500个组件的峰值地面加速度(PGA)大于10 gal,200大于50 gal,115大于100 gal,42大于200 gal,16大于400 gal,以及7大于500 gal。 600加仑借助NSMONS台站和移动台,从强余震中获得了20,000多个加速度记录组成部分。在余震记录中,最大的PGA已超过800 gal,这是2008年8月5日在青川余震中记录的。还显示了一些接近断层的记录特性,例如较大的垂直加速度,破裂指向性效应,断层滑动效应,悬墙。效果,流域效果等

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