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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6948
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dc.contributor.authorallIbanez, J.; University of Granada, Spainen
dc.contributor.authorallDel Pezzo, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallDe Miguel, F.; University of Granada, Spainen
dc.contributor.authorallHerraiz, M.; Universidad Complutense, Madrid, Spainen
dc.contributor.authorallAlguacil, F.; University of Granada, Spainen
dc.contributor.authorallMorales, J.; University of Granada, Spainen
dc.date.accessioned2011-02-24T07:12:01Zen
dc.date.available2011-02-24T07:12:01Zen
dc.date.issued1990-10en
dc.identifier.urihttp://hdl.handle.net/2122/6948en
dc.description.abstractCoda-Q estimates for the Granada Basin (Southern Spain) are obtained by analyzing earthquakes occurring within or close to the borders of this area. The data set is composed of 54 earthquakes with local magnitudes ranging between 2.2 and 4.0 and with epicentral distances to the nearest station smaller than 10 km. A single-scattering process is assumed. Coda-Q values obtained show a clear dependence on frequency according to the relationship Q = Qof", where n ranges from 0.81 to 0.89. After removing the main site effects and discussing the possible multiple-scattering influence, the lapse-time dependence is interpreted as due to attenuation variations with depth. This result agrees with the variation of coda Q obtained by using different sets of events with increasing hypocentral depth ranges.en
dc.language.isoEnglishen
dc.publisher.nameSeismological Society of Americaen
dc.relation.ispartofBulletin of the Seismological Society of Americaen
dc.relation.ispartofseries5/80 (1990)en
dc.subjectSeismic attenuationen
dc.subjectCoda-Qen
dc.titleDEPTH-DEPENDENT SEISMIC ATTENUATION IN THE GRANADA ZONE (SOUTHERN SPAIN)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1232-1244en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysisen
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorIbanez, J.en
dc.contributor.authorDel Pezzo, E.en
dc.contributor.authorDe Miguel, F.en
dc.contributor.authorHerraiz, M.en
dc.contributor.authorAlguacil, F.en
dc.contributor.authorMorales, J.en
dc.contributor.departmentUniversity of Granada, Spainen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentUniversity of Granada, Spainen
dc.contributor.departmentUniversidad Complutense, Madrid, Spainen
dc.contributor.departmentUniversity of Granada, Spainen
dc.contributor.departmentUniversity of Granada, Spainen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstituto Andaluz de Geofísica, University of Granada, Granada, Spain,-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptUniversity of Granada, Spain-
crisitem.author.deptUniversidad Complutense Madrid, Madrid, Spain-
crisitem.author.deptUniversity of Granada, Spain-
crisitem.author.deptInstituto Andaluz de Geofísica, Universidad de Granada, Spain-
crisitem.author.orcid0000-0002-9846-8781-
crisitem.author.orcid0000-0002-6981-5967-
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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