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Nat. Hazards Earth Syst. Sci., 9, 501-506, 2009
www.nat-hazards-earth-syst-sci.net/9/501/2009/
doi:10.5194/nhess-9-501-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.


Seismicity anomalies prior to the 13 December 2008, Ms=5.7 earthquake in Central Greece

G. Chouliaras
National Observatory of Athens, Institute of Geodynamics, P.O. Box 20048, 11810 Athens, Greece

Abstract. This investigation has applied a recent methodology to identify seismic quiescence and seismic acceleration, prior to the occurrence of the 13 December 2008, Ms=5.7 earthquake in Central Greece. Anomalous seismic quiescence is observed around the epicentral area almost twelve years prior to the main shock and it lasted for a period of about four and a half years. After this period an acceleration in seismic activity began and lasted until the main shock. Modeling this seismic sequence with the time-to-failure equation and with a fixed value of the exponent "m" equal to 0.32, shows a successful estimation of the occurrence time of the main event within a few days. The physical meaning of this particular choice of the "m" value is discussed.

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Citation: Chouliaras, G.: Seismicity anomalies prior to the 13 December 2008, Ms=5.7 earthquake in Central Greece, Nat. Hazards Earth Syst. Sci., 9, 501-506, doi:10.5194/nhess-9-501-2009, 2009.   Bibtex   EndNote   Reference Manager    XML
 

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