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Random fluctuations of the apparent stress among heterogeneous seismic sources

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The apparent stress, (tau)a, defined as the ration of seismic energy, Es, and seismic moment, M0, has been formulated as the average stress associated with radiation resistance of a sliding fault during as earthquake. The over damped dynamics approximation of a seismic source implies that the seismic energy rate at a given time is proportional to the square of the slip velocity integrates over the rupture area. This result allows us to interpret the apparent stress as a correlation integral of the slip velocity field over space and time. Consequently, other macroscopic parameters, such as momentary and local apparent stress, (tau)m and (tau)l, are proposed to characterize spatial and temporal heterogeneity of complex seismic sources. This approach is used to understand fluctuations of the apparent stress, and other macroscopic parameters in earthquake populations, in terms of their microscopic representation.
Rocznik
Strony
23--36
Opis fizyczny
Bibliogr. 16 poz.
Twórcy
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa, Poland
Bibliografia
  • 1. Abercrombie, R.E., 1995, Earthquake source scaling relationships from -1 to 5 ML using seismograms recorded al 2.5-km depth, J. Geophys. Res. 100, 24015-24036.
  • 2. Achenbach, J.D., 1984, Wave Propagation in Elastic Solids, EIsevier, Amsterdam.
  • 3. Beck, C., and F. Schlögl, 1993, Thermodynamics of Chaotic Systems: an Introduction, Cambridge University Press, Cambridge.
  • 4. Choy, L.G., and J.L. Boatwright, 1995, Global patterns of radiated seismic energy and apparent stress, J. Geophys. Res. 100, 18205-18228.
  • 5. Gibowicz, S.J., 2001, Radiated energy for seismic events induced by mining, Acta Geophys. Pol. 49,95-111.
  • 6. Ide, S., and G.C. Beroza, 2001, Does apparent stress vary with earthquake size? Geophys. Res. Lett. 28, 4000-4000.
  • 7. Izutani, Y., and H. Kanamori, 2001, Scale dependence of seismic energy-to-moment ratio for strike-slip earthquakes in Japan, Geophys. Res. Let. 28, 4007-4010.
  • 8. Kanamori, H., J. Mori, E. Hauksson, T.H. Heaton, L.K. Hutton and M.L. Jones, 1993, Determination of earthquake energy release and ML using terrascope, Bull. Seism. Soc. " Am. 81, 330-346.
  • 9. McGarr, A., and J.B. Fletcher, 2001, A method for mapping apparent stress and energy radiation applied to the 1994 Northridge earthquake faull zone-revisited, Geophys. Res. Lett. 28, 3529-3532.
  • 10. Savage, J.C., and M.D. Wood, 1971, The relation between apparent stress and stress drop, Bull. Seism. Soc. Am. 61,1381-1388.
  • 11. Senatorski, P., 1994, Spatio-temporal evolution of faults: deterministic model, Physica D76, 420-435.
  • 12. Senatorski, P., 2001, Slip-weakening and energy-moment scaling relationship, Acta Geophys. Pol. 49, 75-93.
  • 13. Senatorski, P., 2002a, Slip-weakening and interactive dynamics of an heterogeneous seismic source, Tectonophysics 344,37-60.
  • 14. Senatorski, P., 2002b, Scaling and statistical trends of the apparent stress among heterogeneous seismic sources (submitted to Acta Geophys. Pol.).
  • 15. Wald, D.J., and T.H. Heaton, 1994, Spatial and temporal distribution of slip for the 1992 Landers, California, earthquake, Bull. Seism. Soc. Am. 84, 668-691.
  • 16. Wyss, M., and J.N. Brune, 1968, Seismic moment, stress, and source dimensions for eartquakes in the California-Nevada region, J. Geophys. Res. 73,4681-4694.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0007-0025
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