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GAO XIMING, WANG WEIZHONG . 1983: ON THE CHARACTERISTICS OF THE PHASE OF SOLID TIDAL STRESS FOR DIFFERENT TYPES OF EAR- THQUAKE SEQUENCES OCCURRED IN THE CONTINENT OF CHINA. Acta Seismologica Sinica, 5(3): 323-335.
Citation: GAO XIMING, WANG WEIZHONG . 1983: ON THE CHARACTERISTICS OF THE PHASE OF SOLID TIDAL STRESS FOR DIFFERENT TYPES OF EAR- THQUAKE SEQUENCES OCCURRED IN THE CONTINENT OF CHINA. Acta Seismologica Sinica, 5(3): 323-335.
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ON THE CHARACTERISTICS OF THE PHASE OF SOLID TIDAL STRESS FOR DIFFERENT TYPES OF EAR- THQUAKE SEQUENCES OCCURRED IN THE CONTINENT OF CHINA

  • Institute of Seismology, State Seismological Bureau, Wuhan, China

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  • Published Date: August 31, 2011
    Graphical Abstract
    • Abstract
  • In this paper, the characteristics of phase distribution of solid tidal stress for 131 strong earthquake sequences occurred in the continent of China have been studied.The results obtained about the maximum tidal shear stress are as follows: there is an apparent optimal distribution of phase of the main shock for the earthquake sequence of the single-shock type and main-shock type, but the optimal phase of the main shock of the single-shock type is significantly higher than that of the main-shock type; in the earthquake sequence of the swarm-shock type, it is easily observed that some apparent clusters can be distinguished, and the phases of the sequence which consists of the main earthquake in each cluster tend to decrease orderly; the phase of late strong aftershocks of various types of earthquake sequences are also of optimal distribution.The composite characteristics of the phases of the maximum tidal shear stress and tidal hydrostatic stress of different earthquake sequences have definite physical significance, which is also an intended effect of the stress path of A type and B type loading processes in rock acoustic emission experiments in our problem.
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    • References (1)
  • [1] 高锡铭,殷志山,王威中等,固体潮应力张量对地震的触发作用,地震学报,3, 3, 1981.

    [2] K. Mogi, Study of elastic shocks caused by the fracture of heterogeneous materials and its the earthquake phenomena,, Bull. Earthq. Res. Inst, 40, 1, 1962.

    [3] K. Mogi, Rock mechanics and earthquakes (manuscript), 1978.

    [4] C. H. Scholz, The frequency——magnitude ralation of microfracture in rock and its relation to earthqua kes, B. S. S. A. 58,1,1968.

    [5] С.Д.Винограδов, К. М., Мирзоев, Н. Г. Саломов, Распредение ве времня упругих импулъсов возникающих при разрушении оδразов, цзв. АН. СССР, фцзка земпц, 4, 1975.

    [6] 中国科学院地球物理所第三研究室实验组,单轴压力下岩石破裂的初步研究,地球物理学报,19, 4, 1976.

    [7] 陈颙,声发射技术在岩石力学研究中的应用,地球物理学报,20, 4, 1977.

    [8] 耿乃光等,应力途径和破裂前兆,地震学报,2, 3, 1980.

    [9] 陈颙,不同应力途径三轴压缩下岩石的声发射,地震学报,3, 1, 1981.

    [10] 中国科学院地球物理所,地晨序列的基本类型及其在地震预报中的应用,地震战线,42, 1971.

    [11] 周惠兰,地震震型判断方法探讨,西北地震学报,2, 2, 1980.

    [12] 中央地震工作小组办公室,中国地震目录,第一、二、三、四册,科学出版社,1971.

    [13] 中国科学院地球物理所,中国地震台网观视叮报告,1967——1977年,地震出版社.

    [14] 国家地震局分析预报中心,全国地震目录,1971——1980.6.

    [15] 吴开统等,海城地震序列特征,地球物理学报,19, 2, 1976.

    [16] 李钦祖等,唐山地震的震源机制,地震地质,2, 4, 1980.

    [17] 向宏发等,1978年海城6.0级地震的构造条件分析,地晨地质,2, 2, 1980.

    [18] 卓钰如等,根据断裂力学观点推算1976年盐源地震的发震应力场,地震学报,1,1, 1979.

    [19] 李全林等,b值时空扫描,地球物理学报,21, 2, 1978.

    [20] 傅征祥,1978年5月18日海城6级地震前地震活动的某些特征,地震学报,3, 2, 1981.

    [21] 傅承义,关于地震发生的几点认识,地震战线,43, 1971.

    [22] 郭增建等,震源物理,地震出版社,1979.

    [1] 高锡铭,殷志山,王威中等,固体潮应力张量对地震的触发作用,地震学报,3, 3, 1981.

    [2] K. Mogi, Study of elastic shocks caused by the fracture of heterogeneous materials and its the earthquake phenomena,, Bull. Earthq. Res. Inst, 40, 1, 1962.

    [3] K. Mogi, Rock mechanics and earthquakes (manuscript), 1978.

    [4] C. H. Scholz, The frequency——magnitude ralation of microfracture in rock and its relation to earthqua kes, B. S. S. A. 58,1,1968.

    [5] С.Д.Винограδов, К. М., Мирзоев, Н. Г. Саломов, Распредение ве времня упругих импулъсов возникающих при разрушении оδразов, цзв. АН. СССР, фцзка земпц, 4, 1975.

    [6] 中国科学院地球物理所第三研究室实验组,单轴压力下岩石破裂的初步研究,地球物理学报,19, 4, 1976.

    [7] 陈颙,声发射技术在岩石力学研究中的应用,地球物理学报,20, 4, 1977.

    [8] 耿乃光等,应力途径和破裂前兆,地震学报,2, 3, 1980.

    [9] 陈颙,不同应力途径三轴压缩下岩石的声发射,地震学报,3, 1, 1981.

    [10] 中国科学院地球物理所,地晨序列的基本类型及其在地震预报中的应用,地震战线,42, 1971.

    [11] 周惠兰,地震震型判断方法探讨,西北地震学报,2, 2, 1980.

    [12] 中央地震工作小组办公室,中国地震目录,第一、二、三、四册,科学出版社,1971.

    [13] 中国科学院地球物理所,中国地震台网观视叮报告,1967——1977年,地震出版社.

    [14] 国家地震局分析预报中心,全国地震目录,1971——1980.6.

    [15] 吴开统等,海城地震序列特征,地球物理学报,19, 2, 1976.

    [16] 李钦祖等,唐山地震的震源机制,地震地质,2, 4, 1980.

    [17] 向宏发等,1978年海城6.0级地震的构造条件分析,地晨地质,2, 2, 1980.

    [18] 卓钰如等,根据断裂力学观点推算1976年盐源地震的发震应力场,地震学报,1,1, 1979.

    [19] 李全林等,b值时空扫描,地球物理学报,21, 2, 1978.

    [20] 傅征祥,1978年5月18日海城6级地震前地震活动的某些特征,地震学报,3, 2, 1981.

    [21] 傅承义,关于地震发生的几点认识,地震战线,43, 1971.

    [22] 郭增建等,震源物理,地震出版社,1979.
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