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首页> 外文期刊>Acta Geophysica >Frequency analysis of the 2004 Sumatra-Andaman earthquake using spectral seismograms
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Frequency analysis of the 2004 Sumatra-Andaman earthquake using spectral seismograms

机译:使用频谱地震图分析2004年苏门答腊-安达曼地震的频率

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Frequency analysis of the Sumatra-Andaman earthquake of 2004, one of the most significant and best-recorded earthquakes, is based on spectral seismograms obtained from their broadband seismograms. The Sumatra-Andaman earthquake is found to have a wide-range frequency content of P-wave radiation during the rupturing process. On the basis of stacking spectral seismograms we distinguished four time events of the rupturing process of a total length of about 540 s. The frequency, f_(max), is the highest for the first event (0.163 Hz in time interval 0-88 s), lowest for the second - which is the strongest (0.075 Hz in time interval 88-204 s). For third and fourth events frequencies are similar (0.089 and 0.082 Hz in time intervals 204-452 and 452-537 s, respectively). The frequency also shows an azimuthal dependence (±0.02 Hz). Azimuths for which the frequency, f_(max), has maximum and minimum values are 203-222° and 23-42°, respectively. These observations are discussed in relation to previously published papers on this topic.
机译:2004年苏门答腊-安达曼地震是最重要和记录最好的地震之一,其频率分析是基于从宽带地震图中获得的频谱地震图进行的。发现苏门答腊-安达曼地震在破裂过程中具有大范围的P波辐射频率范围。根据叠加的频谱地震图,我们区分了破裂过程的四个时间事件,总时间约为540 s。频率f_(max)在第一个事件中最高(时间间隔0-88 s中为0.163 Hz),在第二个事件中最低-频率最高(时间间隔88-204 s中为0.075 Hz)。对于第三和第四事件,频率是相似的(在时间间隔204-452和452-537 s中分别为0.089和0.082 Hz)。该频率还显示出方位角依赖性(±0.02 Hz)。频率f_(max)具有最大值和最小值的方位角分别为203-222°和23-42°。这些意见是与先前发表的有关该主题的论文相关的。

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