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  5. Seismic hazard disaggregation in the Molise region, Italy: the case study of Campobasso
 
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Seismic hazard disaggregation in the Molise region, Italy: the case study of Campobasso

Author(s)
Caccavale  
Dipartimento di Scienze Fisiche; Dipartimento di Scienze Fisiche, M.; Dipartimento di Scienze Fisiche, Università Federico II di Napoli, Italy.  
Convertito, V.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Mancini, M.  
Structural and Geotechnical Dynamic Lab StreGa,- University of Molise.  
Fabbrocino, G.  
Structural and Geotechnical Dyn  
Type
Conference paper
Language
English
Obiettivo Specifico
4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionale
Status
Unpublished
Journal
14th European Conference on Earthquake Engineering  
Date Issued
2010
Conference Location
Ohrid, Republic of Macedonia
URI
https://www.earth-prints.org/handle/2122/6751
Subjects
04. Solid Earth::04.06. Seismology::04.06.04. Ground motion  
04. Solid Earth::04.06. Seismology::04.06.11. Seismic risk  
Subjects

seismic hazard

geotechnical monitori...

Abstract
Large scale experimentations play a relevant role in the earthquake engineering research, similarly Structural
Health Monitoring is able to give information of real structures. A few geotechnical structures are documented,
because only data on seismic permanent deformations are available. The present paper deals with seismic hazard
of the site of the Student House at University of Molise, where a geotechnical monitoring system has been
designed and is currently under implementation. It is aimed at refining the seismic hazard characterization for
identifying a set of relevant earthquakes for the theoretical analysis of the structure. Reference earthquakes
expressed in terms of magnitude (M), distance (R) and ε, were therefore investigated. Uniform hazard spectra at
different structural periods for a 475-year return period were disaggregated. Shapes of both the joint and marginal
probability density functions were studied and the first two modes of M, R and ε were extracted and discussed.
References
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