1991: A STUDY ON THE CHARACTERISTICS OF THE INFOR- MATION DIMENSION D1 OF THE TEMPORAL AND SPATIAL DISTRIBUTIONS OF EARTHQUAKES IN AN ACTIVE FAULT ZONE. Acta Seismologica Sinica, 13(3): 372-379.
Citation: 1991: A STUDY ON THE CHARACTERISTICS OF THE INFOR- MATION DIMENSION D1 OF THE TEMPORAL AND SPATIAL DISTRIBUTIONS OF EARTHQUAKES IN AN ACTIVE FAULT ZONE. Acta Seismologica Sinica, 13(3): 372-379.

A STUDY ON THE CHARACTERISTICS OF THE INFOR- MATION DIMENSION D1 OF THE TEMPORAL AND SPATIAL DISTRIBUTIONS OF EARTHQUAKES IN AN ACTIVE FAULT ZONE

More Information
  • Published Date: September 01, 2011
  • The research of the information dimension (D1) in an active fault zone considers the contribution of each seismic event to information and reflects the charact eristics of the temporal and spatial distributions of earthquakes from a new point of view, avoiding the shortcomings of the research about the fractal dimension of capacity (D0).The results of calcu ation show that the information dimension of the temporal distribution in the Xianshuihe active fault zone before the great Luhuo earthquake is D1 =0.1051. It is a consult creterion of large earthquakes in future in the fault zone. The information dimensions lof the temporal distribution of earthquakes about 17 years in the Anninghe active fault zone are respectively D1(tN) =0.1363 (for the north section )and A(ts) =0.06710 (for the south section ). The information dimensions of the spatial distribution are respectively D1(KN) = 1.053 (for the north section )and D1( Ks) = 0.7758 (for the south section ). The north section and the south section belong respectively to two self- similar systems with different information dimensions.The extent of the self- organization of seismic activity in the south section is higher than that in the north section. This is helpful for judging the major dangerous section in the key region of the seismic monitoring. The research about the information dimension of the temporal and spatial ditributions of earthquakes is significant for the exploration of active fault zones and seismisc prediction.
  • [1] Mandelblot, B. B., 1982 .The Frartul Georrmlry of Nature, 1——376. W. H. Freeman, New York.

    [2] 姚勇, 1987.嫡、分维、李雅普诺夫指数与混沌.自然杂志, 10, 5. 359——365.

    [3] 罗久里、韩渭宾、徐叶邦、刘冬燕、彭涛, 1989.地震前兆的动力学特征——是否存在着地震前兆吸引子?大自然探索, 8, 29, 21——27.

    [4] Kaga n, Y. Y.and Knopoff.L.,1980. Spatial distribution of earthquakes:the two——point correlation funstion .Gcoplys, J. R.ast..62—— ,303——320.

    [5] Sadovskiy, M. A.. Golubeva.T. V., Pisarenko . V. F. and Shni r man , M. G., 1984 Characteristic dimenlions of rock and hierachical properties of seismicity.T. V.Acucl . Sci. USSR Phys. Solid. Earth, Engl.Traps., 20, 87——96.

    [6] Kagan, Y. Y. and Knopoff, L..1978. Statistical study of the occurence of shallow earthquakes.J. RW u.str .Sm.55, 87——96.

    [7] Kagan, Y. Y. and Knopoff, L——1981 .Stochastic synthesis of earthquake catalog.J. Genplws.Res 86 2853——286?.

    [8] Smallev, Jr——R. F, Chatelain, J. L——Turcotte, D. L. and Prevot, 8.1987. A fractal approach to the clus tering of earthquakes applications to the seismicity of the New Hebrides.Bull. Selsm . Snc ..4nu r . ,77 1368——1381

    [9] 郝柏林, 1985.分形分维.科学杂志, 38 ,1 ,9——17

    [10] 程光主编1989.分形理论及其应用.全国分形理论及应川学术讨论会文集, 94一四川大学出版社, 成都

    [11] Jens Feder.1988 .lrcurul.88 .Plcnum Press、New York

    [12] Tamas, V19H9 Frc——l Grnwllr Plmrromercr.55 .World Scientific Publishing Co .Pte. Ltd——Singapore.

    [1] Mandelblot, B. B., 1982 .The Frartul Georrmlry of Nature, 1——376. W. H. Freeman, New York.

