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Symmetropy of earthquake patterns: asymmetry and rotation in a disordered seismic source

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Języki publikacji
EN
Abstrakty
EN
We demonstrate that the idea of symmetropy can be used for quantification of earthquake patterns. The symmetropy can be considered as a measure of asymmetry. A pattern is richer in asymmetry when the symmetropy is smaller. The specific results of its applications are obtained as follows. In a discrete model of a seismic source with self-organized criticality, the spatial patterns of earthquakes during critical states and subcritical states are distinguished by the behaviour of the symmetropy: subcritical patterns show that the symmetropy is approximately a constant but this has various values during critical states. The critical patterns show asymmetric property without any asymmetric force from the outside and without asymmetric intracellular rule. We show that the emergence of asymmetric patterns is a generic feature of dynamic ruptures in our model. Such a generic asymmetry results from the model which is an inherently discrete system consisting of finite -sized cells. These cells may represent geometrical disordered fault zones. We further discuss rotational motions that generate seismic rotational waves. In micro-morphic continuum theory, such rotations are attributed to dynamic ruptures in dis-ordered systems. We note that the concept of disorder in this theory is expressed by a set of finite-sized microstructures and is consistent with the concept of disorder modelled in the present study. Thus, we suggest that the spatially asymmetric patterns of earthquakes might be related to the rotational motions, because both come from dynamic limit.
Czasopismo
Rocznik
Strony
3--14
Opis fizyczny
Twórcy
autor
autor
autor
  • The Institute of Statistical Mathematics 4-6-7, Minami Azabu, Minato-ku, Tokyo 106-8569, Japan, nanjo@ism.ac.jp
Bibliografia
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  • Moriya, T., and R. Teisseyre, 1999: "Discussion on the recording of seismic rotation waves", Acta Geophys. Pol. 47, 351-362.
  • Nagahama, H., and R. Teisseyre, 2000: "Micromorphic continuum and fractal fracturing in the lithosphere", Pure Appl. Geophys. 155, 559-574.
  • Nagahama, H., and R. Teisseyre, 2006: "From non-local to asymmetric deformation field". In: R. Teisseyre, M. Takeo and E. Majewski (eds.), Earthquake Source Asymmetry, Structural Media and Rotation Effects, Springer-Verlag (in press).
  • Nanjo, K., H. Nagahama and E. Yodogawa, 2000: "Symmetry properties of spatial distribution of microfracturing in rock", Forma 15, 95-101.
  • Nanjo, K., H. Nagahama and E. Yodogawa, 2001: "Symmetropy and self-organized criticality", Forma 16, 213-224.
  • Nanjo, K., H. Nagahama and E. Yodogawa, 2004: "Symmetry in the self-organized criticality". In: D. Nagy and G. Lugosi (eds.), Symmetry: Art and Science 2004. ISIS-Symmetry, Budapest, 302-305.
  • Nanjo, K.Z., H. Nagahama and E. Yodogawa, 2005: "Symmetropy of fault patterns: quantitative measurement of anisotropy and entropic heterogeneity", Math. Geol. 37, 277-293.
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  • Teisseyre, R., 1973: "Earthquake processes in a micromorphic continuum", Pure Appl. Geophys. 102, 15-28.
  • Teisseyre, R., 1974: "Symmetric micromorphic continuum: wave propagation, point source solution and some applications to earthquake processes". In: P. Thoft-Christensen (ed.), Continuum Mechanics Aspects of Geodynamics and Rock Fracture Mechanics, D. Reidel Pub., Boston, 201-244.
  • Twiss, R.J., G.M. Protzman and S.D. Hurst, 1991: "Theory of slikenline patterns based on the velocity gradient tensor and microrotation", Tectonophysics 186, 215-239.
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  • Walsh, J.L., 1999: "A closed set of normal orthogonal functions". In: T.J. Rivlin and E.B. Saff (eds.), Joseph L Walsh Selected Papers, Springer-Verlag, New York, 109-128.
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  • Xie, X., 2004: "Discussion on rotational tectonic stress field and the genesis of circum-Ordos landmass fault system", Acta Seismol. Sinica 17, 464-472.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0014-0029
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