single-dr.php

JDR Vol.4 No.2 pp. 111-117
(2009)
doi: 10.20965/jdr.2009.p0111

Paper:

A Model of Earthquake-Generation Cycle with Scale-Dependent Frictional Property - Preliminary Results and Research Plan for a Project of Evaluation for Coming Tokai, Tonankai, and Nankai Earthquakes

Takane Hori*, Shin’ichi Miyazaki**, and Noa Mitsui*

*Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology

**Graduate School of Science, Kyoto University

Received:
December 28, 2008
Accepted:
March 30, 2009
Published:
April 1, 2009
Keywords:
Nankai trough, earthquake cycle, time predictable, scale dependence
Abstract
To estimate rupture timing and location for coming Nankai trough earthquakes, we must know the mechanism of variation in earthquake size and recurrence time. Recurrence time varies fairly widely, and shows “time-predictable” behavior based on historical data. We propose a conceptual model for reproducing recurrence-timing variation related to earthquake size. The model includes smaller patches in a larger patch where all patches are velocity-weakening. We assume that characteristic slip distance L under the rate- and state-dependent friction law depends on patch size. We test simple two-scale heterogeneity and reproduce time-predictable behavior. Results show that slip patterns among earthquake-generation cycles vary significantly. Within a seismogenic zone, afterslip occurs during interseismic periods of giant earthquakes rupturing the entire seismogenic zone.
Cite this article as:
T. Hori, S. Miyazaki, and N. Mitsui, “A Model of Earthquake-Generation Cycle with Scale-Dependent Frictional Property - Preliminary Results and Research Plan for a Project of Evaluation for Coming Tokai, Tonankai, and Nankai Earthquakes,” J. Disaster Res., Vol.4 No.2, pp. 111-117, 2009.
Data files:
References
  1. [1] K. Ishibashi, “Status of historical seismology in Japan,” Ann. Geophys., 47, pp. 339-368, 2004.
  2. [2] K. Satake and B. F. Atwater, “Long-Term Perspectives on Giant Earthquakes and Tsunamis at Subduction Zones,” Annu. Rev. Earth Planet. Sci., 35, pp. 349-74, 2007.
  3. [3] K. Shimazaki and T. Nakata, “Time-predictable recurrence model for large earthquakes,” Geophys. Res. Lett., 7, pp. 279-282, 1980.
  4. [4] T. Hori, “Mechanisms for variation in size and occurrence interval of interplate earthquakes,” Zisin (in Japanese with English abstract), (in pres).
  5. [5] T. Hori, “Mechanisms of separation of rupture area and variation in time interval and size of great earthquakes along the Nankai Trough, southwest Japan,” J. Earth Simulator, 5, pp. 8-19, 2006.
  6. [6] S. Kodaira, T. Hori, A. Ito, S. Miura, G. Fujie, J. O. Park, T. Baba, H. Sakaguchi, and Y. Kaneda, “A cause of rupture segmentation and synchronization in the Nankai trough revealed by seismic imaging and numerical simulation,” J. Geophys. Res., 111 ,B09301, doi:10.1029/2005JB004030, 2006.
  7. [7] N. Kato, “Numerical simulation of recurrence of asperity rupture in the Sanriku region, northeastern Japan,” J. Geophys. Res., 113, B06302, doi:10.1029/2007JB005515, 2008.
  8. [8] S. Ide and G. C. Beroza, “Does apparent stress vary with earthquake size?”, Geophys. Res. Lett., 28, pp. 3349-3352, 2001.
  9. [9] N. Kato, “Repeating slip events at a circular asperity: Numerical simulation with a rate- and state-dependent friction law,” Bull. Earthquake Res. Inst. Univ. Tokyo, 78, pp. 151-166, 2003.
  10. [10] C. H. Scholz, “Earthquakes and friction laws,” Nature, 391, pp. 37-42, 1998.
  11. [11] A. Bizzarri and M. Cocco, “Slip-weakening behavior during the propagation of dynamic ruptures obeying rate- and state-dependent friction laws,” J. Geophys. Res., 108, 2373, doi:10.1029/2002JB002198, 2003.
