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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6557
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dc.contributor.authorallFinizola, A.; Laboratoire GéoSciences Réunion, UR, IPGP, UMR 7154, Saint Denis, La Réunion, Franceen
dc.contributor.authorallRicci, T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallDeiana, R.; Dipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italyen
dc.contributor.authorallBarde Cabusson, S.; Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italyen
dc.contributor.authorallRossi, M.; Dipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italyen
dc.contributor.authorallPraticelli, N.; Dipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italyen
dc.contributor.authorallGiocoli, A.; Laboratorio di Geofisica, IMAA-CNR, Tito Scalo, Potenza, Italyen
dc.contributor.authorallRomano, G.; Tito Scalo, Potenza, Italyen
dc.contributor.authorallDelcher, E.;en
dc.contributor.authorallSuski, B.; Institut de Géophysique, Université de Lausanne, Lausanne, Switzerlanden
dc.contributor.authorallRevil, A.; Colorado School of Mines, Illinois St. Golden, Colorado, USA; CNRS-LGIT, UMR 5559, Université de Savoie, Equipe Volcan, Le Bourget du Lac, Franceen
dc.contributor.authorallMenny, P.; Laboratoire Magmas et Volcans, Université Blaise Pascal, Clermont-Ferrand, Franceen
dc.contributor.authorallDi Gangi, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallLetort, J.; Ecole et Observatoire des Sciences de la Terre, Université de Strasbourg, Franceen
dc.contributor.authorallPeltier, A.; Institut de Physique du Globe de Paris, UMR 7154, Paris, Franceen
dc.contributor.authorallVillasante-Marcos, V.; Instituto Geografico Nacional, Madrid, Spainen
dc.contributor.authorallDouillet, G.; Ecole et Observatoire des Sciences de la Terre, Université de Strasbourg, Franceen
dc.contributor.authorallAvard, G.; Department of Geological Sciences, University of Missouri, USAen
dc.contributor.authorallLelli, M.; Istituto di Geoscienze e Georisorse, CNR, Pisa, Italyen
dc.date.accessioned2011-01-12T08:58:32Zen
dc.date.available2011-01-12T08:58:32Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6557en
dc.description.abstractOn March 15th 2007 a paroxysmal explosion occurred at the Stromboli volcano. This event generated a large amount of products,mostly lithic blocks, someofwhich impacted the ground as far as down to 200 m a.s.l., about 1.5 kmfaraway fromthe active vents. Two days after the explosion, a newvapouremissionwas discovered on the north-eastern flank of the volcanic edifice, at 560 m a.s.l., just above the area called “Nel Cannestrà”. This new vapour emission was due to a block impact. In order to investigate the block impact area to understand the appearance of the vapour emission, we conducted on May 2008 a multidisciplinary study involving Electrical Resistivity Tomography (ERT), Ground Penetrating Radar (GPR), Self-Potential (SP), CO2 soil diffuse degassing and soil temperature surveys. This complementary data set revealed the presence of an anomalous conductive body, probably related to a shallow hydrothermal level, at about 10–15 m depth, more or less parallel to the topography. It is the first time that such a hydrothermal fluid flow,with a temperature close to thewater boiling point (76 °C) has been evidenced at Stromboli at this low elevation on the flank of the edifice. The ERT results suggest a possible link between (1) the main central hydrothermal system of Stromboli, located just above the plumbing system feeding the active vents, with a maximum of subsurface soil temperature close to 90 °C and limited by the NeoStromboli summit crater boundary and (2) the investigated area of Nel Cannestrà, at ~500 m a.s.l., a buried eruptive fissure active 9 ka ago. In parallel, SP and CO2 soil diffuse degassingmeasurements suggest in this sector at slightly lower elevation fromthe block impact crater a magmatic and hydrothermal fluid rising system along the N41° regional fault. A complementary ERT profile, on May 2009, carried out from the NeoStromboli crater boundary downto the block impact crater displayed a flank fluid flowapparently connected to a deeper system. The concept of shallow hydrothermal level have been compared to similar ERT results recently obtained onMount Etna and La Fossa cone of Vulcano. This information needs to be taken into account in general fluid flow models on volcanoes. In particular, peripheral thermal waters (as those bordering the northeastern coast of Stromboli) could be contaminated by hydrothermal and magmatic fluids coming from regional faults but also from the summit.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries/196(2010)en
dc.subjectStrombolien
dc.subjecthydrothermal systemen
dc.subjectadventive hydrothermal flowen
dc.subjectelectrical resistivity tomographyen
dc.subjectself-potentialen
