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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9291
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dc.contributor.authorallCarafa, M. M. C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallKastelic, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2015-01-22T10:48:20Zen
dc.date.available2015-01-22T10:48:20Zen
dc.date.issued2014-03en
dc.identifier.urihttp://hdl.handle.net/2122/9291en
dc.description.abstractThe goal of earthquake rate models is to define the long-term rate of seismicity above an established magnitude threshold. No earthquake rate models exist for the External Dinarides, although this area is prone to frequent earthquakes that have significant impacts on natural and human environments. In this study, we apply a tectonic/geodynamic approach to build a fault-based and a deformation-based earthquake rate model for the External Dinarides. The main difference between the two models is the inclusion of off-fault seismicity in the deformation-based earthquake rate model. We explore the impact of the moment-balancing uncertainties on the expected number of earthquakes above an established magnitude. The results show comparable earthquake rates for both input models. The slip rate, the elastic modulus and the seismogenic depth play important roles in the variability of earthquake rates, whereas the effects of the corner magnitude and the Gutenberg-Richter β parameter are insignificant. A comparison with the available historical seismic catalogue shows good agreement for MW>5.8 earthquakes.en
dc.language.isoEnglishen
dc.publisher.nameIstituto Nazionale di Oceanografia e di Geofisica Sperimentale-OGSen
dc.relation.ispartofBollettino di Geofisica Teorica ed Applicataen
dc.relation.ispartofseries1/55(2014)en
dc.subjectactive fault, geodynamics, moment rate, earthquake rate, seismic hazard, External Dinaridesen
dc.titleEarthquake rates inferred from active faults and geodynamics: the case of the External Dinaridesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber69-83en
dc.identifier.URLhttp://www2.ogs.trieste.it/bgta/pdf/bgta0112_CARAFA.pdfen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismologyen
dc.identifier.doi10.4430/bgta0112en
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dc.description.obiettivoSpecifico1T. Geodinamica e interno della Terraen
dc.description.obiettivoSpecifico2T. Tettonica attivaen
dc.description.obiettivoSpecifico3T. Pericolosità sismica e contributo alla definizione del rischioen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.relation.issn0006-6729en
dc.contributor.authorCarafa, M. M. C.en
dc.contributor.authorKastelic, V.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0001-5463-463X-
crisitem.author.orcid0000-0002-7751-0055-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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