Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4152
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dc.contributor.authorallLanzafame, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallNeri, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallAcocella, V.; Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.contributor.authorallBilli, A.; Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.contributor.authorallFuniciello, R.; Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.contributor.authorallGiordano, G.; Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.date.accessioned2008-11-11T11:46:00Zen
dc.date.available2008-11-11T11:46:00Zen
dc.date.issued2003-07en
dc.identifier.urihttp://hdl.handle.net/2122/4152en
dc.description.abstractWe describe the evolution of the volcanic activity and deformation patterns observed at Mount Etna during the July–August 2001 eruption. Seismicity started at 3000 m below sea level on 13 July, accompanied by moderate ground swelling. Ground deformation culminated on 16 July with the development of a NE–SW graben c. 500 m wide and c. 1 m deep in the Cisternazza area at 2600–2500 m above sea level on the southern slope of the volcano. On 17 July, the eruption started at the summit of Mount Etna from the SE Crater (central–lateral eruptive system), from which two radial, c. 30 m wide, c. 3000 m long fracture zones, associated with eruptive fissures, propagated both southward (17 July) and northeastward (20 July). On 18 July, a new vent formed at 2100 m elevation, at the southern base of the Montagnola, followed on the next day by the opening of a vent further upslope, at 2550 m (eccentric eruptive system). The eruption lasted for 3 weeks. Approximately 80% of the total lava volume was erupted from the 2100 m and the 2550 m vents. The collected structural data suggest that the Cisternazza graben developed as a passive local response of the volcanic edifice to the ascent of a north–south eccentric dyke, which eventually reached the ground surface in the Montagnola area (18–19 July). In contrast, the two narrow fracture zones radiating from the summit are interpreted as the lateral propagation, from the conduit of the SE Crater, of north–south- and NE–SW-oriented shallow dykes, 2–3 m wide. The evolution of the fracture pattern together with other volcanological data (magma ascent and effusion rate, eruptive style, petrochemical characteristics of the erupted products, and petrology of xenoliths within magma) suggest that the eccentric and central–lateral eruptions were fed by two distinct magmatic systems. Examples of eccentric activity accompanied by central–lateral events have never been described before at Etna.en
dc.language.isoEnglishen
dc.publisher.nameGeological Society of Londonen
dc.relation.ispartofJournal of the Geological Societyen
dc.relation.ispartofseries4/160 (2003)en
dc.subjectMount Etnaen
dc.subjectJuly–August 2001 Eruptionen
dc.subjectmagmasen
dc.subjectdykesen
dc.titleStructural features of the July–August 2001 Mount Etna eruption: evidence for a complex magma supply systemen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber531-544en
dc.identifier.URLhttp://jgs.geoscienceworld.org/cgi/content/abstract/160/4/531?maxtoshow=&HITS=10&hits=10&RESULTFORMAT=1&author1=neri+&andorexacttitle=and&field_name=fulltext&searchid=1&FIRSTINDEX=0&sortspec=relevance&fdate=2/1/2002&tdate=12/31/2003&resourcetype=HWCITen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.05. Stressen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.03. Magmasen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocksen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoringen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.subject.INGV05. General::05.02. Data dissemination::05.02.03. Volcanic eruptionsen
dc.identifier.doi10.1144/0016-764902-151en
dc.description.obiettivoSpecifico1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcanien
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.obiettivoSpecifico3.5. Geologia e storia dei sistemi vulcanicien
dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorLanzafame, G.en
dc.contributor.authorNeri, M.en
dc.contributor.authorAcocella, V.en
dc.contributor.authorBilli, A.en
dc.contributor.authorFuniciello, R.en
dc.contributor.authorGiordano, G.en
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.departmentDip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.contributor.departmentDip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.contributor.departmentDip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
dc.contributor.departmentDip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
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.deptUniversità Roma Tre, Dipartimento di Scienze Geologiche, Rome, Italy-
crisitem.author.deptUniversità degli Studi di Roma Tre-
crisitem.author.orcid0000-0002-5890-3398-
crisitem.author.orcid0000-0002-6368-1873-
crisitem.author.orcid0000-0002-5819-443X-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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