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Common dependence on stress for the two fundamental laws of statistical seismology

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Abstract

Two of the long-standing relationships of statistical seismology are power laws: the Gutenberg–Richter relation1 describing the earthquake frequency–magnitude distribution, and the Omori–Utsu law2 characterizing the temporal decay of aftershock rate following a main shock. Recently, the effect of stress on the slope (the b value) of the earthquake frequency–magnitude distribution was determined3 by investigations of the faulting-style dependence of the b value. In a similar manner, we study here aftershock sequences according to the faulting style of their main shocks. We show that the time delay before the onset of the power-law aftershock decay rate (the c value) is on average shorter for thrust main shocks than for normal fault earthquakes, taking intermediate values for strike-slip events. These similar dependences on the faulting style indicate that both of the fundamental power laws are governed by the state of stress. Focal mechanisms are known for only 2 per cent of aftershocks. Therefore, c and b values are independent estimates and can be used as new tools to infer the stress field, which remains difficult to measure directly.

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Figure 1: Influence of faulting style on the time delay before the onset of the power-law aftershock decay rate in southern California.
Figure 2: Influence of faulting style on the time delay before the onset of the power-law aftershock decay rate in Japan.

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References

  1. Gutenberg, B. & Richter, C. F. Frequency of earthquakes in California. Bull. Seismol. Soc. Am. 34, 185–188 (1944)

    Google Scholar 

  2. Utsu, T. Aftershocks and earthquake statistics. J. Fac. Sci. Hokkaido Univ. Ser. VII 3, 379–441 (1965)

    Google Scholar 

  3. Schorlemmer, D., Wiemer, S. & Wyss, M. Variations in earthquake-size distribution across different stress regimes. Nature 437, 539–542 (2005)

    Article  CAS  ADS  Google Scholar 

  4. Narteau, C., Shebalin, P. & Holschneider, M. Temporal limits of the power law aftershock decay rate. J. Geophys. Res. 107 B2359 10.1029/2002JB001868 (2002)

    Article  ADS  Google Scholar 

  5. Shcherbakov, R., Turcotte, D. L. & Rundle, J. B. A generalized Omori's law for earthquake aftershock decay. Geophys. Res. Lett. 31 L11613 10.1029/2004GL019808 (2004)

    Article  ADS  Google Scholar 

  6. Vidale, J. E., Peng, Z. & Ishii, M. Anomalous aftershock decay rates in the first hundred seconds revealed from the Hi-net borehole data. Eos Trans. AGU 85 (Fall Meet. Suppl.), abstr. S23C-07 (2004)

  7. Peng, Z. G., Vidale, J. E., Ishii, M. & Helmstetter, A. Seismicity rate immediately before and after main shock rupture from high frequency waveforms in Japan. J. Geophys. Res. 112 B03306 10.1029/2006JB004386 (2007)

    Article  ADS  Google Scholar 

  8. Enescu, B., Mori, J. & Miyasawa, M. Quantifying early aftershock activity of the 2004 mid-Niigata Prefecture earthquake (Mw6.6). J. Geophys. Res. 112, B04310, 10.1029/2006JB004629 (2007)

    Article  ADS  Google Scholar 

  9. Nanjo, K. Z. et al. Decay of aftershock activity for Japanese earthquakes. J. Geophys. Res. 112 B08309 10.1029/2006JB004754 (2007)

    Article  ADS  Google Scholar 

  10. Kilb, D., Martynov, V. & Vernon, F. Aftershock detection as a function of time: results from the ANZA seismic network following the 31 October 2001 M L 5.1 Anza, California, earthquake. Bull. Seismol. Soc. Am. 97, 780–792 (2007)

    Article  Google Scholar 

  11. Kagan, Y. Y. Short-term properties of earthquake catalogs and models of earthquake source. Bull. Seismol. Soc. Am. 94, 1207–1228 (2004)

    Article  Google Scholar 

  12. Lolli, B. & Gasperini, P. Comparing different models of aftershock rate decay: the role of catalog incompleteness in the first times after main shock. Tectonophysics 423, 43–59 (2006)

