黄春梅, 苏金蓉, 唐淋, 魏娅玲, 吴朋, 王宇航. 新震级国家标准在四川台网的应用——宽频带面波震级[J]. 华北地震科学, 2018, 36(1): 25-30. DOI: 10.3969/j.issn.1003-1375.2018.01.004
引用本文: 黄春梅, 苏金蓉, 唐淋, 魏娅玲, 吴朋, 王宇航. 新震级国家标准在四川台网的应用——宽频带面波震级[J]. 华北地震科学, 2018, 36(1): 25-30. DOI: 10.3969/j.issn.1003-1375.2018.01.004
HUANG Chun-mei, SU Jin-rong, TANG Lin, WEI Ya-ling, WU Peng, WANG Yu-hang. Application of the New National Magnitude Standards in Sichuan Network-Broadband Surface Wave Magnitude[J]. North China Earthquake Sciences, 2018, 36(1): 25-30. DOI: 10.3969/j.issn.1003-1375.2018.01.004
Citation: HUANG Chun-mei, SU Jin-rong, TANG Lin, WEI Ya-ling, WU Peng, WANG Yu-hang. Application of the New National Magnitude Standards in Sichuan Network-Broadband Surface Wave Magnitude[J]. North China Earthquake Sciences, 2018, 36(1): 25-30. DOI: 10.3969/j.issn.1003-1375.2018.01.004

新震级国家标准在四川台网的应用——宽频带面波震级

Application of the New National Magnitude Standards in Sichuan Network-Broadband Surface Wave Magnitude

  • 摘要: 利用四川区域地震台网记录到的国内2009-2016年间的217次地震事件,重新测定宽频带面波震级MS(BB)、面波震级MS和部分矩震级MW,并进行对比分析,结果显示:①MSMS(BB)差值分布为-0.1~0.6,其中97%的地震MSMS(BB)偏大,通过正交回归分析,MS(BB)MS系统偏小0.27左右;②MWMS差值为-0.8~0.35,其中MWMS差值在±0.3以内的地震数约为74%,由正交回归分析4.0 ≤ M ≤ 8.0时MS整体偏大,且偏差值随着震级的增加呈上升趋势,偏大范围为0.1~0.4之间;③MWMS(BB)差值分布为-0.5~0.55,差值在±0.3以内地震占87%,正交回归分析出4.0 ≤ M ≤ 5.0时MWMS(BB)偏大,偏大范围为0~0.13,而5.0 ≤ M ≤ 8.0时MWMS(BB)偏小,偏差值均在0.23以内。总体来说,相较于MSMS(BB)MW的偏差更小,MS(BB)更接近地震矩震级MW,更能准确评估地震震级。

     

    Abstract: We calculated the broadband surface wave magnitude MS(BB), surface wave magnitude MS and partial moment magnitude MW of 217 earthquakes in China recorded by Sichuan Seismic Network from 2009 to 2016. The systematic comparison and analysis research of the results shows:the difference between MS(BB) and MS is -0.1~0.6, for 97% earthquakes, MS is greater than MS(BB). The orthogonal regression analysis result shows, MS(BB) is about 0.27 less than MS. The difference between MW and MS is -0.8~0.35, for 74% earthquakes, the difference between MW and MS is within ±0.3. Through orthogonal regression analysis, for 4.0 ≤ M ≤ 8.0 earthquakes MS is greater than MW, the deviation range from 0.1~0.4 and increase with magnitude increasing. The difference between MW and MS(BB) is -0.55~0.5, for 74% earthquakes, the difference between MW and MS is within ±0.3. By orthogonal regression analysis, for 4.0 ≤ M ≤ 5.0 earthquakes MW is greater than MS(BB), the deviation range from 0.1~0.13, for 5.0 ≤ M ≤ 8.0 earthquakes MW is less than MS(BB), the deviation within 0.23. On the whole,the difference between MW and MS(BB) is less than MW and MS. That is, because of closer to MW, broadband surface wave magnitude MS(BB) can more accurately evaluate the magnitude of earthquake.

     

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