Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11618
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dc.date.accessioned2018-03-30T12:33:45Zen
dc.date.available2018-03-30T12:33:45Zen
dc.date.issued2017-09-15en
dc.identifier.urihttp://hdl.handle.net/2122/11618en
dc.description.abstractIn the Central Mediterranean region, the production of chemically diverse volcanic products (e.g., those from Mt. Etna and the Aeolian Islands archipelago) testifies to the complexity of the tectonic and geodynamic setting. Despite the large number of studies that have focused on this area, the relationships among volcanism, tectonics, magma ascent, and geodynamic processes remain poorly understood. We present a tomographic inversion of P-wave velocity using active and passive sources. Seismic signals were recorded using both temporary on-land and ocean bottom seismometers and data from a permanent local seismic network consisting of 267 seismic stations. Active seismic signals were generated using air gun shots mounted on the Spanish Oceanographic Vessel ‘Sarmiento de Gamboa’. Passive seismic sources were obtained from 452 local earthquakes recorded over a 4-month period. In total, 184,797 active P-phase and 11,802 passive P-phase first arrivals were inverted to provide three different velocity models. Our results include the first crustal seismic active tomography for the northern Sicily area, including the Peloritan–southern Calabria region and both the Mt. Etna and Aeolian volcanic environments. The tomographic images provide a detailed and complete regional seismotectonic framework and highlight a spatially heterogeneous tectonic regime, which is consistent with and extends the findings of previous models. One of our most significant results was a tomographic map extending to 14 km depth showing a discontinuity striking roughly NW–SE, extending from the Gulf of Patti to the Ionian Sea, south-east of Capo Taormina, corresponding to the Aeolian–Tindari– Letojanni fault system, a regional deformation belt. Moreover, for the first time, we observed a high-velocity anomaly located in the south-eastern sector of the Mt. Etna region, offshore of the Timpe area, which is compatible with the plumbing system of an ancient shield volcano located offshore of Mt. Etna.en
dc.language.isoEnglishen
dc.relation.ispartofSurveys in Geophysicsen
dc.relation.ispartofseries/39 (2018)en
dc.rightsCC0 1.0 Universalen
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/en
dc.subjectSeismic tomographyen
dc.subjectMt. Etnaen
dc.subjectAeolian Islandsen
dc.subjectVolcanicen
dc.titleNew Insights on Mt. Etna’s Crust and Relationship with the Regional Tectonic Framework from Joint Active and Passive P-Wave Seismic Tomographyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber57-97en
dc.subject.INGV04en
dc.identifier.doi10.1007/s10712-017-9425-3en
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dc.description.obiettivoSpecifico7T. Struttura della Terra e geodinamicaen
dc.description.journalTypeJCR Journalen
dc.contributor.authorDíaz-Moreno, A.en
dc.contributor.authorBarberi, Graziellaen
dc.contributor.authorCocina, Ornellaen
dc.contributor.authorKoulakov, I.en
dc.contributor.authorScarfì, Lucianoen
dc.contributor.authorZuccarello, Lucianoen
dc.contributor.authorPrudencio, J.en
dc.contributor.authorGarcía-Yeguas, A.en
dc.contributor.authorÁlvarez, I.en
dc.contributor.authorGarcìa, L.en
dc.contributor.authorIbáñez, J. M.en
dc.contributor.departmentDepartment of Earth, Ocean and Ecological Sciences, School of Environmental Sciences, Jane Herdman Building, 4 Brownlow Street, Liverpool, Merseyside L69 3GP, UKen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentTrofimuk Institute of Petroleum Geology and Geophysics SB RAS, Prospekt Koptyuga, 3, Novosibirsk, Russia 630090en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentDepartment of Earth and Planetary Science, University of California at Berkeley, Berkeley, CA 94709, USAen
dc.contributor.departmentInstituto Andaluz de Geofisica, University of Granada, 18071 Granada, Spainen
dc.contributor.departmentDepartment of Communication and Signal Theory, University of Granada, 18071 Granada, Spainen
dc.contributor.departmentDepartment of Communication and Signal Theory, University of Granada, 18071 Granada, Spainen
dc.contributor.departmentInstituto Andaluz de Geofisica, University of Granada, 18071 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.deptUniversity of Liverpool, UK-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIPGG SB RAS, Novosibirsk, Russia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Italy-
crisitem.author.deptInstituto Andaluz de Geofisica, Universidad de Granada-
crisitem.author.deptInstituto Andaluz de Geofísica, Universidad de Granada, Granada, Spain-
crisitem.author.deptInstituto Andaluz de Geofísica, University of Granada, Granada, Spain,-
crisitem.author.orcid0000-0002-8273-0458-
crisitem.author.orcid0000-0003-1856-830X-
crisitem.author.orcid0000-0002-5995-3880-
crisitem.author.orcid0000-0003-0094-9577-
crisitem.author.orcid0000-0003-1755-3771-
crisitem.author.orcid0000-0002-9846-8781-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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