Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5838
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dc.contributor.authorallChiodini, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.date.accessioned2010-01-22T18:40:41Zen
dc.date.available2010-01-22T18:40:41Zen
dc.date.issued2009-01-17en
dc.identifier.urihttp://hdl.handle.net/2122/5838en
dc.description.abstractLong time series of fumarolic compositions at Campi Flegrei (Italy), Mammoth Mountain (California), Panarea (Italy) and Nisyros (Greece) show rapid increases, up to orders of magnitude, of the CO2/CH4 ratio systematically with the occurrence of volcanic unrest periods. These easily detected anomalies originate with the arrival of CH4-poor magmatic fluids in the shallower levels of the volcanoes. The data suggest that volcanoes are characterized by magmatic activity at depth also in periods of apparent quiescence. The activity is constituted by the pulsing release of large amount of fluids which either cause unrest periods (seismicity and ground deformation) or possibly could precede volcanic eruption. This type of volcanic activity can be monitored trough the classical geophysical techniques together with the systematic sampling and analysis of fumaroles.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeophysical Research Lettersen
dc.relation.ispartofseries/36(2009)en
dc.subjectCO2/CH4en
dc.subjectmagma degassingen
dc.subjectquiescent volcanoesen
dc.titleCO2/CH4 ratio in fumaroles a powerful tool to detect magma degassing episodes at quiescent Volcanoesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberL02302en
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gasesen
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systemsen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
dc.identifier.doi10.1029/2008GL036347en
dc.relation.referencesCaliro, S., G. Chiodini, R. Moretti, R. Avino, D. Granieri, M. Russo, and J. Fiebig (2007), The origin of the fumaroles of La Solfatara (Campi Flegrei, south Italy), Geochim. Cosmochim. Acta, 71, 3040–3055. Chiodini, G., and L. Marini (1998), Hydrothermal gas equilibria: The H2OH2- CO2-CO-CH4 system, Geochim. Cosmochim. Acta, 62, 2673– 2687. Chiodini, G., R. Cioni, and L. Marini (1993), Reactions governing the chemistry of crater fumaroles from Vulcano Island, Italy, and implications for volcanic surveillance, Appl. Geochem., 8, 357–371. Chiodini, G., F. Frondini, C. Cardellini, D. Granieri, L.Marini, and G. Ventura (2001), CO2 degassing and energy release at Solfatara volcano, Campi Flegrei, Italy, J. Geophys. Res., 106, 16,213–16,221. Chiodini, G., T. Brombach, S. Caliro, C. Cardellini, L.Marini, and V. Dietrich (2002), Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece), Geophys. Res. Lett., 29(16), 1759, doi:10.1029/ 2001GL014355. Chiodini, G., M. Todesco, S. Caliro, C. Del Gaudio, G. Macedonio, and M. Russo (2003), Magma degassing as a trigger of bradyseismic events: The case of Phlegrean Fields (Italy), Geophys. Res. Lett., 30(8), 1434, doi:10.1029/2002GL016790 Chiodini, G., S. Caliro, G. Caramana, D. Granieri, C. Minopoli, R. Moretti, L. Perrotta, and G. Ventura (2006), Geochemistry of the submarine gaseous emissions of Panarea (Aeolian Islands, southern Italy): Magmatic vs. hydrothermal origin and implications for volcanic surveillance, Pure Appl. Geophys., 163, 759– 780, doi:10.1007/s00024-006-0037-y. D’Amore, F., and C. Panichi (1980), Evaluation of deep temperature of hydrothermal systems by a new gas-geothermometer,Geochim. Cosmochim. Acta, 44, 549–556. Dvorak, J. J., and G. Mastrolorenzo (1991), The Mechanisms of Recent Vertical Crustal Movements in Campi Flegrei Caldera, Southern Italy, Spec. Pap. Geol. Soc. Am., 263, 47 pp. Giggenbach, W. F. (1987), Redox processes governing the chemistry of fumarolic gas discharges from White Island, New Zeland, Appl. Geochem., 2, 143–161. Giggenbach, W. F. (1996), Chemical composition of volcanic gases, in Monitoring and Mitigation of Volcanic Hazards, edited by R. Scarpa and R. I. Tilling, pp. 221–256, Springer, New York. Giggenbach, W. F. (1997), Relative importance of thermodynamic and kinetic processes in governing the chemical and isotopic composition of carbon gases in high-heatflow sedimentary systems, Geochim. Cosmochim. Acta, 61, 3763–3785. Italiano, F., and P.M.Nuccio (1991), Geochemical investigations of submarine exhalations to the east of Panarea, Aeolian Islands, Italy, J. Volcanol. Geotherm. Res., 46, 125– 141. Miller, S. A., C. Collettini, L. Chiaraluce, M. Cocco, M. R. Barchi, and B. Kaus (2004), Aftershocks driven by a high pressure CO2 source at depth, Nature, 427, 724–727. Orsi, G., L. Civetta, C. Del Gaudio, S. de Vita, M. Di Vito, R. M. Isaia, S. Petrazzuoli, G. Ricciardi, and C. Ricco (1999), Short-term ground deformations and seismicity in the nested Campi Flegrei caldera (Italy): An example of active block resurgence in a densely populated area, J. Volcanol. Geotherm. Res., 91, 415–451. Ricco, C., I. Aquino, S. Borgstro¨m, and C. Del Gaudio (2007), The study of the tiltmetric inversion recorded from July to October 2006 at the Phlegrean Fields (Naples, Italy), Ann. Geophys., 50, 661– 674. Sachpazi, M., C. Kontoes, N. Voulgaris, M. Laigle, G. Vougioukalakis, O. Sikioti, G. Stavrakakis, J. Baskoutas, J. Kalogeras, and J. C. Lepine (2002), Seismological and SAR signature of unrest at Nisyros caldera, Greece, J. Volcanol. Geotherm. Res., 116, 19–33. Sorey, M. L., W. C. Evans, B. M. Kennedy, C. D. Farrar, L. J. Hainsworth, and B. Hausback (1998), Carbon dioxide and helium emissions from a reservoir of magmatic gas beneath Mammoth Mountain, California, J. Geophys. Res., 103, 15,303–15,323. Todesco, M., G. Chiodini, and G. Macedonio (2003), Monitoring and modeling hydrothermal fluid emission at La Solfatara (Phlegrean Fields, Italy). An interdisciplinary approach to the study of diffuse degassing, J. Volcanol. Geotherm. Res., 125, 57– 80. Troise, C., G. De Natale, F. Pingue, F. Obrizzo, P. De Martino, U. Tammaro, and E. Boschi (2007), Renewed ground uplift at Campi Flegrei caldera (Italy): New insight on magmatic processes and forecast, Geophys. Res. Lett., 34, L03301, doi:10.1029/2006GL028545en
dc.description.obiettivoSpecifico1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveen
dc.description.obiettivoSpecifico2.4. TTC - Laboratori di geochimica dei fluidien
dc.description.obiettivoSpecifico4.5. Studi sul degassamento naturale e sui gas petroliferien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorChiodini, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
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 Bologna, Bologna, Italia-
crisitem.author.orcid0000-0002-0628-8055-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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