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Hu XIAOXING, LIN BANGHUI h. 1989: STEREOSCOPIC FIGURES OF THE TIME-VARIATION IN THE SPACE DISTRIBUTION OF FOCI OF THE XINGTAI EARTHQUAKES AND THEIR OCCURRENCE PROCEDURE. Acta Seismologica Sinica, 11(1): 1-11.
Citation: Hu XIAOXING, LIN BANGHUI h. 1989: STEREOSCOPIC FIGURES OF THE TIME-VARIATION IN THE SPACE DISTRIBUTION OF FOCI OF THE XINGTAI EARTHQUAKES AND THEIR OCCURRENCE PROCEDURE. Acta Seismologica Sinica, 11(1): 1-11.
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STEREOSCOPIC FIGURES OF THE TIME-VARIATION IN THE SPACE DISTRIBUTION OF FOCI OF THE XINGTAI EARTHQUAKES AND THEIR OCCURRENCE PROCEDURE

  • Institute of Geophysics, State Scismological Bureau

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  • Published Date: September 01, 2011
    Graphical Abstract
    • Abstract
  • In this paper,the procedure of the time-variation in focal space distribution during the high seismicity period of the Xingtai earthquakes of March 1966 is studied by using seismic data obtained by the Xingtai Local Seismic Network.A series of stereoscopic figures showing the process of seismogeny and rupture of the strong shocks,adjustment of the stress field and seismo-structure are given. A further study is made of the relation between earthquakes and barriers existing in the crustal medium of the seismic region. It is this kind of non-uniform structure in the seismic area that caused the rupture of the Xingtai earthquake to be a discontinuous growing procedure expanding along the NNE direction,through which the occurrence of several earthquakes stronger than Ms 6.0 and the phenomenon of flip-flops from one and to the other of the fault of big aftershocks after the high seismicity period can be well explained.Besides,the ruptures of strong shocks bigger,than Ms 6.0 are discussed and compared with some results obtained before. And a survey is made of the relation between the variation in focal depth with time and the occurrence of big earthquake in the Xingtai region.
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    • References (1)
  • [1] 何志桐、谢挺,1977.邢台地震序列的空间分布,构造应力场及其发生过程探讨.地球物理学报,20,130——141.

    [2] 林邦慧、胡小幸、王新华、张卫平,华北地区强震前小震"密集——平静"的特征及其初步解释.地震预报论文集,地震出版社(待出版)

    [3] 刘国栋、顾群、史书林、孙洁、石障松、刘金汉,1983.京、津、唐、渤和周围地区地壳上地慢电性结构及其与地震活动性的关系.地球物理学报,26,149——157.

    [4] 滕吉文、王国正、刘道洪、邢纪润、梁文斗、徐世林,1975.华北平原中部地区深部构造背景及邢台地震(二).地球物理学报,18,196——207.

    [5] Keiiti Aki, 1984. Asperites, barriers, characteristic earthquakes and strong motion prediction. J. Geophys. Res. 89,B7, 5867——5872

    [6] 河北省地震局,1986,一九六六年邢台地震, 33——39,地震出版社.

    [7] 林邦慧、董大南、林纪曾、胡小幸,1988.用复合型法反演1962年广东河源地震及1969年广东阳江地展的破裂过程.地震学报,4, 337——356.

    [8] Wei——Ying Chung, John J. Cipar, 1983. Source modeling of the Hsingtai, China Earthquake of March 1966. Phys. Earth Planet. Int. 33, 111——125.

    [1] 何志桐、谢挺,1977.邢台地震序列的空间分布,构造应力场及其发生过程探讨.地球物理学报,20,130——141.

    [2] 林邦慧、胡小幸、王新华、张卫平,华北地区强震前小震"密集——平静"的特征及其初步解释.地震预报论文集,地震出版社(待出版)

    [3] 刘国栋、顾群、史书林、孙洁、石障松、刘金汉,1983.京、津、唐、渤和周围地区地壳上地慢电性结构及其与地震活动性的关系.地球物理学报,26,149——157.

    [4] 滕吉文、王国正、刘道洪、邢纪润、梁文斗、徐世林,1975.华北平原中部地区深部构造背景及邢台地震(二).地球物理学报,18,196——207.

    [5] Keiiti Aki, 1984. Asperites, barriers, characteristic earthquakes and strong motion prediction. J. Geophys. Res. 89,B7, 5867——5872

    [6] 河北省地震局,1986,一九六六年邢台地震, 33——39,地震出版社.

    [7] 林邦慧、董大南、林纪曾、胡小幸,1988.用复合型法反演1962年广东河源地震及1969年广东阳江地展的破裂过程.地震学报,4, 337——356.

    [8] Wei——Ying Chung, John J. Cipar, 1983. Source modeling of the Hsingtai, China Earthquake of March 1966. Phys. Earth Planet. Int. 33, 111——125.
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