Seismicity map of the 622 aftershocks recorded at more than 20 stations with an RMS smaller than 0.15 sec and located with uncertainties smaller than 1 km in terms of both epicenter and depth. The best solution for the relocated main shock is indicated by a star. The Servia and Deskati faults are plotted as thin barbed lines, whereas the surface ruptures in Paleohori during the earthquake are thick barbed line. The aftershocks were recorded after deploying a temporary seismological network of 40 mobile stations around the epicentral zone within a week after the mainshock.
[from Hatzfeld et al. (1998)].
|
