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汶川地震序列b值的分析研究
引用本文:王俊,阮祥,郑江蓉,孙业君,江昊琳,詹小艳.汶川地震序列b值的分析研究[J].地震地磁观测与研究,2009,30(2):15-21.
作者姓名:王俊  阮祥  郑江蓉  孙业君  江昊琳  詹小艳
作者单位:1. 中国南京,210014,江苏省地震局
2. 中国成都,610041,四川省地震局
基金项目:中国地震局科技支撑计划 
摘    要:采用Aki等(1965)和Shi等(1982)计算b值及标准差的方法,分析了2008年5月12日~2008年8月31日四川地震台网所记录到的汶川地震序列ML≥2.0地震的b值,在空间、时间以及随震源深度的变化特征。结果显示:汶川地震序列b值在震源区上分布是非均匀的,但基本在0.5,0.9]之间变化,震源区的中段b值高于两端;同时发现,几次M≥6.0余震都发生在b值较低的区域内;震源区b值具有随震源深度增加而减小的趋势,在20km左右处,减小的趋势最为明显;随着时间的推移,b值波动变化幅度逐渐减小,周期变大。

关 键 词:汶川地震序列  b值  震源区  震源深度

Study on the variation of b value in Wenchuan earthquake series
Wang Jun,Ruan Xiang,Zhen Jiangrong,Sun Yejun,Jiang Haolin,Zhan Xiaoyan.Study on the variation of b value in Wenchuan earthquake series[J].Seismological and Geomagnetic Observation and Research,2009,30(2):15-21.
Authors:Wang Jun  Ruan Xiang  Zhen Jiangrong  Sun Yejun  Jiang Haolin  Zhan Xiaoyan
Institution:Wang Jun , Ruan Xiang , Zhen Jiangrong , Sun Yejun , Jiang Haolin , Zhan Xiaoyan(1.Earthquake Administration of J iangsu Province, Nanjing 210014, China;2. Earthquake Administration of Sichuan Province, Chengdu 610041, China)
Abstract:In this paper, using the method presented by Aki(1965), Shi and Bolt (1982), the b value in Wenehuan earthquake series (ML≥2.0) recorded by Sichuan seismic network at the time between 2008-05-12 and 2008-08-31 is analyzed. The results show that the variation of b val- ue in the earthquake source region is non-uniform. The b value is in the range form 0. 5 to 0.9, and the b value of middle segment of the earthquake source region is high than that of other regions. At the same time, we found that almost all strong aftershoeks (M≥6.0) occurred in the low b value region. In addition, the results show that the b value deceases with earthquake depth increasing. The variation features is most significant at 20 km depth. The variation of b value of Wenchuan earthquake series with time was also discussed. The variation of amplitude is deceasing with time and the variation of period is on the contrary.
Keywords:Wenchuan earthquake series  b value  earthquake source region  earthquake depth
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