Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4319
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dc.contributor.authorallAmicucci, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallBarchi, M. R.; Università di Perugiaen
dc.contributor.authorallMontone, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallRubiliani, N.; ENI S.p.A.en
dc.date.accessioned2008-11-26T08:13:47Zen
dc.date.available2008-11-26T08:13:47Zen
dc.date.issued2008-12-31en
dc.identifier.urihttp://hdl.handle.net/2122/4319en
dc.description.abstractThe aim of this paper was to provide a significant case-history concerning the evolution of a segmented system of extensional faults and related basins, investigated by a set of seismic reflection profiles. We investigated two kinematically linked semi-grabens, developed at the hangingwall of two opposite- dipping normal faults: the Vallo di Diano and Auletta basins, located in the southern Apennines, one of the most seismically active regions of the Italian peninsula. Our interpretation suggests that the Pliocene–Quaternary tectonic history consists of a single extensional phase, where the major NW–SE trending normal faults, generating the basins, and the strike-slip and transtensional faults connecting adjacent normal fault seg- ments, simultaneously act, being part of the same extensional system. We also conclude that major normal faults, bordering the basins, should be considered as potential seismogenic sources in the seismic hazard evaluation.en
dc.description.sponsorshipThis work has been developed within the 2005–2008 FIRB Project Research and Development of New Technologies for Protection and Defence of Territory from Natural Risks , W.P. C3 Crustal Imaging in Italy coordinated by P. Montone, funded by the Italian Ministry of Uni- versity and Research.en
dc.language.isoEnglishen
dc.publisher.nameBlackwellen
dc.relation.ispartofTerra Novaen
dc.relation.ispartofseries6/20 (2008)en
dc.subjectSeismotectonicsen
dc.subjectCommercial seismic linesen
dc.subjectVallo di Dianoen
dc.subjectSouthern Italyen
dc.titleThe Vallo di Diano and Auletta extensional basins in the southernen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber475 - 482en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methodsen
dc.identifier.doi10.1111/j.1365-3121.2008.00841.xen
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorAmicucci, L.en
dc.contributor.authorBarchi, M. R.en
dc.contributor.authorMontone, P.en
dc.contributor.authorRubiliani, N.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniversità di Perugiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentENI S.p.A.en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
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.deptUniversità degli studi di Perugia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptENI S.p.A.-
crisitem.author.orcid0000-0003-0431-4341-
crisitem.author.orcid0000-0002-9297-1730-
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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