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Article |
Geophysical Laboratory
School of Geology
University of Thessaloniki
Thessaloniki, Greece
costas{at}lemnos.geo.auth.gr
karakais{at}geo.auth.gr
alekos{at}lemnos.geo.auth.gr
basil{at}lemnos.geo.auth.gr
A region of intense accelerating seismic crustal deformation has been
identified in the southwestern part of the Hellenic arc (broader area of
Cythera island). The identification is performed using a detailed parametric
grid search of the broader southern Aegean area for accelerating energy
release behavior. The identified region has similar properties with past
preshock (critical) regions, which have been identified for strong mainshocks
in the Aegean area. Based on such observations, which suggest that this region
is at a critical state that can lead to a critical point, that is, to the
generation of a mainshock, an estimation is made of the possible epicenter
coordinates, magnitude, and origin time of this oncoming large (M
7.0)
earthquake. The estimation procedure is validated on the basis of
retrospective analysis of strong events in the Aegean area, as well as by
appropriate application on synthetic random catalogs. These results, the
existence of similar observations of accelerating seismic deformation in
eastern part of southern Aegean and independent information on the time
distribution of large earthquakes (M
6.8) for the whole southern Aegean
indicate that the generation of strong earthquakes in this area in the next
few years must be considered as very probable.
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