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Source Parameters and Epicentral Relocation of The 22 June 2002 Avaj Earthquake

机译:2002年6月22日AVAJ地震的源参数和震中搬迁

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The Changoureh-Avaj earthquake of June 22nd 2002 is the largest shock since the occurrence of the 1962 Buyin-Zahra earthquake in Qazvin province. The ground-motion characteristics during the main shock should be considered for the high safety design of structures in the region. we calculated the ground motion parameters of this event using digital accelerograms Data of Building and Housing Research Center (BHRC) by using Seismosignal and Sigmaplot softwares. The earthquake was recorded by 78 digital accelerographs installed in different points of the area. We used 18 accelerograms which had good signal to noise ratios at a distance range of 26 - 100 km. The maximum acceleration recorded in this event so far is about 0.5g at the Avaj station which is situated 26km from the earthquake hypocentre. We relocated the epicentre of this event and the first 23 aftershocks by using Tehran Seismic Network Data and Hypoinverse Software. A focal depth of 7 km is estimated for the mainshock. Different seismological Agencies such as (IGTU, NEIC, HRVD) reported different location, in this study, results are consistent with the computation results.
机译:2002年6月22日的长江 - Avaj地震是自1962年Qazvin省省1962年苏州扎哈拉地震发生以来的最大震荡。主要休克期间的地运动特性应考虑该地区结构的高安全性设计。我们使用SeisMoSignal和Sigmaplot软件使用建筑和住房研究中心(BHRC)的数字加速器数据计算了这一事件的地面运动参数。地震录制了78个数字加速器,安装在该地区的不同点。我们使用了18臂,其发出良好的噪声比率,距离范围为26到100公里。到目前为止在此事件中记录的最大加速度为AVAJ站的约0.5g,位于距离地震效率26公里。我们通过使用德黑兰地震网络数据和倍增软件重新安置了这一事件的震中和前23个余震。主屏幕估计了7公里的焦距。在本研究中报告了不同地点(IGTU,NeiC,HRVD)的不同地震机构(IGTU,NEIC,HRVD),结果与计算结果一致。

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