李赞, 刘瑞丰, 孔韩东, 王子博, 袁乃荣. 2019: 中强地震能量震级测定. 地震学报, 41(3): 289-301. DOI: 10.11939/jass.20180139
引用本文: 李赞, 刘瑞丰, 孔韩东, 王子博, 袁乃荣. 2019: 中强地震能量震级测定. 地震学报, 41(3): 289-301. DOI: 10.11939/jass.20180139
Li Zan, Liu Ruifeng, Kong Handong, Wang Zibo, Yuan Nairong. 2019: Energy magnitude determination of moderate-strong earthquakes. Acta Seismologica Sinica, 41(3): 289-301. DOI: 10.11939/jass.20180139
Citation: Li Zan, Liu Ruifeng, Kong Handong, Wang Zibo, Yuan Nairong. 2019: Energy magnitude determination of moderate-strong earthquakes. Acta Seismologica Sinica, 41(3): 289-301. DOI: 10.11939/jass.20180139

中强地震能量震级测定

Energy magnitude determination of moderate-strong earthquakes

  • 摘要: 本文根据地震波衰减特性,开展了利用宽频带地震波形数据测定地震波能量ES和能量震级Me的方法研究。利用震中距处于20°—98°范围内的宽频带远震P波波形数据,测定了4次国外和4次国内中强震的能量震级Me,并对其面波震级MS、矩震级MW及能量震级Me进行了分析对比。结果表明:面波震级MS表示的是地震在某一固定频率所辐射的地震波能量大小;矩震级MW与地震所产生的断层长度、断层宽度、震源破裂的平均位错量等静态构造效应密切相关;而能量震级Me反映的是震源动态特征,与地震震源的动力学特性密切相关。由于地震是以地震波形式辐射,能量主要集中在震源谱的拐角频率附近,因此能量震级Me更适合描述地震的破坏性。由此可见,联合测定面波震级MS,矩震级MW和能量震级Me对于地震定量研究以及地震灾害与风险评估具有重要作用。

     

    Abstract: This paper, based on the seismic wave attenuation characteristics, explores a method for utilizing broadband seismic waveform data to measure seismic energy ES and energy magnitude Me. The energy magnitudes Me of four overseas and four domestic moderate-strong earthquakes are measured by using broadband teleseismic P waveform data with epicentral distance in the range of 20°−98°. The comparison of surface wave magnitude MS, moment magnitude MW and energy magnitude Me of several earthquakes shows that: surface wave magnitude MS represents the magnitude of the energy of seismic wave radiating at a fixed frequency; the moment magnitude MW is closely related to the static structural effects such as the length of fault, the width of fault and the average dislocation amount of the source rupture produced by the earthquake; the energy magnitude Me reflects source dynamic characteristics and is closely related to the dynamic characteristics of the seismic source. The energy radiated by the earthquake in the form of seismic waves is mainly concentrated near the corner frequency of the source spectrum, so the energy magnitude Me is more suitable to describe the destructiveness of the earthquake. Therefore, joint determination of surface wave magnitude MS, moment magnitude MW and energy magnitude Me are of great significance for quantifying and evaluating the disasters caused by earthquakes or tsunamis.

     

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