Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8757
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dc.contributor.authorallDe Lauro, E.; Università degli Studi di Salernoen
dc.contributor.authorallDe Martino, S.; Università degli Studi di Salernoen
dc.contributor.authorallFalanga, M.; Università degli Studi di Salernoen
dc.contributor.authorallPetrosino, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.date.accessioned2013-09-20T07:08:12Zen
dc.date.available2013-09-20T07:08:12Zen
dc.date.issued2013-08-02en
dc.identifier.urihttp://hdl.handle.net/2122/8757en
dc.description.abstractLong continuous seismic data recorded at five broadband seismic stations during 2006 at Campi Flegrei caldera have been analyzed. Introducing a coarse-grained method, we evaluate the time evolution of amplitude and polarization of the seismic noise in the frequency band common to long-period events. The series are modulated on tidal time scales: the root-mean square is basically dominated by solar contribution, while the azimuth of the polarization vector shows lunar diurnal and semidiurnal constituents. In addition, we find that in the frequency band common to long-period events the azimuths are polarized toward a specific area, suggesting that these persistent oscillations can be induced by the activity of the shallow geothermal reservoir.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeochemistry, Geophysics, Geosystemsen
dc.relation.ispartofseries/14 (2013)en
dc.subjectsustained hydrothermal tremoren
dc.subjectCampi Flegrei Calderaen
dc.subjectpolarization analysisen
dc.subjecttidal modulationen
dc.titleSynchronization between tides and sustained oscillations of the hydrothermal system of Campi Flegrei (Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber2628–2637en
dc.identifier.URLhttp://onlinelibrary.wiley.com/doi/10.1002/ggge.20149/pdfen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismologyen
dc.identifier.doi10.1002/ggge.20149en
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn1525-2027en
dc.relation.eissn1525-2027en
dc.contributor.authorDe Lauro, E.en
dc.contributor.authorDe Martino, S.en
dc.contributor.authorFalanga, M.en
dc.contributor.authorPetrosino, S.en
dc.contributor.departmentUniversità degli Studi di Salernoen
dc.contributor.departmentUniversità degli Studi di Salernoen
dc.contributor.departmentUniversità degli Studi di Salernoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversity of Salerno-
crisitem.author.deptUniversity of Salerno-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.orcid0000-0002-8841-1861-
crisitem.author.orcid0000-0002-5042-0244-
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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