Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/12701
DC FieldValueLanguage
dc.date.accessioned2019-09-16T07:17:29Zen
dc.date.available2019-09-16T07:17:29Zen
dc.date.issued2019-08en
dc.identifier.urihttp://hdl.handle.net/2122/12701en
dc.description.abstractOn December 24th, Mt. Etna volcano underwent a seismic crisis beneath the summit and upper southern flank of the volcano, accompanied by significant ash emission. Eruptive fissures opened at the base of summit craters, propagating SE‐wards. This lateral eruption lasted until December 27th. Despite the small eruption, seismic swarm and ground deformation were very strong. Sentinel‐1 interferograms show a wide and intense ground deformation with some additional features related to volcano‐tectonic structures. We inverted DInSAR data to characterise the magma intrusion. The resulting model indicates that a large dyke intruded but aborted its upraise at about the sea level; however, this big intrusion stretched the edifice, promoting the opening of the eruptive fissures fed by a shallower small dyke, and activating also several faults. This model highlights that a big intrusion beneath a structurally complex volcano represents a main issue even if the eruption is aborted.en
dc.language.isoEnglishen
dc.relation.ispartofTerra Novaen
dc.relation.ispartofseries4/31 (2019)en
dc.subjectgeodesyen
dc.subjecteruptionen
dc.subjectmodelingen
dc.subjectvolcano-tectonicsen
dc.subjectinsaren
dc.subjectdeformationen
dc.titleLarge dyke intrusion and small eruption: The December 24, 2018 Mt. Etna eruption imaged by Sentinel‐1 dataen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber405-412en
dc.identifier.URLhttps://onlinelibrary.wiley.com/doi/10.1111/ter.12403en
dc.subject.INGV04.08. Volcanologyen
dc.subject.INGV04.03. Geodesyen
dc.identifier.doi10.1111/ter.12403en
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Surface deformation due to shear and tensile faults in a half-space: Bulletin of the Seismological Society of America, v. 75, no. 4, p. 1135–1154. Poland, M., Peltier, A., Bonforte, A., and Puglisi, G. (2017). The spectrum of persistent volcanic flank instability: A review and proposed framework based on Kīlauea, Piton de la Fournaise, and Etna. J. Volcanol. Geotherm. Res., 339, 63-80, doi: 10.1016/j.jvolgeores.2017.05.004 Puglisi, G., Bonforte, A., Ferretti, A., Guglielmino, F., Palano, M., and Prati, C. (2008). Dynamics of Mount Etna before, during, and after the July–August 2001 eruption inferred from GPS and differential synthetic aperture radar interferometry data. J. Geophys. Res., 113, B06405, doi:10.1029/2006JB004811. Yang, X.-M., Davis, P.M., and Dieterich, J.H. (1988). Deformation from inflation of a dipping finite prolate spheroid in an elastic half-space as a model for volcanic stressing: Journal of Geophysical Research, v. 93, no. B5, p. 4249–4257.en
dc.description.obiettivoSpecifico5V. Processi eruttivi e post-eruttivien
dc.description.journalTypeJCR Journalen
dc.contributor.authorBonforte, Alessandroen
dc.contributor.authorGuglielmino, Francescoen
dc.contributor.authorPuglisi, Giuseppeen
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.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
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.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0003-0435-7763-
crisitem.author.orcid0000-0003-3258-9975-
crisitem.author.orcid0000-0003-4503-5808-
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.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
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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