Jiancheng Leiup, Zhenliang Shiup2, Jiaquan Yanup2loans.com sh advanceaunch a career 2. 1991: THE RESEARCH ON DETERMINING THE ANNUAL OCCURRENCE RATES OF POTENTIAL SEISMIC SOURCE AREAS. Acta Seismologica Sinica, 13(4): 496-504.
Citation: Jiancheng Leiup, Zhenliang Shiup2, Jiaquan Yanup2loans.com sh advanceaunch a career 2. 1991: THE RESEARCH ON DETERMINING THE ANNUAL OCCURRENCE RATES OF POTENTIAL SEISMIC SOURCE AREAS. Acta Seismologica Sinica, 13(4): 496-504.

THE RESEARCH ON DETERMINING THE ANNUAL OCCURRENCE RATES OF POTENTIAL SEISMIC SOURCE AREAS

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  • Published Date: September 01, 2011
  • To actually reflect the seismic temporal-spatial inhomogeneity of intracontinental strong earthquakes of North China in seismic hazard analysis, several seismological and geological characteristics have been selected and quantized to describe the seismicity features in time and space of every magnitude interval with the thought of dividing the interesting magnitude range into several intervals and using of the spatial probability distribution function. A component analysis method with orthogonal transformation is introduced to avoid the repeated use of the same element and the subjective effects in determining the annual occurrence rates. By passing synthetic fuzzy judgement on the nonintercorrelated new characteristics, the annual occurrence rates of every magnitude interval of each potential source area are obtained associated with the adjustments of earthquake reducing process after the occurrence of M>7 quake. An intensity map of the Beijing-Tianjin-Tangshan-Zhangjiakou area is calculated as an example which shows a close coincidence with the seismic temporal-spatial inhomogeneity of North China.
  • [1] 高孟潭,1988.关于地震年平均发生率问题的讨论.国际地震动态.1: 1——5.

    [2] Cornel C. A. , 1968, Engineering seismic risk analysis. Bull. Seism. Soc. Arrrer. 58, 5, 1583——1606.

    [3] Kiureghian, A. H——S Ang, 1977, A fault——rupture model for seismic risk analysis. Bull. Seism. Soc. Amer.,67, 4.1173——1194.

    [4] 余金生、李裕伟,1985.地质因子分析.地质出版社,北京.21——23.

    [5] 汪培庄,1983.模糊集合论及其应用.上海科技出版社,上海.105——109

    [6] 冯德益、楼世博,1985.模糊数学方法与应用.地震出版社,北京.73——76

    [7] 黄克中、毛善培,1987.随机方法与模糊数学及应用.同济大学出版社,上海.313——315.

    [8] 方仲景,1988.华北最新剪切构造网络与地震区划.华北地震科学,32. 1——8.

    [9] 郑建中,1983.中国地震的发震方式、时间间隔及概率分布.地震研究,6,增刊,433——447

    [10] 章淮鲁,1989.华北地区强震的背景地震活动性的研究.地震学报,11. 225——235.

    [1] 高孟潭,1988.关于地震年平均发生率问题的讨论.国际地震动态.1: 1——5.

    [2] Cornel C. A. , 1968, Engineering seismic risk analysis. Bull. Seism. Soc. Arrrer. 58, 5, 1583——1606.

    [3] Kiureghian, A. H——S Ang, 1977, A fault——rupture model for seismic risk analysis. Bull. Seism. Soc. Amer.,67, 4.1173——1194.

    [4] 余金生、李裕伟,1985.地质因子分析.地质出版社,北京.21——23.

    [5] 汪培庄,1983.模糊集合论及其应用.上海科技出版社,上海.105——109

    [6] 冯德益、楼世博,1985.模糊数学方法与应用.地震出版社,北京.73——76

    [7] 黄克中、毛善培,1987.随机方法与模糊数学及应用.同济大学出版社,上海.313——315.

    [8] 方仲景,1988.华北最新剪切构造网络与地震区划.华北地震科学,32. 1——8.

    [9] 郑建中,1983.中国地震的发震方式、时间间隔及概率分布.地震研究,6,增刊,433——447

    [10] 章淮鲁,1989.华北地区强震的背景地震活动性的研究.地震学报,11. 225——235.
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