Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/12095
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dc.date.accessioned2019-01-28T09:44:32Zen
dc.date.available2019-01-28T09:44:32Zen
dc.date.issued2015en
dc.identifier.urihttp://hdl.handle.net/2122/12095en
dc.description.abstractCampi Flegrei caldera (Italy) was affected by a new unrest phase during 2011-13. We exploit two COSMO-SkyMed datasets to map the deformation field, obtaining displacement rates reaching 9 cm/yr in 2012 in the caldera center. The resulting dataset is fitted in a geophysical inversion framework using finite element forward models to account for the 3D heterogeneous medium. The best-fit model is a North dipping mixed-mode dislocation source lying at ~5 km depth. The driving mechanism is ascribable to magma input into the source of the large 1982-84 unrest (since similar source characteristics were inferred) that generates initial inflation followed by additional shear slip accompanying the extension of crack tips. The history and the current state of the system indicate that Campi Flegrei is able to erupt again, and the advanced techniques adopted provide useful information for short-term forecasting.en
dc.language.isoEnglishen
dc.publisher.nameAGUen
dc.relation.ispartofGeophysical Research Lettersen
dc.relation.ispartofseries/42 (2015)en
dc.titleGeodetic constraints to the source mechanism of the 2011-2013 unrest at Campi Flegrei (Italy) calderaen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber3847-3854en
dc.identifier.doi10.1002/2015gl063621en
dc.relation.referencesAmoruso, A., L. Crescentini, and I. Sabbietta (2014a), Paired deformation sources of the Campi Flegrei caldera (Italy) required by recent (1980–2010) deformation history, J. Geophys. Res., 119, 858-879, doi:10.1002/2013JB010392. Amoruso, A., L. Crescentini, I. Sabbietta, P. De Martino, F. Obrizzo, and U. Tammaro (2014b), Clues to the cause of the 2011-2013 Campi Flegrei caldera unrest, Italy, from cGPS data, Geophys. Res. Lett., 3081-3088, doi:10.1002/2014GL059539. Chiarabba, C., and M. Moretti (2006), An insight into the unrest phenomena at the Campi Flegrei caldera from Vp and Vp/Vs tomography, Terra Nova, 18, 373–379, doi:10.1111/j.1365-3121.2006.00701.x. Chiodini, G., S. Caliro, P. De Martino, R. Avino, and F. Gherardi (2012), Early signals of new volcanic unrest at Campi Flegrei caldera? Insights from geochemical data and physical simulations, Geology, 40, 943-946, doi:10.1130/G33251.1. Chiodini, G., J. Vandemeulebrouck, S. Caliro, L. D’Auria, P. De Martino, A. Mangiacapra, and Z. Petrillo (2015), Evidence of thermal-driven processes triggering the 2005–2014 unrest at Campi Flegrei caldera, Earth Plan. Sci. Lett., 414, 58-67, doi:10.1016/j.epsl.2015.01.012. De Martino, P., U. Tammaro, and F. Obrizzo (2014), GPS time series at Campi Flegrei caldera (2000-2013), Ann. Geophys., 57, 2, S0213, doi:10.4401/ag-6431. De Natale, G., F. Pingue, P. Allard, and A. Zollo (1991), Geophysical and geochemical modelling of the 1982–1984 unrest phenomena at Campi Flegrei caldera (southern Italy), J. Volcanol. Geotherm. Res., 48, 199–222. De Siena, L., E. Del Pezzo, and F. Bianco (2010), Seismic attenuation imaging of Campi Flegrei: Evidence of gas reservoirs, hydrothermal basins, and feeding systems, J. Geophys. Res., 115, B09312, doi:10.1029/2009JB006938. Macedonio, G., F. Giudicepietro, L. D'Auria, and M. Martini (2014), Sill intrusion as a source mechanism of unrest at volcanic calderas, J. Geophys. Res. Solid Earth, 119, 3986–4000, doi:10.1002/2013JB010868. Manconi, A., T. R. Walter, and F. Amelung (2007), Effects of mechanical layering on volcano deformation, Geophys. J. Int., 170, 952–958, doi: 10.1111/j.1365-246X.2007.03449.x. Parascandola, A. (1947), I fenomeni bradisismici del Serapeo di Pozzuoli, Napoli Tip. Genovese, 156 pp. Rosi, M., A. Sbrana, and C. Principe (1983), The Phlegraean Fields; structural evolution, volcanic history and eruptive mechanisms, J. Volcanol. Geotherm. Res., 17, 273–288. Sambridge, M. (1999a), Geophysical inversion with a neighbourhood algorithm - I. Searching a parameter space, Geophys. J. Int., 138 (2), 479-494. Sambridge, M. (1999b), Geophysical inversion with a neighbourhood algorithm - II. Appraising the ensemble, Geophys. J. Int., 138 (3), 727-746. Samsonov, S. V., K. F. Tiampo, A. G. Camacho, J. Fernández, and P. J. González (2014), Spatiotemporal analysis and interpretation of 1993–2013 ground deformation at Campi Flegrei, Italy, observed by advanced DInSAR, Geophys. Res. Lett., 41, 6101–6108, doi:10.1002/2014GL060595. Trasatti, E., C. Giunchi, and M. Bonafede (2005), Structural and rheological constraints on source depth and overpressure estimates at the Campi Flegrei Caldera, Italy, J. Volc. Geotherm. Res., 144, 105–118. Trasatti, E., C. Giunchi, and N. P. Agostinetti (2008), Numerical inversion of deformation caused by pressure sources: application to Mount Etna (Italy), Geophys. J. Int., 172 (2), 873-884. Trasatti, E., M. Bonafede, C. Ferrari, C. Giunchi, and G. Berrino (2011), On deformation sources in volcanic areas: modeling the Campi Flegrei (Italy) 1982–84 unrest, Earth Plan. Sci. Lett., 306, 175-185, doi:10.1016/j.epsl.2011.03.033. Werner, C., U. Wegmüller, T. Strozzi, and A. Wiesmann (2003), Interferometric Point Target Analysis for Deformation Mapping, Geosci. and Remote Sensing Symp, 7, 4362-4364, doi:10.1109/IGARSS.2003.1295516. Zollo, A., N. Maercklin, M. Vassallo, D. Dello Iacono, J. Virieux, and P. Gasparini, (2008), Seismic reflections reveal a massive melt layer feeding Campi Flegrei caldera, Geophys. Res. Lett.,35, L12306, doi:10.1029/2008GL034242.en
dc.description.obiettivoSpecifico4V. Dinamica dei processi pre-eruttivien
dc.description.journalTypeJCR Journalen
dc.contributor.authorTrasatti, Elisaen
dc.contributor.authorPolcari, Marcoen
dc.contributor.authorBonafede, Maurizioen
dc.contributor.authorStramondo, Salvatoreen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptUniversity of Bologna-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0002-2983-045X-
crisitem.author.orcid0000-0003-0506-3492-
crisitem.author.orcid0000-0003-0163-7647-
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.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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