Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/13447
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dc.date.accessioned2020-03-10T10:14:06Z-
dc.date.available2020-03-10T10:14:06Z-
dc.date.issued2019-02-20-
dc.identifier.urihttp://hdl.handle.net/2122/13447-
dc.descriptionAn edited version of this paper was published by AGU. Copyright (2019) American Geophysical Unionen_US
dc.description.abstractTectonic and magmatic activity may couple at volcanic arcs, even though any relationship is less defined in smaller arcs, experiencing limited activity. Here we use gas geochemistry data collected during the 2011–2012 unrest at Santorini (Greece) to understand better the dynamics of the Aegean Volcanic Arc with regard to its tectonic setting. Since the most recent eruption in 1950 and before the unrest, minor seismicity and CO2 degassing (mainly from the fumaroles of Nea Kameni islet) were observed at Santorini. On January 2011, anomalous seismicity along the NE‐SW trending Kameni Line was accompanied by an inflation north of Nea Kameni. Fumarolic gas composition changed and gas release notably increased. We carried out geochemical study on both Kameni and Thera islands from January 2012 to June 2013. We repeated surveys of diffuse soil CO2 degassing and of in‐soil gas concentration, and we analyzed fumaroles and gas dissolved in thermal waters for chemical and isotopic composition. In agreement with previous studies, our geochemical data, particularly the diffuse soil CO2 flux increase, the increase of H2 content, and of CO2/CH4 and 3He/4He ratios in fumarolic gases, support geophysical data in indicating that unrest was associated with the emplacement of new mafic magma. This unrest had limited effect on the regional setting, with gas emissions focusing along the regional NE‐SW structures, without triggering by any seismic event, conversely to the 1950 eruption, which probably occurred in a frame of general tectonic reorganization of the Aegean microplate.en_US
dc.language.isoEnglishen_US
dc.publisher.nameAguen_US
dc.relation.ispartofTectonicsen_US
dc.relation.ispartofseries3/38 (2019)en_US
dc.subjectExtensive and systematic geochemical surveys followed the anomalous degassing during Santorini unrest, both in the caldera center and on the inner caldera walls;en_US
dc.subjectGas ratios and isotopic composition indicate deep mafic magma refilling into the shallow dacitic plumbing system;en_US
dc.subjectUnrest has limited apparent relations with the longer-term tectonic evolution of the Arc, conversely to the 1950 eruptionen_US
dc.titleFluid Geochemistry Contribution to the Interpretation of the 2011–2012 Unrest of Santorini, Greece, in the Frame of the Dynamics of the Aegean Volcanic Arcen_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.type.QualityControlPeer-revieweden_US
dc.description.pagenumber1033-1049en_US
dc.identifier.URLhttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018TC005377en_US
dc.subject.INGV04.08. Volcanologyen_US
dc.subject.INGV04.06. Seismologyen_US
dc.identifier.doi10.1029/2018TC005377en_US
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dc.description.obiettivoSpecifico2V. Struttura e sistema di alimentazione dei vulcanien_US
dc.description.obiettivoSpecifico4V. Processi pre-eruttivien_US
dc.description.obiettivoSpecifico6V. Pericolosità vulcanica e contributi alla stima del rischioen_US
dc.description.journalTypeJCR Journalen_US
dc.contributor.authorTarchini, Luca-
dc.contributor.authorCarapezza, Maria Luisa-
dc.contributor.authorRanaldi, Massimo-
dc.contributor.authorSortino, Francesco-
dc.contributor.authorGattuso, Alessandro-
dc.contributor.authorAcocella, Valerio-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen_US
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 Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptUniversità Roma Tre, Dipartimento di Scienze Geologiche, Rome, Italy-
crisitem.author.orcid0000-0001-6045-0802-
crisitem.author.orcid0000-0002-0223-6012-
crisitem.author.orcid0000-0001-6464-6298-
crisitem.author.orcid0000-0002-2400-911X-
crisitem.author.orcid0000-0003-1815-0421-
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.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-
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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