HAN WEIBIN, XI DUNLI=. 1984: TEMPORAL AND SPATIAL CHARACTERISTICS OF SEISMIC GAPS FORMED BY WEAK EARTHQUAKES BEFORE STRONG EARTHQUAKES IN SICHUAN PROVINCE. Acta Seismologica Sinica, 6(1): 8-21.
Citation: HAN WEIBIN, XI DUNLI=. 1984: TEMPORAL AND SPATIAL CHARACTERISTICS OF SEISMIC GAPS FORMED BY WEAK EARTHQUAKES BEFORE STRONG EARTHQUAKES IN SICHUAN PROVINCE. Acta Seismologica Sinica, 6(1): 8-21.

TEMPORAL AND SPATIAL CHARACTERISTICS OF SEISMIC GAPS FORMED BY WEAK EARTHQUAKES BEFORE STRONG EARTHQUAKES IN SICHUAN PROVINCE

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  • Published Date: August 31, 2011
  • This work is based on the earthquake catalog prepared by the Sichuan seismological network, with reference to some earthquake catalogs of the neighbouring provinces. The earthquakes with magnitude greater than 5 that occurred during the,period from June 1970 to October 1981 are divided into 20 groups, 5 of which are excluded due to the lack of enough data. For the remaining 15 groups plots of R-t (radial distance with time) or D-t (distance along a belt with time) are made to show seismic gaps with time. Also, epicenter distribution maps are drawn to show seismic gaps in space. Through comparative analysis, it is found that in each of the 6 groups of earthquakes with maximum magnitude greater than 6 and in each of the 4 groups of'earthquakes with maximum magnitude between 5 and 6, a seismic gap appeared around the epicenter of the impending strong earthquake. According to the process of development of the seismic gaps, they may be divided into two categories: expanding and then, contracting and gradually expanding. The location and shape of the spatial gags are usually related to the regional tectonics. For the other 5 of the 15 groups also with maximum magnitudes between 5 and 6, seismic gaps did not appear. The reason may be either that earthquakes occurred incessantly in the impending epicentral area or there are too few weak earthquakes in the epicentral area and its vicinity before the main shocks.From the data of the groups of earthquakes associated with seismic gaps three empirical formulas connecting the seismic gap parameters with the magnitudes of the impending earthquakes are obtained. They are M=5.50 lg Rmax-2.331.32 M=2.98 lgT+2.941.06 M=2.52lg(RmaxT)-0.510.96 These relations are compared with that obtained by M. Ohtake. It seems that the asperity model proposed by H. Kanamori could be used to explainthe difference in the behaviour of the seismic gaps by assigning proper parameters to hismodel for different cases.
  • [1] Mogi(茂木清夫),Two Kinds of Seismic Gaps,, Pageoph, 117, Birkhavser Verlag, Basel, 1979.

    [2] 魏光兴等,华北地区大地震前地震的围空区特证,地球物理学报,21, 3, 213——217, 1918,

    [3] 陆远忠等,地震空区与"逼近地震",地震学报,4, 4, 327——336, 1982,

    [4] 韩渭宾、夏大德、松潘、平武7.2级地震和川青块体的运动,地震科学研究,年第一辑,39——47, 1980,

    [5] 韩渭宾、黄圣睦,鲜水河断裂带上的一个地震活动空区,地震学报,5, 3, 280——286, 1983.

    [6] 中国科学院数学研究所概率统计室,常用数理统计表,科学出版社,1974,

    [7] 大竹政和,地震予报中第二种空区现象的意义,日本地震学会,1979年秋季讲演予稿集(B26),

    [8] 金森博雄,地震活动和地震预报一一南加利福尼亚的例子,卢振恒译,国外地震,9, 11——19, 1981,

    [1] Mogi(茂木清夫),Two Kinds of Seismic Gaps,, Pageoph, 117, Birkhavser Verlag, Basel, 1979.

    [2] 魏光兴等,华北地区大地震前地震的围空区特证,地球物理学报,21, 3, 213——217, 1918,

    [3] 陆远忠等,地震空区与"逼近地震",地震学报,4, 4, 327——336, 1982,

    [4] 韩渭宾、夏大德、松潘、平武7.2级地震和川青块体的运动,地震科学研究,年第一辑,39——47, 1980,

    [5] 韩渭宾、黄圣睦,鲜水河断裂带上的一个地震活动空区,地震学报,5, 3, 280——286, 1983.

    [6] 中国科学院数学研究所概率统计室,常用数理统计表,科学出版社,1974,

    [7] 大竹政和,地震予报中第二种空区现象的意义,日本地震学会,1979年秋季讲演予稿集(B26),

    [8] 金森博雄,地震活动和地震预报一一南加利福尼亚的例子,卢振恒译,国外地震,9, 11——19, 1981,
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