Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4825
AuthorsConsole, R.* 
Murru, M.* 
Falcone, G.* 
Catalli, F.* 
TitleStress interaction effect on the occurrence probability of characteristic earthquakes in Central Apennines
Issue Date19-Aug-2008
Series/Report no./113(2008)
DOI10.1029/2007JB005418
URIhttp://hdl.handle.net/2122/4825
KeywordsStress interaction, occurrence probability, characteristic earthquakes
Subject Classification01. Atmosphere::01.02. Ionosphere::01.02.03. Forecasts 
04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology 
04. Solid Earth::04.04. Geology::04.04.06. Rheology, friction, and structure of fault zones 
04. Solid Earth::04.06. Seismology::04.06.02. Earthquake interactions and probability 
04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics 
AbstractIn this study, we compute the effect of stress change due to previous historical earthquakes on the probability of occurrence of future earthquakes on neighboring faults. Following a methodology developed in the last decade, we start from the estimate of the probability of occurrence in the next 50 years for a characteristic earthquake on known seismogenic structures, based on a time-dependent renewal model. Then a physical model for the Coulomb stress change caused by previous earthquakes on these structures is applied. The influence of this stress change on the occurrence rate of characteristic earthquakes is computed, taking into account both permanent (clock advance) and temporary (rate-and-state) perturbations. We apply this method to the computation of earthquake hazard of the main seismogenic structures recognized in the Central and Southern Apennines region, for which both historical and paleoseismological data are available. This study provides the opportunity of reviewing the problems connected with the estimate of the parameters of a renewal model in case of characteristic earthquakes characterized by return times longer than the time spanned by the available catalogues and the applicability of the concept of characteristic earthquake itself. The results show that the estimated effect of earthquake interaction in this region is small compared with the uncertainties affecting the statistical model used for the basic time-dependent hazard assessment.
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