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一种矩张量反演新方法及其对2008年汶川M_S8.0地震序列的应用 被引量:42

A new technique for moment tensor inversion with applications to the 2008 Wenchuan M_S8.0 earthquake sequence
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摘要 本文利用全球地震台网(GSN)的宽频带与长周期地震波形资料,采用矩张量反演的新方法,反演得到了2008年5月12日四川省汶川县MS8.0地震及其7个较大余震(MS5.0—6.0)的矩张量解与震源时间函数等震源参数.文章首先简要叙述矩张量反演新方法的理论背景和技术途径,并以汶川大地震的一个余震为例阐述了具体的实现过程;然后给出包括主震在内的8次地震的矩张量解和震源时间函数;最后分析探讨这些结果的构造意义.本文提出的矩张量反演新方法,不但与全球矩心矩张量(GCMT)一样,可以给出点源矩张量解,而且还可以给出点源的震源时间函数.反演得到的汶川大地震的7个较大余震的震源时间函数表明,即使是中等强度的地震也可能有复杂的震源过程;汶川大地震的多数余震发生在以逆冲为主、兼具小量走滑分量的龙门山断裂带的主断裂上,但很可能有些余震则发生在主断裂附近的次级走滑断裂上. A Ms8.0 earthquake occurred in Wenchuan County, Sichuan Prov ince, on May 12, 2008, and subsequently, numerous aftershocks followed. We obtained the moment tensor solutions and source time functions (STFs) for the Wenchuan earthquake and its 7 larger aftershocks (Ms5.0 6.0) by a new technique of moment tensor inversion using the broadband and long-period seismic waveform data from the Global Seismographic Network (GSN). Firstly, the theoretical background and technical flow of the new technique was briefly introduced, and an aftershock of the Wenchuan earthquake sequence was employed to illustrate the practical procedure for inverting the moment tensor; then, the moment tensor solutions and STFs of the 8 events, including the main shock, were presented; and finally, the interpretation of the results was made. The agreement of our results with the GCMT results indicates that the new technique is efficient and feasible. By using this technique, not only the moment tensor solution can be obtained but also the STF can be retrieved; the inverted STFs indicate that the source rupture process may be complicated even for the moderate earthquakes. The inverted focal mechanisms of the Wenchuan earthquake sequence show that most of the aftershocks occurred in the main faults of the Longmenshan Fault Zone with predominantly thrusting with minor right-lateral strike-slip component, but some of them may have occurred in the subfaults with strike-slip faulting in the vicinity of the main faults.
出处 《地震学报》 CSCD 北大核心 2008年第4期329-339,共11页 Acta Seismologica Sinica
基金 国家基础研究计划(2004CB418404-4 2001CB711005) 国家自然基金项目(40574025 40474018) 中国地震局地球物理研究所基本业务专项(PQJB08Z05)资助 中国地震局地球物理研究所论著08AC2020
关键词 矩张量反演 汶川地震 震源时间函数 震源机制 Moment tensor inversion Wenehuan earthquake source time function focal mechanism
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参考文献18

  • 1陈国光,计凤桔,周荣军,徐杰,周本刚,黎小刚,叶友青.龙门山断裂带晚第四纪活动性分段的初步研究[J].地震地质,2007,29(3):657-673. 被引量:188
  • 2陈运泰.巧家、石棉的小震震源参数的测定及其地震危险性的估计[J].地球物理学报,1976,19(3).
  • 3许力生,陈运泰.2004.格林函数库技术与快速地震矩张量反演[G]//陈运泰,滕吉文,阚荣举,等主编.中国大陆地震学与地球内部物理学研究进展:庆贺曾融生院士八十寿辰.北京:地震出版社:625-630.
  • 4张勇,冯万鹏,许力生,周成虎,陈运泰.2008年汶川大地震的时空破裂过程[J].中国科学(D辑),2008,38(10):1186-1194. 被引量:214
  • 5Dziewonski A M, Woodhouse J H. 1983. An experiment in the systematic study of global seismicity:Centroid-moment tensor solutions for 201 moderate and large earthquakes of 1981[J]. J Geophys Res, 88:3247-3271.
  • 6Dahm T. 1996. Relative moment tensor inversion based on ray theory: Theory and synthetic tests[J]. Geophys J Int, 124(1): 245-257.
  • 7Frohlich C, Davis S D. 1993. Teleseismic h values Or, much ado about 1.0[J]. J Geophys Res, 98: 641-644.
  • 8Gilbert F, Dziewonski A M. 1975. An application of normal mode theory to the retrieval of structural parameters and source mechanisms from seismic spectra[J]. PhilTrans Roy Soci London, 278: 187-269.
  • 9Kagan Y Y. 1997. Seismic moment frequency relation for shallow earthquakes: Regional comparison[J]. J Geophys Res, 102:2835-2852.
  • 10Kagan Y Y. 2000. Temporal correlations of earthquake focal mechanisms[J]. Geophys J Int, 143: 881-897.

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