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Paterns and regularity of ring distribution of seismic activity before great earthquakes in China
引用本文:梅世蓉,宋治平,薛艳.Paterns and regularity of ring distribution of seismic activity before great earthquakes in China[J].地震学报(英文版),1996,9(4):535-543.
作者姓名:梅世蓉  宋治平  薛艳
作者单位:SHI RONGMEI,ZHI PINGSONG and YAN XUE Center for Analysis and Prediction,State Seismological Bureau,Beijing 100036,China
摘    要:PaternsandregularityofringdistributionofseismicactivitybeforegreatearthquakesinChinaSHI-RONGMEI(梅世蓉),ZHI-PINGSONG(宋治平)andYAN...

收稿时间:11 March 1995
修稿时间:21 August 1995

Patterns and regularity of ring distribution of seismic activity before great earthquakes in China
SHI RONGMEI,ZHI PINGSONG and YAN XUE Center for Analysis and Prediction,State Seismological Bureau,Beijing ,China.Patterns and regularity of ring distribution of seismic activity before great earthquakes in China[J].Acta Seismologica Sinica(English Edition),1996,9(4):535-543.
Authors:SHI RONGMEI  ZHI PINGSONG and YAN XUE Center for Analysis and Prediction  State Seismological Bureau  Beijing  China
Institution:(1) Center for Analysis and Prediction, State Seismological Bureau, 100036 Beijing, China
Abstract:A systematic study on “ring phenomena” frequently occurring before great earthquakes has made in this paper, which has analyzed the features of ring distributions before 16 great earthquakes and part of large earthquakes in China and its boundary areas, and discussed their features of generality, regularity and predictive meaning. The results have showed that moderate earthquakes or larger earthquakes distribute around the epicenter like a ring from decades to hundred years before the great earthquakes of magnitude more than 7, which is a general phenomenon of great earthquakes without an exception. The active ring generally occurs in the areas from hundreds to thousands of kilometers from the epicenter (according to the magnitude). The seismicity in the ring has three basic stages with different features. in the first stage, seismicity remains at low level and the earthquakes distribute scatteredly, while the source area of the future great earthquake remains quiet; in the second stage, the seismicity strengthens, whose frequency, intensity, concentrated degree, released rate of strain and ratio of distributed area etc. increase, while the quiet area decreases or disappears; in the third stage, the seismicity is weaker than in the former stage, and the quiet area appears again. The source area surrounded by the active ring might have three periods of activity (called as early-term, medium-term and late-term foreshocks activity). The length of the quiet area undergoes the process from large to small, then to large. Therefore, we can estimate the occurring place, magnitude and seismogenic stage of great earthquake according to the area, length and the seismicity in the active ring, which is valuable to make a long-term prediction of great earthquakes. At last, we had a preliminary discussion on the mechanism of active ring formation.
Keywords:ring  phenomenon  strengthening area of  earthquake  activity  earthquake clusters  hard inclusion body  strong body earthquake  generating model  
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