Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1412
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dc.contributor.authorallCastro, R. R.; División Ciencias de la Tierra, CICESE, Baja California, Méxicoen
dc.contributor.authorallMucciarelli, M.; Università della Basilicata, Potenza, Italyen
dc.contributor.authorallMonachesi, G.; Osservatorio Geofisico Sperimentale di Macerata, Italyen
dc.contributor.authorallPacor, F.; ISMES, Divisione Geofisica, Bergamo, Italyen
dc.contributor.authorallBerardi, R.; Ente Nazionale per l'Energia Elettrica (ENEL), Roma, Italyen
dc.date.accessioned2006-07-26T12:52:16Zen
dc.date.available2006-07-26T12:52:16Zen
dc.date.issued1999-08en
dc.identifier.urihttp://hdl.handle.net/2122/1412en
dc.description.abstractWe used a set of previously published nonparametric attenuation functions to calculate average functions for the Italian region. These nonparametric functions describe the spectral amplitude decay of the S waves as a function of distance for 14 frequencies between 1 and 20 Hz for the regions of Lombardia-Piemonte, Eastern Sicily, Friuli, Marche and the Central Apennines. Since all the attenuation functions were obtained using the same methodology, we were able to make a fair comparison of the attenuation characteristics of the different regions. In general, while the Central Apennines show the strongest amplitude decay for all the frequencies analyzed, the regions of Lombardia and Eastern Sicily show the smallest attenuation. The Marche region also shows a strong amplitude decay, particularly for frequencies f > 3 Hz, and in the frequency band between 1 and 3 Hz the rate of decay of the spectral amplitudes with distance becomes similar to that of the region of Friuli. Since the attenuation functions analyzed represent different geologic and tectonic environments, we used them to calculate an average set of attenuation functions, one per frequency, for the hypocentral distance range between 10 and 120 km. The resulting functions permit a mean attenuation correction to spectral records of S waves in regions of Italy where the specific values of the attenuation parameters are unknown.en
dc.format.extent5146706 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries4/42 (1999)en
dc.subjectSeismic attenuationen
dc.subjectS wavesen
dc.subjectnon-parametric inversioen
dc.subjectacceleration spectraen
dc.titleA review of nonparametric attenuation functions computed for different regions of Italyen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysisen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorCastro, R. R.en
dc.contributor.authorMucciarelli, M.en
dc.contributor.authorMonachesi, G.en
dc.contributor.authorPacor, F.en
dc.contributor.authorBerardi, R.en
dc.contributor.departmentDivisión Ciencias de la Tierra, CICESE, Baja California, Méxicoen
dc.contributor.departmentUniversità della Basilicata, Potenza, Italyen
dc.contributor.departmentOsservatorio Geofisico Sperimentale di Macerata, Italyen
dc.contributor.departmentISMES, Divisione Geofisica, Bergamo, Italyen
dc.contributor.departmentEnte Nazionale per l'Energia Elettrica (ENEL), Roma, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCICESE, División Ciencias de la Tierra, Departamento de Sismología, Ensenada, Baja California, México-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia-
crisitem.author.deptEnte Nazionale per l'Energia Elettrica (ENEL), Roma, Italy-
crisitem.author.orcid0000-0001-5745-0414-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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