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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5011
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dc.contributor.authorallIacono Marziano, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallGaillard, F.; CNRS, INSU, Université d’Orléans, Institut des Sciences de la Terre d’Orléans (ISTO), UMR 6113 CNRS, Orléans Cedex 2, Franceen
dc.contributor.authorallScaillet, B.; CNRS, INSU, Université d’Orléans, Institut des Sciences de la Terre d’Orléans (ISTO), UMR 6113 CNRS, Orléans Cedex 2, Franceen
dc.contributor.authorallPichavant, M.; CNRS, INSU, Université d’Orléans, Institut des Sciences de la Terre d’Orléans (ISTO), UMR 6113 CNRS, Orléans Cedex 2, Franceen
dc.contributor.authorallChiodini, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.date.accessioned2009-04-07T12:37:03Zen
dc.date.available2009-04-07T12:37:03Zen
dc.date.issued2009-04en
dc.identifier.urihttp://hdl.handle.net/2122/5011en
dc.description.abstractMount Vesuvius, Italy, quiescent since A.D. 1944, is a dangerous volcano currently characterized by elevated CO2 emissions of debated origin. We show that such emissions are most likely the surface manifestation of the deep intrusion of alkalic-basaltic magma into the sedimentary carbonate basement, accompanied by sidewall assimilation and CO2 volatilization. During the last eruptive period (1631–1944), the carbonate-sourced CO2 made up 4.7–5.3 wt% of the vented magma. On a yearly basis, the resulting CO2 production rate is comparable to CO2 emissions currently measured in the volcanic area. The chemical and isotopic composition of the fumaroles supports the predominance of this crust-derived CO2 in volatile emissions at Mount Vesuvius.en
dc.language.isoEnglishen
dc.publisher.nameGSAen
dc.relation.ispartofGeologyen
dc.relation.ispartofseries4/37 (2009)en
dc.subjectVolcanic degassingen
dc.subjectcarbonate assimilationen
dc.subjectmagmaen
dc.subjectVesuviusen
dc.titleRole of non-mantle CO2 in the dynamics of volcano degassing: The Mount Vesuvius exampleen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber319-322en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.01. Gasesen
dc.identifier.doi10.1130/G25446A.1en
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dc.description.obiettivoSpecifico4.5. Studi sul degassamento naturale e sui gas petroliferien
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorIacono Marziano, G.en
dc.contributor.authorGaillard, F.en
dc.contributor.authorScaillet, B.en
dc.contributor.authorPichavant, M.en
dc.contributor.authorChiodini, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentCNRS, INSU, Université d’Orléans, Institut des Sciences de la Terre d’Orléans (ISTO), UMR 6113 CNRS, Orléans Cedex 2, Franceen
dc.contributor.departmentCNRS, INSU, Université d’Orléans, Institut des Sciences de la Terre d’Orléans (ISTO), UMR 6113 CNRS, Orléans Cedex 2, Franceen
dc.contributor.departmentCNRS, INSU, Université d’Orléans, Institut des Sciences de la Terre d’Orléans (ISTO), UMR 6113 CNRS, Orléans Cedex 2, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptISTO, Université d’Orleans Campus Geosciences,Orléans, France-
crisitem.author.deptCNRS Orleans, Francia-
crisitem.author.deptCNRS Orleans, Francia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0002-0628-8055-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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