Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10710
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dc.date.accessioned2018-02-16T07:43:40Zen
dc.date.available2018-02-16T07:43:40Zen
dc.date.issued2017-02-22en
dc.identifier.urihttp://hdl.handle.net/2122/10710en
dc.description.abstractCoda wave attenuation imaging is able to detect fluid/melt accumulation and ancient magmatic bodies in volcanoes. Here we use recently developed space-weighting sensitivity functions to invert for the spatial distributions of multifrequency coda wave attenuation (Q−1 c ), measured during the largest monitored unrest at Campi Flegrei caldera (1983–1984). High-attenuation anomalies are spatially correlated with the regions of highest structural complexities and cross faulting. They characterize deep fluid circulation in and around the aseismic roots of the 1534 A.D. Mount Nuovo eruption and fluid accumulation in the areas of highest hydrothermal hazard. Just offshore Pozzuoli, and at the highest frequency (wavelengths of ∼150 m), the main cause of ground deformation and seismicity during the unrest is an aseismic low-attenuation circular anomaly, similar in shape and nature to those produced by ancient magmatic reservoirs and active sills at other volcanoes.en
dc.language.isoEnglishen
dc.relation.ispartofGeophysical Research Lettersen
dc.relation.ispartofseries/44 (2017)en
dc.titleSpace-weighted seismic attenuation mapping of the aseismic source of Campi Flegrei 1983-84 unresten
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1740-1748en
dc.identifier.doi10.1002/2017GL072507en
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dc.description.obiettivoSpecifico2V. Struttura e sistema di alimentazione dei vulcanien
dc.description.obiettivoSpecifico4V. Dinamica dei processi pre-eruttivien
dc.description.journalTypeJCR Journalen
dc.contributor.authorDe Siena, Lucaen
dc.contributor.authorAmoruso, Antonellaen
dc.contributor.authorDel Pezzo, Edoardoen
dc.contributor.authorWakeford, Zoeen
dc.contributor.authorCastellano, Marioen
dc.contributor.authorCrescentini, Lucaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), 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.deptUniversità degli Studi di Salerno-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptUniversità degli Studi di Salerno-
crisitem.author.orcid0000-0002-3615-5923-
crisitem.author.orcid0000-0002-6981-5967-
crisitem.author.orcid0000-0003-4603-7127-
crisitem.author.orcid0000-0003-1166-3486-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.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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