PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Statistical properties of aftershock rate decay: Implications for the assessment of continuing activity

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Aftershock rates seem to follow a power law decay, but the assessment of the aftershock frequency immediately after an earthquake, as well as during the evolution of a seismic excitation remains a demand for the imminent seismic hazard. The purpose of this work is to study the temporal distribution of triggered earthquakes in short time scales following a strong event, and thus a multiple seismic sequence was chosen for this purpose. Statistical models are applied to the 1981 Corinth Gulf sequence, comprising three strong (M = 6.7, M = 6.5, and M = 6.3) events between 24 February and 4 March. The non-homogeneous Poisson process outperforms the simple Poisson process in order to model the aftershock sequence, whereas the Weibull process is more appropriate to capture the features of the short-term behavior, but not the most proper for describing the seismicity in long term. The aftershock data defines a smooth curve of the declining rate and a long-tail theoretical model is more appropriate to fit the data than a rapidly declining exponential function, as supported by the quantitative results derived from the survival function. An autoregressive model is also applied to the seismic sequence, shedding more light on the stationarity of the time series.
Słowa kluczowe
Czasopismo
Rocznik
Strony
748--769
Opis fizyczny
Bibliogr. 26 poz.
Twórcy
autor
  • Geophysics Department, Aristotle University of Thessaloniki, Thessaloniki, Greece, aadama@geo.auth.gr
Bibliografia
  • Daley, D.J., and D. Vere-Jones (2003), An Introduction to the Theory of Point Processes, Vol. 1, Elementary Theory and Methods, 2nd ed., Springer, New York, 469 pp.
  • Felzer, K.R., R.E. Abercrombie, and E.E. Brodsky (2003), Testing the stress shadow hypothesis, Eos Trans. AGU 84, 46, Abstract S31A-04.
  • Felzer, K.R., R.E. Abercrombie, and G. Ekström (2004), A common origin for aftershocks, foreshocks, and multiplets, Bull. Seismol. Soc. Am. 94, 1, 88-98.
  • Gardner, J.K., and L. Knopoff (1974), Is the sequence of earthquakes in Southern California, with aftershocks removed, Poissonian?, Bull. Seismol. Soc. Am. 64, 5, 1363-1367.
  • Gomberg, J., P.A. Reasenberg, P. Bodin, and R.A. Harris (2001), Earthquake triggering by seismic waves following the Landers and Hector Mine earthquakes, Nature 411, 462-466.
  • Karakostas, V. (2009), Seismicity patterns before strong earthquakes in Greece, Acta Geophys. 57, 2, 367-386.
  • Kilb, D., J. Gomberg, and P. Bodin (2000), Triggering of earthquake aftershocks by dynamic stresses, Nature 408, 570-574.
  • Lomnitz, C. (1966), Magnitude stability in earthquake sequences, Bull. Seismol. Soc. Am. 56, 1, 247-249.
  • Marsan, D. (2003), Triggering of seismicity at short timescales following Californian earthquakes, J. Geophys. Res. 108, B5, 2266.
  • Marsan, D., and S.S. Nalbant (2005), Methods for measuring seismicity rate changes: A review and a study of how the Mw 7.3 Landers earthquake affected the aftershock sequence of the Mw 6.1 Joshua Tree earthquake, Pure Appl. Geophys. 162, 6-7, 1151-1185.
  • Matsu’ura, R.S. (1986), Precursory quiescence and recovery of aftershock activities before some large aftershocks, Bull. Earthq. Res. Inst. Univ. Tokyo 61, 1-65.
  • Matthews, M.V., and P.A. Reasenberg (1988), Statistical methods for investigating quiescence and other temporal seismicity patterns, Pure Appl. Geophys. 126, 2-4, 357-372.
  • Ogata, Y. (1999), Seismicity analysis through point-process modeling: A review, Pure Appl. Geophys. 155, 2-4, 471-507.
  • Ogata, Y. (2001), Increased probability of large earthquakes near aftershock regions with relative quiescence, J. Geophys. Res. 106, B5, 8729-8744.
  • Ogata, Y. (2005a), Detection of anomalous seismicity as a stress change sensor, J. Geophys. Res. 110, B05S06.
  • Ogata, Y. (2005b), Synchronous seismicity changes in and around the northern Japan preceding the 2003 Tokachi-oki earthquake of M8.0, J. Geophys. Res. 110, B08305.
  • Ogata, Y., and K. Shimazaki (1984), Transition from aftershock to normal activity: The 1965 Rat Islands earthquake aftershock sequence, Bull. Seismol. Soc. Am. 74, 5, 1757-1765.
  • Reasenberg, P. (1985), Second-order moment of central California seismicity, 1969-1982, J. Geophys. Res. 90, 5479-5495.
  • Shaw, B.E. (1993), Generalized Omori law for aftershocks and foreshocks from a simple dynamics, Geophys. Res. Lett. 20, 10, 907-910.
  • Toda, S., R.S. Stein, P.A. Reasenberg, J.H. Dieterich, and A. Yoshida (1998), Stress transferred by the 1995 Mw = 6.9 Kobe, Japan, shock: Effect on aftershocks and future earthquake probabilities, J. Geophys. Res. 103, B10, 24543-24565.
  • Toda, S., R.S. Stein, and T. Sagiya (2002), Evidence from the AD 2000 Izu Island earthquake swarm that stressing rate governs seismicity, Nature 419, 58-61.
  • Utsu, T. (1970), Aftershocks and earthquake statistics (II): Further investigation of aftershocks and other earthquake sequences based on a new classification of earthquake sequences, J. Fac. Sci. Hokkaido Univ., Ser. VII 3, 4, 197-266.
  • Vere-Jones, D. (1992), Statistical methods for the description and display of earthquake catalogs. In: A. Walden and P. Guttorp (eds.), Statistics in the Environmental and Earth Sciences, Edward Arnold Publisher, London, 220-246.
  • Woessner, J., E. Hauksson, S. Wiemer, and S. Neukomm (2004), The 1997 Kagoshima (Japan) earthquake doublet: A quantitative analysis of aftershock rate changes, Geophys. Res. Lett. 31, L03605.
  • Wyss, M., and Y. Toya (2000), Is background seismicity produced at a stationary Poissonian rate?, Bull. Seismol. Soc. Am. 90, 5, 1174-1187.
  • Wyss, M., and S. Wiemer (2000), Change in the probability for earthquakes in southern California due to the Landers magnitude 7.3 earthquake, Science 290, 5495, 1334-1338.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL1-0014-0032
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.