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LONG PERIOD IRANIAN STRONG MOTIONS RECORDED DURING1994-2002, PROCESSING AND ANALYSIS

机译:1994年至2002年期间记录的长时间伊朗强运动,处理和分析

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The recorded strong motion data in Iran since 1994 till the end of 2002 are investigated in order to findthe well recorded (high signal to noise ratio) accelerometric data, specially in the long period ranges. Therecords having low signal to noise ratio in the frequency range of less than 0.3 Hz are excluded, and therest of 100 records are processed and analyzed in this study. The site classification for these records isperformed based on the receiver function method (estimating the H/V ratio for each of the recordedmotions). According to this procedure, the numbers of the selected records were 46, 10, 16 and 28 for thesite classes 1, 2, 3 and 4, respectively. The records are presented based on their code, station name, siteclass, band-pass filter selected for each record, PGA (the greatest of three components), the event's date,epicentral region, moment magnitude, focal depths, focal mechanisms and the hypocentral distances. Thehypocentral distances are estimated for each record based on the s-p arrival time method. 100 recordscorresponding to 15 earthquakes are finally selected. The selected records have different frequencycontents and specifications. This difference corresponds to the magnitude and hypocentral distances, aswell as to the instrument type. Most of the records are noisy in the frequencies less than 0.3 Hz.However, some records show high signal to noise ratios in the frequency band of 0.3Hz or lower. Thefrequency contents of most of the records show dominant amplitudes between frequencies 0.2 and 10Hz.The Fmax values are systematically greater for the vertical components comparing to the horizontal ones.This selected catalog of 100 accelerograms obtained from 15 earthquakes provides a basis for the goodquality/recent strong motion records in Iran, having good quality low frequencies contents.
机译:为了找到记录良好的(高信噪比)加速度计数据,特别是在较长的时间范围内,对1994年以来至2002年底在伊朗记录的强运动数据进行了调查。在此研究中,排除了在0.3 Hz以下的频率范围内具有低信噪比的记录,其余100条记录被处理和分析。这些记录的站点分类基于接收者函数方法(估计每个记录的运动的H / V比)执行。根据此过程,站点级别1、2、3和4的所选记录数分别为46、10、16和28。根据记录的代码,站名,站点类别,为每个记录选择的带通滤波器,PGA(三个分量中最大的一个),事件的日期,主要区域,矩量,焦点深度,焦点机制和震源来显示记录。距离。根据s-p到达时间方法估算每个记录的震中距离。最终选择了对应于15次地震的100条记录。所选记录具有不同的频率内容和规格。此差异对应于幅度和下心距以及乐器类型。大多数记录在低于0.3 Hz的频率中都带有噪声,但是,有些记录显示在0.3Hz或更低的频带中信噪比很高。大多数记录的频率内容显示了0.2至10Hz频率之间的主要振幅。垂直分量的Fmax值与水平分量的Fmax值系统地更大。从15次地震中选择的100张加速度图的选定目录为质量/最近的加速度提供了基础伊朗的高动态记录,具有高质量的低频内容。

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  • 来源
  • 会议地点 Vancouver(CA);Vancouver(CA)
  • 作者

    Mehdi ZARE;

  • 作者单位

    International Institute of Earthquake Engineering and Seismology (IIEES) Tehran P.O.Box: 19395/3913 Iran e-mail:mzare@iiees.ac.ir;

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