期刊文献+

新震级国家标准在四川台网的应用——宽频带面波震级 被引量:3

Application of the New National Magnitude Standards in Sichuan Network-Broadband Surface Wave Magnitude
下载PDF
导出
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M_(S(BB))、面波震级M_S和部分矩震级M_W,并进行对比分析,结果显示:(1)M_S与M_(S(BB))差值分布为-0.1~0.6,其中97%的地震M_S较M_(S(BB))偏大,通过正交回归分析,M_(S(BB))较M_S系统偏小0.27左右;(2)M_W与M_S差值为-0.8~0.35,其中M_W与M_S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M_S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;(3)M_W与M_(S(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M_W较M_(S(BB))偏大,偏大范围为0~0.13,而5.0≤M≤8.0时M_W较M_(S(BB))偏小,偏差值均在0.23以内。总体来说,相较于M_S,M_(S(BB))与M_W的偏差更小,M_(S(BB))更接近地震矩震级M_W,更能准确评估地震震级。 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.
机构地区 四川省地震局
出处 《华北地震科学》 2018年第1期25-30,共6页 North China Earthquake Sciences
基金 中国地震局测震台网青年骨干培养专项(20160521 20170620) 中国地震局台站三结合课题(CEA-JC/3JH-162301 CEA-JC/3JH-162306)
关键词 面波震级MS 宽频带面波震级MS(BB) 矩震级MW 正交回归 broadband surface wave magnitude MS(BB) surface wave magnitude MS moment magnitude MW
  • 相关文献

参考文献2

二级参考文献61

  • 1陈运泰,刘瑞丰.地震的震级[J].地震地磁观测与研究,2004,25(6):1-12. 被引量:120
  • 2陈培善.面波震级测定的发展过程概述[J].地震地磁观测与研究,1989,10(6):1-9. 被引量:14
  • 3刘瑞丰,陈运泰,PETER BORMANN,任枭,侯建民,邹立晔,杨辉.中国地震台网与美国地震台网测定震级的对比(Ⅱ)——面波震级[J].地震学报,2006,28(1):1-7. 被引量:57
  • 4[3]Abe K. 1995. Magnitudes and moments of earthquakes. In: Ahrens T J. (ed). Global Earth Physics: A Handbook of Physical Constants[M]. Washington:American Geophysical Union,206~213
  • 5[4]Abe K and Kanamori H. 1979. Temporal variation of the activity of intermediate and deep focus earthquakes[J]. J Geophys Res,84:3 589~3 595
  • 6[5]Aki K. 1966. Generation and propagation of G waves from Niigata earthquake of June 16,1964. Estimation of earthquake movement, released energy and stress-strain drop from G wave spectrum[J]. Bull Earthq Res Inst. Tokyo Univ, 44: 23~88
  • 7[6]Aki K. 1967. Scaling law of seismic spectrum[J]. J Geophys Res,72:1217~1231
  • 8[8]Bormann P. (ed). 2003. New Manual of Seismological Observatory Practice[M]. (in Press)
  • 9[9]Chinnery M A and North R G. 1975. The frequency of very large earthquake[J]. Science, 190:1197~1198
  • 10[10]Duda S J. 1989. Earthquakes: Magnitude, energy, and intensity. In:James D. (ed). Encyclopedia of Solid Earth Geophysics [M],272~288. New York: Van Nostrand-Reinhold

共引文献168

同被引文献14

引证文献3

二级引证文献15

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部