Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3163
DC FieldValueLanguage
dc.contributor.authorallRestivo, A.; OGS, Triesteen
dc.contributor.authorallMichelini, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallBarnaba, C.; OGS, Triesteen
dc.date.accessioned2007-12-13T07:11:24Zen
dc.date.available2007-12-13T07:11:24Zen
dc.date.issued2006-09en
dc.identifier.urihttp://hdl.handle.net/2122/3163en
dc.description.abstractThe area of Serravalle, sited in the northern part of the town of Vittorio Veneto (TV), NE Italy, has been the target of a seismic microzonation campaign. 10 seismic stations have been deployed for a 7 months period to record in continuous mode. Three stations were installed on bedrock outcrops and seven on sedimentary sites with variable cover thickness. Spectral analyses have been performed on the collected data-set using the Generalized Inversion Technique (GIT, e.g. Andrews, 1986). In particular, spectral ratios have been calculated for each station relatively to the average of the three reference, bedrock sites. The spectral ratios provide quantitative estimates of the seismic motion amplifications which occur in each of the monitored sites. Two sites show high values of amplification, 5 times larger than signal amplitude at the reference sites, in correspondence of well discernible peak frequencies of 5 Hz. Results for the other stations show smaller amounts of site amplification spreading over a broad range of frequencies. Sites where the highest amplifications were recorded all lie on the left bank of the Meschio River and in areas farther away from its outlet into the plain correlating with the presence of thick layers of Quaternary deposits.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofNatural Hazardsen
dc.relation.ispartofseries1/39 (2006)en
dc.subjectspectral ratiosen
dc.subjectreference sitesen
dc.subjectsite effectsen
dc.subjectearthquake grounf motionen
dc.titleSite effects study in the Serravalle village (NE Italy) by means of spectral ratios analyses relatively to multiple reference sitesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber31-49en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.04. Ground motionen
dc.identifier.doi10.1007/s11069-005-2960-0en
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorRestivo, A.en
dc.contributor.authorMichelini, A.en
dc.contributor.authorBarnaba, C.en
dc.contributor.departmentOGS, Triesteen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentOGS, Triesteen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptOGS, Trieste-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptOGS-
crisitem.author.orcid0000-0001-6716-8551-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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