Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/12361
DC FieldValueLanguage
dc.date.accessioned2019-03-04T09:32:51Zen
dc.date.available2019-03-04T09:32:51Zen
dc.date.issued2019-02-19en
dc.identifier.urihttp://hdl.handle.net/2122/12361en
dc.description.abstractSeismic resonance inside sedimentary basins severely influences ground shaking at the free surface in case of earthquakes. Starting from few observations of a low-frequency resonance in the historical center of Rome, Italy, we performed several single-station ambient vibration measures to verify and estimate the resonance frequency in a wide area of the city by Horizontal-to-Vertical spectral ratio method. We verified a stable low-frequency peak in the range 0.3–0.4 Hz. Recordings of August 24th 2016, Mw 6.0 Amatrice earthquake, available both inside and outside the basin of Rome, confirm the presence of high-energy components at frequencies of 0.2–0.4 Hz within the basin. These observations support the hypothesis of a deep seismic impedance contrast responsible for the low frequency resonance. To infer the depth range of subsoil deposits related to this impedance contrast, we analyzed ambient vibration data recorded by 2-D seismic arrays aiming at retrieving the shear-wave velocity structure up to relevant depths. To increase the investigation depth (up to 2000 m), we jointly inverted for Rayleigh-waves dispersion and ellipticity curves and resonance frequency. The shear-wave velocity profile shows two main discontinuities at depths of about 500 m and 1800 m that can be related to the bottom of the Plio-Pleistocene filling of the Rome basin and to the top of the basal limestone formation, respectively. These results fill a gap of knowledge about the deep velocity structure in the city that may be helpful for ground-motion scenario studies.en
dc.language.isoEnglishen
dc.publisher.nameSpringer International Publishingen
dc.relation.ispartofPure and Applied Geophysicsen
dc.relation.ispartofseries6/176 (2019)en
dc.subjectAmbient vibrationsen
dc.subjecthorizontal-to-vertical spectral ratioen
dc.subjectsurface-waves dispersion curveen
dc.subjectjoint inversionen
dc.titleThe Deep Bedrock in Rome, Italy: A New Constraint Based on Passive Seismic Data Analysisen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber2395–2410en
dc.subject.INGV04.06. Seismologyen
dc.identifier.doi10.1007/s00024-019-02130-6en
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dc.description.obiettivoSpecifico4T. Sismicità dell'Italiaen
dc.description.journalTypeJCR Journalen
dc.relation.issn0033-4553en
dc.relation.eissn1420-9136en
dc.contributor.authorMarcucci, Sandroen
dc.contributor.authorMilana, Giulianoen
dc.contributor.authorHailemikael, Salomonen
dc.contributor.authorCarlucci, Giorgiaen
dc.contributor.authorCara, Fabrizioen
dc.contributor.authorDi Giulio, Giuseppeen
dc.contributor.authorVassallo, Maurizioen
dc.contributor.departmentDipartimento della Protezione Civile, Rome, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentENEA, Centro Ricerche Frascati, Frascati, Italyen
dc.contributor.departmentDepartment of Science, Roma Tre University, Rome, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento della Protezione Civile Nazionale, Roma, Italy-
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.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.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-2775-4924-
crisitem.author.orcid0000-0002-3007-0830-
crisitem.author.orcid0000-0002-1702-563X-
crisitem.author.orcid0000-0002-4097-7102-
crisitem.author.orcid0000-0001-8552-6965-
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.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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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