Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9306
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dc.contributor.authorallBruno, P. P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallCastiello, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallVillani, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallImprota, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2015-02-09T07:33:54Zen
dc.date.available2015-02-09T07:33:54Zen
dc.date.issued2013-06-01en
dc.identifier.urihttp://hdl.handle.net/2122/9306en
dc.description.abstractSeismic hazards in extensional regions are mostly posed by high-angle normal faults and deep hanging-wall basins that can promote significant groundmotion amplifications. Characterized by strong lateral velocity variations, these structures represent challenging targets for seismic exploration. In this paper, we show that prestack depth migration of high-resolution seismic-reflection data, collected with nonconventional dense wide-aperture arrays, can effectively assist deterministic seismic-hazard assessment of fault-bounded basins. Our high-resolution 3.2 km long seismic profile was acquired along Vallo di Diano, the largest fault-bounded intramontane basin in the southern Apennines seismic belt (Italy). The imaging strategy combines prestack depth migration with an iterative velocity-building technique that utilizes results of multiscale refraction tomography. In particular, migration of steeply dipping reflections is essential in imaging the complex morphology of the basement rocks beneath the basin. By combining seismic-reflection and VP tomography results we were able to evaluate (1) the structure of the Vallo di Diano basin along a representative transect from near-surface to basement depths; (2) the shallow-depth geometry of the Vallo di Diano fault system, which bounds the basin to the east; (3) the structure of the sediment–basement interface; and (4) the velocity structure of basement and sediments within the basin. These findings are valuable both for understanding the tectonic evolution of the Vallo di Diano and for developing earthquake-shaking scenario studies.en
dc.language.isoEnglishen
dc.relation.ispartofBullettin Seismological Society of Americaen
dc.relation.ispartofseries3/103(2013)en
dc.subjectseismic imaging of a fault-bounded basinen
dc.titleHigh-Resolution Densely Spaced Wide-Aperture Seismic Profiling as a Tool to Aid Seismic Hazard Assessment of Fault-Bounded Intramontane Basins: Application to Vallo di Diano, Southern Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1969-1980en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methodsen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolutionen
dc.identifier.doi10.1785/0120120071en
dc.description.obiettivoSpecifico2T. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorBruno, P. P.en
dc.contributor.authorCastiello, A.en
dc.contributor.authorVillani, F.en
dc.contributor.authorImprota, L.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
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.grantfulltextreserved-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0003-2622-3037-
crisitem.author.orcid0000-0001-7133-0136-
crisitem.author.orcid0000-0003-0952-3978-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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