  12. [12] M. Matsu’ura, H. Kataoka, and B. Shibazaki, “Slip-dependent friction law and nucleation processes in earthquake rupture,” Tectonophysics, 211, pp. 135-148, 1992.
  13. [13] S. Ide and H. Aochi, “Earthquakes as multiscale dynamic rupture with heterogeneous fracture surface energy,” Journal of Geophysical Research, 110, B11303, doi:10.1029/2004JB003591, 2005.
  14. [14] M. Ohnaka and L. F. Shen, “Scaling of the Shear Rupture Process from Nucleation to Dynamic Propagation: Implications of Geometric Irregularity of the Rupturing Surfaces,” J. Geophys. Res. 104, pp. 817-844, 1999.
  15. [15] B. Shibazaki and M. Matsu’ura, “Transition process from nucleation to high-speed rupture propagation: scaling from stick-slip experiments to natural earthquakes,” Geophys. J. Int., 132, pp. 14-30, 1998.
  16. [16] J. R. Rice, “Spatio-temporal complexity of slip on a fault,” J. Geophys. Res., 98, pp. 9885-9907, 1993.
  17. [17] M. Nakatani, “Conceptual and physical clarification of rate and state friction: Frictional sliding as a thermally activated rheology,” J. Geophys. Res., 106, pp. 13,347-13,380, 2001.
  18. [18] M. Comninou and J. Dundurs, “Angular dislocation in a half space,” J. Elasticity, 5, pp. 203-216, 1975.
  19. [19] N. Kato and T. E. Tullis, “A composite rate- and state-dependent law for rock friction,” Geophys. Res. Lett., 28, pp. 1103-1106, 2001.
  20. [20] W. H. Press, S. A. Teukolsky, W. T. Vetterling, and B. P. Flannery, “Numerical Recipies in Fortran 77: The Art of Scientific Computing, 2nd Edition,” Cambridge University Press, 1996.
  21. [21] M. L. Blanpied, C. J. Marone, D. A. Lockner, J. D. Byerlee, and D. P. King, “Quantitative measure of the variation in fault rheology due to fluid-rock interaction,” J. Geophys. Res., 103, pp. 9691-9712, 1998.
  22. [22] G. Hillers, Y. Ben-Zion, and P. M. Mai, “Seismicity on a fault controlled by rate- and state-dependent friction with spatial variations of the critical slip distance,” J. Geophys. Res., 111, B01403, doi:10.1029/2005JB003859, 2006.
  23. [23] M. Nakatani and C. H. Scholz, “Frictional healing of quartz gouge under hydrothermal conditions: 1. Experimental evidence for solution transfer healing mechanism,” J. Geophys. Res., 109, B07201, doi:10.1029/2001JB001522, 2004.
  24. [24] T. Hori and S. Miyazaki, “Various Slip Pattern in Earthquake Generation Cycles Modeled with Heterogeneous Fracture Surface Energy Distribution,” SE82-A030, AOGS 5th Ann. General Meeting, 2008.
  25. [25] F. Nanayama, K. Satake, R. Furukawa, K. Shimokawa, and B. F. Atwater, et al., “Unusually large earthquakes inferred from tsunami deposits along the Kuril trench,” Nature, 424, pp. 660-663, 2003.
  26. [26] S. Nishimura, M. Ando, and S. Miyazaki, “Inter-plate coupling along the Nankai trough and southeastward motion along southern part of Kyushu,” Zishin, 51, pp. 443-456, 1999.
  27. [27] Headquarters for Earthquake Research Promotion, “Long-term evaluation of seismicity off Hyuga and Southwestern Islands areas along Ryukyu trench,” 2004.
  28. [28] Y. Yagi, M. Kikuchi, and T. Sagiya, “Co-seismic slip, post-seismic slip, and aftershocks associated with two large earthquakes in 1996 in Hyuga-nada, Japan,” Earth, Planets and Space, 53, pp. 793-803, 2001.
  29. [29] P. Wessel and W. H. F. Smith, “New version of the generic mapping tools (GMT) version 3.0 released,” EOS Trans. AGU, 76, p. 329, 1995.

*This site is desgined based on HTML5 and CSS3 for modern browsers, e.g. Chrome, Firefox, Safari, Edge, Opera.

Last updated on Apr. 22, 2024