F检测算法及其在识别地震地表反射波震相中的初步应用s

F-detection algorithm and its preliminary application toseismic surface reflected wave phase identification

  • 摘要: 地震P波波列中地表反射波pP或sP震相的准确识别,对地震震源深度的精确测定具有重要作用.基于新疆和田地震台阵部分地震记录数据,利用F检测算法对震中距分别为22.1deg;, 6.44deg;和39.62deg;的3次地震事件进行了地表反射波pP或sP震相检测.结果表明,应用F检测分析新疆和田小孔径地震台阵数据,可以帮助分析人员识别地震的地表反射波pP或sP震相.为进一步验证F检测算法对识别地表反射波震相的有效性,本文对震中距为22.1deg;的地震事件波形叠加不同水平噪声后,再进行F检测,结果仍能检测出其地表反射波震相.

     

    Abstract: Accurate identification of reflected wave phase pP or sP is of great importance in precise determination of focal depth. Using seismic wave data recorded by Hotan, Xinjiang, seismic array, we apply F-detection algorithm to identify pP or sP phase on P-wave seismograms of 3 earthquakes, of which the epicentral distances are 22.1deg;,6.44deg;and 39.62deg;, respectively. The study result indicates that the F-detection algorithm is helpful in relatively accurate identification of pP or sP phase. To verify the validity of F-detection algorithm, we use it to analyze the wave data of central distance 22.1deg;event with additional different level noises. The result indicates that pP or sP phase can still be identified.

     

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