    Article  ADS  Google Scholar 

  13. Peng, Z. G., Vidale, J. E. & Houston, H. Anomalous early aftershock decay rate of the 2004 M w 6.0 Parkfield, California, earthquake. Geophys. Res. Lett. 33 10.1029/2006GL026744 (2006)

  14. Hauksson, E. Crustal structure and seismicity distribution adjacent to the Pacific and North America plate boundary in southern California. J. Geophys. Res. 105, 13875–13903 (2000)

    Article  ADS  Google Scholar 

  15. Gardner, J. & Knopoff, L. Is the sequence of earthquakes in southern California with aftershocks removed Poissonian? Bull. Seismol. Soc. Am. 5, 1363–1367 (1974)

    Google Scholar 

  16. Reasenberg, P. Second-order moment of central California seismicity, 1969–1982. J. Geophys. Res. 90, 5479–5495 (1985)

    Article  ADS  Google Scholar 

  17. Schorlemmer, D. & Woessner, J. Probability of detecting an earthquake. Bull. Seismol. Soc. Am. 98, 2103–2117 (2008)

    Article  Google Scholar 

  18. Wiemer, S. & Wyss, M. Minimum magnitude of completeness in earthquake catalogs: examples from Alaska, the western United States, and Japan. Bull. Seismol. Soc. Am. 90, 859–869 (2000)

    Article  Google Scholar 

  19. Sibson, R. H. Frictional constraints on thrusts, wrench and normal faults. Nature 249, 542–544 (1974)

    Article  ADS  Google Scholar 

  20. Dieterich, J. A constitutive law for rate of earthquake production and its application to earthquake clustering. J. Geophys. Res. 99, 2601–2618 (1994)

    Article  ADS  Google Scholar 

  21. Scholz, C. Microfractures, aftershocks, and seismicity. Bull. Seismol. Soc. Am. 58, 1117–1130 (1968)

    Google Scholar 

  22. Shcherbakov, R. & Turcotte, D. L. A damage mechanics model for aftershocks. Pure Appl. Geophys. 161, 2379–2391 (2004)

    Article  ADS  Google Scholar 

  23. Ben-Zion, Y. & Lyakhovsky, V. Analysis of aftershocks in a lithospheric model with seismogenic zone governed by damage rheology. Geophys. J. Int. 165, 197–210 (2006)

    Article  ADS  Google Scholar 

  24. Atkinson, B. K. Subcritical crack growth in geological materials. J. Geophys. Res. 89, 4077–4114 (1984)

    Article  CAS  ADS  Google Scholar 

  25. Amitrano, D. Brittle-ductile transition and associated seismicity: experimental and numerical studies and relationship with the b-value. J. Geophys. Res. B 108 2044 10.1029/2001JB000680 (2003)

    Article  ADS  Google Scholar 

  26. O'Connell, D. R. H., Ma, S. & Archuleta, R. J. Influence of dip and velocity heterogeneity on reverse- and normal-faulting rupture dynamics and near-fault ground motions. Bull. Seismol. Soc. Am. 97, 1970–1989 (2007)

    Article  Google Scholar 

  27. Narteau, C., Shebalin, P. & Holschneider, M. Loading rates in California inferred from aftershocks. Nonlin. Process. Geophys. 15, 245–263 (2008)

    Article  ADS  Google Scholar 

  28. Schorlemmer, D. & Wiemer, S. Microseismicity data forecast rupture area. Nature 434, 1086 (2005)

    Article  CAS  ADS  Google Scholar 

  29. Wells, D. L. & Coppersmith, K. J. New empirical relationships among magnitude, rupture length, rupture width, rupture area and surface displacement. Bull. Seismol. Soc. Am. 84, 974–1002 (1994)

    Google Scholar 

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Correspondence to Clément Narteau.

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Narteau, C., Byrdina, S., Shebalin, P. et al. Common dependence on stress for the two fundamental laws of statistical seismology . Nature 462, 642–645 (2009). https://doi.org/10.1038/nature08553

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