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云南及周边地区Lg尾波Q值的分布特征 被引量:46

DISTRIBUTION CHARACTERISTICS OF Q VALUE OF THE Lg CODA IN YUNNAN AND ITS ADJACENT REGIONS
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摘要 收集了昆明台 1990~ 2 0 0 0年间大于 4 .0级的地震宽频记录资料 ,以及分布在云南境内的 2 3个昆明数字化台网 1999~ 2 0 0 0年的资料 ,使用单台叠加谱比方法处理了 2 80个Lg尾波信号 .在假定Lg尾波Q与频率f有Q=Q0 fη关系的基础上 ,计算出各射线 1Hz时的Q值及频率相关因子 η .在此基础上 ,运用反投影技术反演得到云南及周边地区 0 .5°× 0 .5°网格内的Q0 和 η的分布图像 .结果表明 :云南及周边地区的Q0 在 15 0~ 30 0之间变化 ,滇东地区的Q0 明显高于滇西地区 ;η的变化范围在 0 .3~ 0 .8之间 ,绝大部分地区 η的变化范围为 0 .5~ 0 .6 . We have collected broadband seismograms of earthquakes with magnitudes greater than 4.0 recorded by the Kunming station during the period 1990~2000 and 23 Kunming digital network stations located in Yunnan province during the period 1999~2000. The total 280 Lg coda traces are studied using the stack spectral ratio (SSR) method. Supposing Q of Lg coda correlates with frequency, f by Q=Q 0f η, the Q value at 1Hz, Q 0 and η for each record are calculated. Based on the calculated results, the distribution maps of Q 0 and η for 0.5°×0.5° cells are obtained using the back-projection technique. The results indicate Q 0 in Yunnan and its adjacent regions exhibits low values, varying between 150 and 300. Q 0 in eastern Yunnan is higher than that in western Yunnan. η varies between 0.3 and 0.8. For most of the study regions η is within the range between 0.5 and 0.6.
出处 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2003年第6期809-813,T004,共6页 Chinese Journal of Geophysics
基金 云南省自然科学基金 ( 98D0 0 3R) 国家自然科学基金 ( 4 99740 12 40 2 740 3 0 )
关键词 LG尾波 叠加谱比 反投影技术 Q成像 Lg coda, Stack spectral ratio, Back-projection technique, Q tomography.
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参考文献20

  • 1Knopoff L, Schwab F, Kausel E. Interpretation of Lg. Geophys. J.R. Astr. Soc., 1973, 33: 389-404
  • 2Herrmann R B, Kijko A. Modeling some empirical Lg relations.Bull. Seism. Soc. Am., 1983, 56: 172~ 257
  • 3Wang C Y, Herrmann R B. Synthesis of coda waves in layered medium. Pure Appl. Geophys., 1988, 128: 7 ~ 42
  • 4Zhang T, Lay T. Why the Lg phase does not traverse oceanic crust.Bull. Seism. Soc. Am. , 1995, 85: 1665- 1678
  • 5Mitchell B J. Anelastic structure and evolution of the continental crust and upper mantle from seismic surface wave attenuation. Rev. of Geophysics, 1995, 33(2): 441 ~ 462
  • 6Henmann R B. Q estimates using coda of local earthquakes. Bull.Seism. Soc. Am., 1980, 70:447~469
  • 7Xie J, Nuttli O W. Interpretation of high-frequency coda at large distances: stochastic modeling and method of inversion. Geophysical J.Int., 1988, 95:579~5951
  • 8Aki K. Analysis of the seismic coda of local earthquakes as scatted waves. J. Geophys. Res., 1969, 74(2): 615 ~ 663
  • 9Baqer S, Mitchell B J. Regional variations of Lg coda Q in the continental United States and its relation to crustal structure and evolution.Pure Appl. Geophys., 1998, 158:613 ~ 638
  • 10De Souza J L, Mitchell B J. Lg coda Q variations across South America and their relation to crustal evolution. Pure Appl. Geophys.,1998, 158:587 ~ 612

二级参考文献28

  • 1徐常芳,豫北-鲁西南地区地球物理综合探测研究专辑,1989年
  • 2孙洁,中国地震,1988年,4卷,3期
  • 3虢顺民,现代地壳运动研究.4,1988年
  • 4孔祥儒,地球物理学报,1987年,30卷,2期
  • 5吴乾蕃,地震地质,1987年,10卷,4期
  • 6金性春,板块构造学基础,1987年
  • 7阚荣举,中国地震,1986年,2卷,4期
  • 8吴大宁,现代地壳运动研究.1,1985年
  • 9张俊昌,云南现代断裂活动与地震危险性分析,1985年
  • 10刘国栋,大地电磁测深研究,1984年

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