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pure and applied geophysics

, Volume 140, Issue 4, pp 593–612 | Cite as

Long-term earthquake prediction in the Aegean area based on a time and magnitude predictable model

  • B. C. Papazachos
  • Ch. A. Papaioannou
Article

Abstract

The Aegean and surrounding area (34°N–43°N, 18°E–30°E) is separated into 76 shallow and intermediate depth seismogenic sources. For 74 of these sources intervent times for strong mainshocks have been determined by the use of instrumental and historical data. These times have been used to determine the following empirical relations:
$$\begin{gathered} \log T_t = 0.24M_{\min } + 0.25M_p - 0.36\log \dot M_0 + 7.36 \hfill \\ M_f = 1.04M_{\min } - 0.31M_p + 0.28\log \dot M_0 - 4.85 \hfill \\ \end{gathered} $$
whereT1 is the interevent time, measured in years,Mmin the surface wave magnitude of the smallest mainshock considered,Mp the magnitude of the preceding mainshock,Mf the magnitude of the following mainshock,\(\dot M_0 \) the moment rate in each source per year. A multiple correlation coefficient equal to 0.74 and a standard deviation equal to 0.18 for the first of these relations were calculated. The corresponding quantities for the second of these relations are 0.91 and 0.22.

On the basis of the first of these relations and taking into consideration the time of occurence and the magnitude of the last mainshock, the probabilities for the occurrence of mainshocks in each seismogenic source of this region during the decade 1993–2002 are determined. The second of these relations has been used to estimate the magnitude of the expected mainshock.

Key words

Earthquake prediction seismicity models aegean area 

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Copyright information

© Birkhäuser Verlag 1993

Authors and Affiliations

  • B. C. Papazachos
    • 1
  • Ch. A. Papaioannou
    • 1
  1. 1.Geophysical LaboratoryUniversity of ThessalonikiThessaloniki, MacedoniaGreece

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