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25 janvier 2010
- handle: 10670/1.gmwn98
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Copyright (c) 2017 G.F. Karakaisis, C.B. Papazachos, E.M. Scordilis , https://creativecommons.org/licenses/by-nc/4.0
Mots-clés
seismic sources seismic faultsSujets proches
Primary sources Forerunners Primary sourcesCiter ce document
G.F. Karakaisis et al., « SEISMIC SOURCES AND MAIN SEISMIC FAULTS IN THE AEGEAN AND SURROUNDING AREA », eJournals, ID : 10670/1.gmwn98
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A seismic source is defined, in the present work, as the part of the seismogenic layer of theearth’s crust with a circular horizontal dimension (E, R), where E is the epicenter of the largestearthquake (mainshock) ever occurred in this seismic source and radius equal to the half faultlength of this largest earthquake (R=L/2). In addition to foreshocks and aftershocks othersmaller mainshocks occur in other smaller faults of this source or in parts of the main fault.All available historical and instrumental data concerning strong (M³6.0) shallow (h≤60 km) andintermediate depth (60km