Xiuiang Ma, Liping Fu. 1991: STATISTICAL TESTING OF THE RELATION BETWEEN BURST OF AFTERSHOCKS AND STRONG EARTHQUAKE. Acta Seismologica Sinica, 13(3): 273-280.
Citation: Xiuiang Ma, Liping Fu. 1991: STATISTICAL TESTING OF THE RELATION BETWEEN BURST OF AFTERSHOCKS AND STRONG EARTHQUAKE. Acta Seismologica Sinica, 13(3): 273-280.

STATISTICAL TESTING OF THE RELATION BETWEEN BURST OF AFTERSHOCKS AND STRONG EARTHQUAKE

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  • Published Date: September 01, 2011
  • According to geological tectonics and seismic activites this paper devided North China ( 30- 45N, 105 - 130E) into four areas. We analized the Nouth China earthquake catalogue from 1970 to 1986 (from 1965 to 1986 for Hua Bei, the North China, plain region) and identified forty- two bursts of aftershock. Seven of them occurred in aftershock regions of strong earthquakes and seventeen of them in the seismic swarm regions. The relation between strong earthquakes with the remaining eighteen bursts of aftershocks has been studied and tested statistically in this paper. The result of statistical testing show that the random probability p of coincidence of bursts of aftershock with subsqeuent strong earthquakes is less than six percent. By Xu's R scoring method the efficacy of predicating strong earthquake from bursts of aftershock is estimated qreater than 39 percent.Following the method proposed in the paper we analyzed the earhtquake catalogue of China from 1987 to 1988-6 The results show that there was only one brust of aftershock occurred on Jan. 6,1988 with M=3.6 in Xiuyan of Northeast China. It implicates that a potential earthquake with Ms 5 might occur in one year afterwards in the region of Northeast China. Actually on Feb.25,1988 an earthquate with Ms= 5.3 occurred in Zhangwu of Northeast China. Another example is Datong-Yanggao shock on October -18, 1989 which is a burst of aftershock. Three hours after an expected shock with M=6.l took place in the same area. Two examples above have been tested in practical predication and this shows that bursts of aftershock are significant in predicating strong earthquakes.
  • [1] Keilis——Borok,V. 1. and Konopotl: L——1980. Bursts of aftershock of strong earthquakes. Nuture,283. 5744. 259——263.

    [2] Caputo. M. R. . Console,A. M——Gabrielov, Keilis——Borok. V. I——and Sidorenko. T. V.1983. Long——term premonitory seismicity patterns in Italy. Goophrs. J. R. u.str. 50——75. 7l——75

    [3] 石绍先,1981.爆发型余震可能是强震的前兆.地震研究、4 , 2 85——289.

    [4] 陈锦标、陈佩燕、李全林、王克祥、吴春珍、李伯民,1987.中国地震数据库.地震学报,9, 326——334.

    [5] Keilis——Borok, V. I. and Kossobokov, V. G——1986 Time of increased probability for the great earthquakes of the world. Ru Corrutcttirn:ul Se i.srrnrlo, 1, 19, 48——58

    [6] 国家地震局分析预报中心编,1983.中国东部地震目录(M).地震出版社,北京.

    [7] 林少宫、1964.墓础概率与数理统计,25——32.人民教育出版社,北京.

    [8] 中国科学院地球物理研究所,1973.震兆分析一例.地震、2: 78——82.

    [9] Kanamori. H——1972. Relation between tectonic stress great eathquakes and eatthquake swarms. Tcotnnophvsics, 14, 1——12

    [10] 马杏垣主编、1987.中国岩石圈动力学纲要,中国及邻近海域岩石圈动力学图集.地质出版社,北京.

    [1] Keilis——Borok,V. 1. and Konopotl: L——1980. Bursts of aftershock of strong earthquakes. Nuture,283. 5744. 259——263.

    [2] Caputo. M. R. . Console,A. M——Gabrielov, Keilis——Borok. V. I——and Sidorenko. T. V.1983. Long——term premonitory seismicity patterns in Italy. Goophrs. J. R. u.str. 50——75. 7l——75

    [3] 石绍先,1981.爆发型余震可能是强震的前兆.地震研究、4 , 2 85——289.

    [4] 陈锦标、陈佩燕、李全林、王克祥、吴春珍、李伯民,1987.中国地震数据库.地震学报,9, 326——334.

    [5] Keilis——Borok, V. I. and Kossobokov, V. G——1986 Time of increased probability for the great earthquakes of the world. Ru Corrutcttirn:ul Se i.srrnrlo, 1, 19, 48——58

    [6] 国家地震局分析预报中心编,1983.中国东部地震目录(M).地震出版社,北京.

    [7] 林少宫、1964.墓础概率与数理统计,25——32.人民教育出版社,北京.

    [8] 中国科学院地球物理研究所,1973.震兆分析一例.地震、2: 78——82.

    [9] Kanamori. H——1972. Relation between tectonic stress great eathquakes and eatthquake swarms. Tcotnnophvsics, 14, 1——12

    [10] 马杏垣主编、1987.中国岩石圈动力学纲要,中国及邻近海域岩石圈动力学图集.地质出版社,北京.

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