dc.subjectsoil diffuse degassingen
dc.subjecttemperatureen
dc.subject2007 Stromboli eruptive crisisen
dc.titleAdventive hydrothermal circulation on Stromboli volcano (Aeolian Islands, Italy) revealed by geophysical and geochemical approaches: Implications for general fluid flow models on volcanoesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber111-119en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.04. Thermodynamicsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.identifier.doi10.1016/j.jvolgeores.2010.07.022en
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dc.description.obiettivoSpecifico1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveen
dc.description.obiettivoSpecifico1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcanien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorFinizola, A.en
dc.contributor.authorRicci, T.en
dc.contributor.authorDeiana, R.en
dc.contributor.authorBarde Cabusson, S.en
dc.contributor.authorRossi, M.en
dc.contributor.authorPraticelli, N.en
dc.contributor.authorGiocoli, A.en
dc.contributor.authorRomano, G.en
dc.contributor.authorDelcher, E.en
dc.contributor.authorSuski, B.en
dc.contributor.authorRevil, A.en
dc.contributor.authorMenny, P.en
dc.contributor.authorDi Gangi, F.en
dc.contributor.authorLetort, J.en
dc.contributor.authorPeltier, A.en
dc.contributor.authorVillasante-Marcos, V.en
dc.contributor.authorDouillet, G.en
dc.contributor.authorAvard, G.en
dc.contributor.authorLelli, M.en
dc.contributor.departmentLaboratoire GéoSciences Réunion, UR, IPGP, UMR 7154, Saint Denis, La Réunion, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentDipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Firenze, Firenze, Italyen
dc.contributor.departmentDipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italyen
dc.contributor.departmentDipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italyen
dc.contributor.departmentLaboratorio di Geofisica, IMAA-CNR, Tito Scalo, Potenza, Italyen
dc.contributor.departmentTito Scalo, Potenza, Italyen
dc.contributor.departmentInstitut de Géophysique, Université de Lausanne, Lausanne, Switzerlanden
dc.contributor.departmentColorado School of Mines, Illinois St. Golden, Colorado, USA; CNRS-LGIT, UMR 5559, Université de Savoie, Equipe Volcan, Le Bourget du Lac, Franceen
dc.contributor.departmentLaboratoire Magmas et Volcans, Université Blaise Pascal, Clermont-Ferrand, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentEcole et Observatoire des Sciences de la Terre, Université de Strasbourg, Franceen
dc.contributor.departmentInstitut de Physique du Globe de Paris, UMR 7154, Paris, Franceen
dc.contributor.departmentInstituto Geografico Nacional, Madrid, Spainen
dc.contributor.departmentEcole et Observatoire des Sciences de la Terre, Université de Strasbourg, Franceen
dc.contributor.departmentDepartment of Geological Sciences, University of Missouri, USAen
dc.contributor.departmentIstituto di Geoscienze e Georisorse, CNR, Pisa, 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 Roma1, Roma, Italia-
crisitem.author.deptDepartment of Cultural Heritage, University of Padova, Padova, Italy-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy-
crisitem.author.deptDipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italy-
crisitem.author.deptDipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italy-
crisitem.author.deptLaboratorio di Geofisica, IMAA-CNR, Tito Scalo, Potenza, Italy-
crisitem.author.deptUniversità degli Studi di Bari-
crisitem.author.deptLaboratoire GeoSciences Reunion, Universite de la Reunion, Institut de Physique du Globe de Paris, La Reunion, Indian Ocean, France-
crisitem.author.deptUniversité de Lausanne (UNIL), Institut de Géophysique, Lausanne, Switzerland; CNRS-CEREGE, Université Paul Cézanne, Aix en Provence, France-
crisitem.author.deptCentre National de la Recherche Scientifique, Université Paul Cézanne-Aix-Marseille III, CEREGE, Equipe Hydrogéophysique et Milieux Poreux, Aix-en-Provence, France.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptEcole et Observatoire des Sciences de la Terre, Universite de Strasbourg, France-
crisitem.author.deptUniv Paris Diderot, Inst Phys Globe Paris, Sorbonne Paris Cite, Observ Volcanol Piton Fournaise,UMR CNRS 7154, F-97418 La Plaine Des Cafres, France-
crisitem.author.deptEcole et Observatoire des Sciences de la Terre, Université de Strasbourg, France-
crisitem.author.deptLudwig Maximilians Universitaet, Munich, Germany-
crisitem.author.deptObservatorio Vulcanologico y Sismologico de Costa Rica, Costa Rica-
crisitem.author.deptCNR – Istituto di Geoscienze e Georisorse-
crisitem.author.orcid0000-0002-5083-7349-
crisitem.author.orcid0000-0002-0553-5384-
crisitem.author.orcid0000-0002-6037-697X-
crisitem.author.orcid0000-0002-0005-301X-
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-
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