魏贵春, 姚运生, 张丽芬, 申学林. 2017: 方位角对地方震震级测定的影响. 地震学报, 39(6): 880-890. DOI: 10.11939/jass.2017.06.006
引用本文: 魏贵春, 姚运生, 张丽芬, 申学林. 2017: 方位角对地方震震级测定的影响. 地震学报, 39(6): 880-890. DOI: 10.11939/jass.2017.06.006
Wei Guichun, Yao Yunsheng, Zhang Lifen, Shen Xuelin. 2017: Influences of azimuth on the local earthquake magnitude measurement. Acta Seismologica Sinica, 39(6): 880-890. DOI: 10.11939/jass.2017.06.006
Citation: Wei Guichun, Yao Yunsheng, Zhang Lifen, Shen Xuelin. 2017: Influences of azimuth on the local earthquake magnitude measurement. Acta Seismologica Sinica, 39(6): 880-890. DOI: 10.11939/jass.2017.06.006

方位角对地方震震级测定的影响

Influences of azimuth on the local earthquake magnitude measurement

  • 摘要: 收集了湖北省数字测震台网2007—2015年记录到的数字地震波形,利用震相清晰的台站测定了地方震震级,并计算了其与中国地震台网中心公布震级的偏差.在此基础上,以每个数字测震台站为中心,按照每30°为一个区间,将每个台站记录到的地震事件分为12个区间,对每个区间的平均震级偏差和标准离差予以统计分析.结果显示,除去24个无地震事件区间,300个区间的平均震级偏差中,81.7%的偏差小于0.3;再除去14个样本数为1的区间,其余286个区间的方位标准离差中,98.3%的离差小于0.5.经校正后各区间的平均震级偏差和方位标准离差均有所下降,表明地震传播方位对地方震震级测定的影响有所降低.因此,针对数字测震台站对不同方位地震所测定的震级偏差存在的差异进行相应校正是必要且有意义的.

     

    Abstract: Azimuth is one of the factors that affect the local earthquake magnitude measurement. In this study, we collected the earthquake events from 2007 to 2015 recorded by the Hubei regional seismograph network. Using the digital seismic waveforms, we measured the magnitudes of the local earthquakes in the Hubei area and calculated the magnitude differences from those published by the China Earthquake Networks Center. To deep understand the influences of azimuth on the local earthquake magnitude measurement, the average magnitude deviation and standard deviation in each interval are statistically analyzed. Taking each digital seismic station as the center, the earthquake events recorded by each station are divided into 12 intervals with 30° as an interval. The results show that except the 24 non-earthquake intervals, in the remaining 300 intervals the average magnitude deviation less than 0.3 accounts for 81.7%. Furthermore, deducting the 14 intervals with only one event, in the other 286 intervals, 98.3 percentage of the azimuth standard deviation is less than 0.5. After azimuth corrections, both the average magnitude deviations and the azimuth standard deviations of each interval decrease, indicating the influences of azimuth on the measurement of local earthquake magnitude decreasing. Therefore, it is necessary and meaningful to correct the magnitude deviation caused by different azimuths.

     

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