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On correlation between seismic activities and focal mechanisms of subsequent strong earthquakes
作者姓名:王慧敏  黎明晓  吕梅梅  张晓东
作者单位:China Earthquake Networks Center, China Earthquake Administration, Beijing 100036, China
基金项目:State Science and Techniology Key Program (2004BA601 B01-01, 2004BA601 B01-01-04).
摘    要:Introduction Earthquakes are direct results from tectonic deformation and crustal movements, which usu- ally contain abundant information of crustal stress status and medium property in the deep lithosphere. Seismic activities might reflect accumulation and concentration of crustal stress in the seismogenic process. And different mechanisms of rock ruptures lead to different precursory phe- nomena prior to earthquakes (ZHANG, et al, 2001). Therefore, seismic activities before a strong earthq…

关 键 词:震源机制  地震  活动性  相关分析
文章编号:1000-9116(2006)04-0406-11
收稿时间:2005-12-21
修稿时间:2006-03-13

On correlation between seismic activities and focal mechanisms of subsequent strong earthquakes
WANG Hui-min,LI Ming-xiao,LU Mei-mei,ZHANG Xiao-dong.On correlation between seismic activities and focal mechanisms of subsequent strong earthquakes[J].Acta Seismologica Sinica(English Edition),2006,19(4):406-416.
Authors:WANG Hui-min  LI Ming-xiao  LU Mei-mei  ZHANG Xiao-dong
Institution:China Earthquake Networks Center, China Earthquake Administration, Beijing 100036, China
Abstract:On the basis of the results from spatial-temporal scanning of moderate seismic activities prior to 63 strong earth- quakes occurred since 1966, we investigate in this paper the characteristics of anomalous evolution of moderate seismic activities prior to strong earthquakes with different focal mechanisms in different tectonic blocks, as well as the correlation between principal seismic activities and nodal planes of focal mechanisms. The research results indicate that the moderate seismic activities prior to strong earthquakes display two significant stages of stress concentration and stress weakening, which are consistent to the evolvement of local tectonic stress field. The first stage, defined as medium-term stage, is characterized by seismic belts, seismic gaps and centralized activities; The second stage, defined as short-term stage, is predominated by continuous quiescence. For the earthquakes occurred on the strike-slip and normal faults, the two stages are relatively evident; while for the earthquakes occurred on the thrust faults, there are not characteristic images and seismic quiescence in both stages. The spatial distribution of moderate shock belts before strong earthquakes show a good coherence with that of the two nodal planes of focal mechanisms, while the spatial distribution of seismic gaps enclosed by moderate shocks display a poor coherence with the nodal planes.
Keywords:focal mechanism  strong earthquake  seismic activity  correlation analysis
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