Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10388
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dc.contributor.authorallDi Napoli, R.; Dipartimento di Scienze della Terra e del Mare, Universit a di Palermoen
dc.contributor.authorallAiuppa, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallSulli, A.; Dipartimento di Scienze della Terra e del Mare, Universit a di Palermoen
dc.contributor.authorallCaliro, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallChiodini, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallAcocella, V.; Dipartimento di Scienze Universit a di Roma Tre, Roma, Italyen
dc.contributor.authorallCiraolo, G.; Dipartimento di Ingegneria di Palermo, Palermo Civile, Ambientale, Aerospaziale, dei Materiali, Universitàen
dc.contributor.authorallDi Vito, M. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallInterbartolo, F.; Dipartimento di Scienze della Terra e del Mare, Universit a di Palermo, Palermoen
dc.contributor.authorallNasello, C.; Dipartimento di Ingegneria Civile, Ambientale, Aerospaziale, dei Materiali, Università di Palermoen
dc.contributor.authorallValenza, M.; Dipartimento di Scienze della Terra e del Mare, Universit a di Palermoen
dc.date.accessioned2016-11-21T07:21:43Zen
dc.date.available2016-11-21T07:21:43Zen
dc.date.issued2016en
dc.identifier.urihttp://hdl.handle.net/2122/10388en
dc.description.abstractThe ongoing unrest at the Campi Flegrei caldera (CFc) in southern Italy is prompting exploration of its poorly studied offshore sector. We report on a multidisciplinary investigation of the Secca delle Fumose (SdF), a submarine relief known since antiquity as the largest degassing structure of the offshore sector of CFc. We combined high-resolution morphobathymetric and seismostratigraphic data with onshore geological information to propose that the present-day SdF morphology and structure developed during the initial stages of the last CFc eruption at Monte Nuovo in AD 1538. We suggest that the SdF relief stands on the eastern uplifted border of a N-S-trending graben-like structure formed during the shallow emplacement of the Monte Nuovo feeding dike. We also infer that the high-angle bordering faults that generated the SdF relief now preferentially allow the ascent of hot brines (with an equilibrium temperature of 1798C), thereby sustaining hydrothermal degassing on the seafloor. Systematic vertical seawater profiling shows that hydrothermal seafloor venting generates a sizeable CO2, pH, and temperature anomaly in the overlying seawater column. Data for the seawater vertical profile can be used to estimate the CO2 and energy (heat) outputs from the SdF area at 50 tons/d ( 0.53 kg/s) and 80 MW, respectively. In view of the cause-effect relationship with the Monte Nuovo eruption, and the substantial gas and energy outputs, we consider that the SdF hydrothermal system needs to be included in monitoring programs of the ongoing CFc unrest.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeochemistry, Geophysics, Geosystemsen
dc.relation.ispartofseries10/17 (2016)en
dc.subjectHydrothermal fluiden
dc.subjectCampi Flegrei calderaen
dc.titleHydrothermal fluid venting in the offshore sector of Campi Flegrei caldera: A geochemical, geophysical and volcanological studyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber4153–4178en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneousen
dc.identifier.doi10.1002/2016GC006494en
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dc.description.obiettivoSpecifico1V. Storia e struttura dei sistemi vulcanicien
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.eissn1525-2027en
dc.contributor.authorDi Napoli, R.en
dc.contributor.authorAiuppa, A.en
dc.contributor.authorSulli, A.en
dc.contributor.authorCaliro, S.en
dc.contributor.authorChiodini, G.en
dc.contributor.authorAcocella, V.en
dc.contributor.authorCiraolo, G.en
dc.contributor.authorDi Vito, M. A.en
dc.contributor.authorInterbartolo, F.en
dc.contributor.authorNasello, C.en
dc.contributor.authorValenza, M.en
dc.contributor.departmentDipartimento di Scienze della Terra e del Mare, Universit a di Palermoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra e del Mare, Universit a di Palermoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentDipartimento di Scienze Universit a di Roma Tre, Roma, Italyen
dc.contributor.departmentDipartimento di Ingegneria di Palermo, Palermo Civile, Ambientale, Aerospaziale, dei Materiali, Universitàen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra e del Mare, Universit a di Palermo, Palermoen
dc.contributor.departmentDipartimento di Ingegneria Civile, Ambientale, Aerospaziale, dei Materiali, Università di Palermoen
dc.contributor.departmentDipartimento di Scienze della Terra e del Mare, Universit a di Palermoen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità di Palermo, DiSTeM, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptUniversità degli Studi di Palermo-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptUniversità Roma Tre, Dipartimento di Scienze Geologiche, Rome, Italy-
crisitem.author.deptDipartimento di Ingegneria di Palermo, Palermo Civile, Ambientale, Aerospaziale, dei Materiali, Università-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptDipartimento di Scienze della Terra e del Mare, Universit a di Palermo, Palermo-
crisitem.author.deptDipartimento di Ingegneria Civile, Ambientale, Aerospaziale, dei Materiali, Università di Palermo-
crisitem.author.deptDiSTeM, Universit a degli Studi di Palermo, Palermo, Italy-
crisitem.author.orcid0000-0002-6175-3124-
crisitem.author.orcid0000-0002-0254-6539-
crisitem.author.orcid0000-0002-7705-3632-
crisitem.author.orcid0000-0002-8522-6695-
crisitem.author.orcid0000-0002-0628-8055-
crisitem.author.orcid0000-0002-7913-9149-
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.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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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