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G. Akis Tselentis
Evidence for stability in Coda Q associated with the Egion (central Greece) earthquake of 15 June 1995
Bulletin of the Seismological Society of America (December 1997), 87(6):1679-1884
Abstract: Index Terms/Descriptors: Latitude & Longitude:
GeoRef, Copyright 2004, American Geological Institute.
One hundred seventy-two seismograms, recorded at one seismological station located close to the source region of the Egion (M s = 6.2) 15 June 1995 earthquake, were used to measure values of Q from the decay of the earthquake coda. The collected data were compared between events that occurred before and after the main event. The analysis showed no significant temporal variation in the value of coda Q for the region.
attenuation; coda waves; earthquakes; Egion earthquake 1995; Egion Greece; elastic waves; equations; Europe; Greece; guided waves; Q; seismic waves; seismograms; Southern Europe; surface waves; time variations
N38°00'00" -
N38°30'00" and
E21°30'00" -
E22°30'00" (Search for maps and images at Alexandria Digital Library)