    [2] 姚勇, 1987.嫡、分维、李雅普诺夫指数与混沌.自然杂志, 10, 5. 359——365.

    [3] 罗久里、韩渭宾、徐叶邦、刘冬燕、彭涛, 1989.地震前兆的动力学特征——是否存在着地震前兆吸引子?大自然探索, 8, 29, 21——27.

    [4] Kaga n, Y. Y.and Knopoff.L.,1980. Spatial distribution of earthquakes:the two——point correlation funstion .Gcoplys, J. R.ast..62—— ,303——320.

    [5] Sadovskiy, M. A.. Golubeva.T. V., Pisarenko . V. F. and Shni r man , M. G., 1984 Characteristic dimenlions of rock and hierachical properties of seismicity.T. V.Acucl . Sci. USSR Phys. Solid. Earth, Engl.Traps., 20, 87——96.

    [6] Kagan, Y. Y. and Knopoff, L..1978. Statistical study of the occurence of shallow earthquakes.J. RW u.str .Sm.55, 87——96.

    [7] Kagan, Y. Y. and Knopoff, L——1981 .Stochastic synthesis of earthquake catalog.J. Genplws.Res 86 2853——286?.

    [8] Smallev, Jr——R. F, Chatelain, J. L——Turcotte, D. L. and Prevot, 8.1987. A fractal approach to the clus tering of earthquakes applications to the seismicity of the New Hebrides.Bull. Selsm . Snc ..4nu r . ,77 1368——1381

    [9] 郝柏林, 1985.分形分维.科学杂志, 38 ,1 ,9——17

    [10] 程光主编1989.分形理论及其应用.全国分形理论及应川学术讨论会文集, 94一四川大学出版社, 成都

    [11] Jens Feder.1988 .lrcurul.88 .Plcnum Press、New York

    [12] Tamas, V19H9 Frc——l Grnwllr Plmrromercr.55 .World Scientific Publishing Co .Pte. Ltd——Singapore.
  • Cited by

    Periodical cited type(10)

    1. 李思妍,李桂荣,王晓飞,阿卜杜塔伊尔·亚森. 利用GPS资料分析新疆两次6级地震震前位移微动态特征. 内陆地震. 2024(03): 231-241 .
    2. 丁宇,李桂荣,朱治国,李瑞,苏力坦·玉散,李杰,刘代芹,杨磊,赵磊,孙小旭,塔依尔·喀哈尔. 新疆4次M_S≥6.0地震基线时间序列异常变化特征研究. 内陆地震. 2022(01): 33-41 .
    3. 黄帅堂,常想德,马建,胡伟华,任静,刘建明,张文秀,赖爱京. 天山北麓库松木契克山山前断裂东段断层陡坎研究. 地震地质. 2022(01): 20-34 .
    4. 郑雪刚,马学军,赵鹏毕. 新疆精河M_S6.6地震震源深度研究. 内陆地震. 2022(04): 312-319 .
    5. 张占阳,孙启凯,何亚东,张俊青,刘坤. 定量与定性分析在2017年精河M_S6.6地震中的应用. 华北地震科学. 2021(01): 64-69 .
    6. 王平川,张勇,冯万鹏. 2017年精河M_S6.6地震的断层参数和破裂过程. 地震学报. 2021(02): 137-151+135 . 本站查看
    7. 李惠玲,曹建玲,魏文薪. 新疆精河2017年6.6级地震对2018年5.4级地震的应力影响分析. 大地测量与地球动力学. 2021(12): 1253-1257+1320 .
    8. 王月,胡少乾,何骁慧,郭凯,解孟雨,邓世广,马亚伟. 2021年5月21日云南漾濞6.4级地震序列重定位及震源机制研究. 地球物理学报. 2021(12): 4510-4525 .
    9. 郭志,高星,路珍. 2019年6月17日四川长宁地震重定位及震源机制研究. 地震学报. 2020(03): 245-255+377 . 本站查看
    10. 唐明帅,王海涛,魏芸芸,李艳永,王琼,魏斌,苏金波. 利用接收函数探讨新疆几次中强地震的地壳孕育深度. 中国地震. 2020(03): 517-526 .

    Other cited types(2)

Catalog

    Article views (1189) PDF downloads (75) Cited by(12)

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return