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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10269
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dc.contributor.authorallLiuzzo, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallDi Muro, A.; Institut de Physique du Globe de Paris, Observatoire Volcanologique du Piton de la Fournaise, Sorbonne Paris-Cite, CNRS UMR-7154, Universite Paris Diderot, Paris, Franceen
dc.contributor.authorallGiudice, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallMichon, L.; Laboratoire Geosciences Reunion, Universite de La Reunion, Institut de Physique du Globe de Paris, Sorbonne Paris Cite, CNRS, F-97744 Saint-Denis, Franceen
dc.contributor.authorallFerrazzini, V.; Institut de Physique du Globe de Paris, Observatoire Volcanologique du Piton de la Fournaise, Sorbonne Paris-Cite, CNRS UMR-7154, Universite Paris Diderot, Paris, Franceen
dc.contributor.authorallGurrieri, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.date.accessioned2016-02-29T08:43:16Zen
dc.date.available2016-02-29T08:43:16Zen
dc.date.issued2015-12-31en
dc.identifier.urihttp://hdl.handle.net/2122/10269en
dc.description.abstractPiton de la Fournaise (PdF) is recognised as one of the world’s most active volcanoes in terms of eruptive frequency and the substantial quantity of lava produced. Yet, with the sole exception of rather modest intracrateric fumarole activity, this seems to be in contrast with an apparent absence of any type of natural fluid emission during periods of quiescence. Measurement campaigns were undertaken during a long-lasting quiescent period (2012-2014) and just after a short lived summit eruption (June 2014) in order to identify potential degassing areas in relation to the main structural features of the volcano (ex. rift zones) with the aim of developing a broader understanding of the geometry of the plumbing and degassing system. In order to assess the possible existence of anomalous soil CO2 flux, 513 measurements were taken along transects roughly orthogonal to the known tectonic lineaments crossing PdF edifice. In addition, 53 samples of gas for C isotope analysis were taken at measurement points that showed a relatively high CO2 concentration in the soil. CO2 flux values range from 10 to 1300 g m-2 d-1 while 13C are between -26.6 to -8‰. The results of our investigation clearly indicate that there is a strong spatial correlation between the anomalous high values of diffusive soil emissions and the main rift zones cutting the PdF massif and, moreover, that generally high soil CO2 fluxes show a d13C signature clearly related to a magmatic origin.en
dc.description.sponsorshipINSU (CNRS) and La Réunion Préfecture (Projet pour la quantification de l’aléa volcanique à La Réunion)en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeochemistry, Geophysics, Geosystemsen
dc.relation.ispartofseries12/16 (2015)en
dc.subjectCO2 soil degassing anomalies at Piton de la Fournaiseen
dc.subjectd13C magmatic signatureen
dc.subjectClose link between anomalous CO2 degassing and the main seismotectonic structuresen
dc.titleNew evidence of CO2 soil degassing anomalies on Piton de la Fournaise volcano and the link with volcano tectonic structuresen
dc.title.alternativeCO2 SOIL DEGASSING ON PITON DE LA FOURNAISEen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber4388–4404en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.01. Geochemical explorationen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.01. Gasesen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoringen
dc.identifier.doi10.1002/2015GC006032en
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dc.description.obiettivoSpecifico2V. Dinamiche di unrest e scenari pre-eruttivien
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.eissn1525-2027en
dc.contributor.authorLiuzzo, M.en
dc.contributor.authorDi Muro, A.en
dc.contributor.authorGiudice, G.en
dc.contributor.authorMichon, L.en
dc.contributor.authorFerrazzini, V.en
dc.contributor.authorGurrieri, S.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Observatoire Volcanologique du Piton de la Fournaise, Sorbonne Paris-Cite, CNRS UMR-7154, Universite Paris Diderot, Paris, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentLaboratoire Geosciences Reunion, Universite de La Reunion, Institut de Physique du Globe de Paris, Sorbonne Paris Cite, CNRS, F-97744 Saint-Denis, Franceen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Observatoire Volcanologique du Piton de la Fournaise, Sorbonne Paris-Cite, CNRS UMR-7154, Universite Paris Diderot, Paris, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
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crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Pisa, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptLaboratoire Geosciences Reunion, Universite de La Reunion, Institut de Physique du Globe de Paris, Sorbonne Paris Cite, CNRS, F-97744 Saint-Denis, France-
crisitem.author.deptObservatoire Volcanologique du Piton de la Fournaise, Institut de Physique du Globe de Paris, La Réunion, France-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.orcid0000-0002-3099-7505-
crisitem.author.orcid0000-0002-9410-4139-
crisitem.author.orcid0000-0003-4085-0440-
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.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
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-
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