Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/12701
DC Field | Value | Language |
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dc.date.accessioned | 2019-09-16T07:17:29Z | en |
dc.date.available | 2019-09-16T07:17:29Z | en |
dc.date.issued | 2019-08 | en |
dc.identifier.uri | http://hdl.handle.net/2122/12701 | en |
dc.description.abstract | On 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.iso | English | en |
dc.relation.ispartof | Terra Nova | en |
dc.relation.ispartofseries | 4/31 (2019) | en |
dc.subject | geodesy | en |
dc.subject | eruption | en |
dc.subject | modeling | en |
dc.subject | volcano-tectonics | en |
dc.subject | insar | en |
dc.subject | deformation | en |
dc.title | Large dyke intrusion and small eruption: The December 24, 2018 Mt. Etna eruption imaged by Sentinel‐1 data | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 405-412 | en |
dc.identifier.URL | https://onlinelibrary.wiley.com/doi/10.1111/ter.12403 | en |
dc.subject.INGV | 04.08. Volcanology | en |
dc.subject.INGV | 04.03. Geodesy | en |
dc.identifier.doi | 10.1111/ter.12403 | en |
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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.obiettivoSpecifico | 5V. Processi eruttivi e post-eruttivi | en |
dc.description.journalType | JCR Journal | en |
dc.contributor.author | Bonforte, Alessandro | en |
dc.contributor.author | Guglielmino, Francesco | en |
dc.contributor.author | Puglisi, Giuseppe | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.orcid | 0000-0003-0435-7763 | - |
crisitem.author.orcid | 0000-0003-3258-9975 | - |
crisitem.author.orcid | 0000-0003-4503-5808 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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Bonforte_et_al-2019-Terra_Nova.pdf | 2.04 MB | Adobe PDF | View/Open |
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