Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11452
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dc.date.accessioned2018-03-23T10:20:03Zen
dc.date.available2018-03-23T10:20:03Zen
dc.date.issued2017-02-24en
dc.identifier.urihttp://hdl.handle.net/2122/11452en
dc.description.abstractThe Sardinia microplate in the western Mediterranean represents an ideal example for examining the relationship between fluid geochemistry, tectonic and heat sources in hydrothermal circuits. It consists of a portion of Variscan basement partly covered by sedimentary (mainly carbonate) and volcanic successions that record significant Permian to Pliocene geodynamic events within the southern European margin. The regional structure of the northern Sardinia is dominated by Tertiary ENE–WSW trending strike-slip and NNW–SSE trending normal faults, both capable of controlling deep and shallow fluid circulation. In this paper, results of a detailed geochemical investigation of waters and gases coming from a W-E trending section of central-north Sardinia are presented in order to explain the contrasting thermal and geochemical features of two - already known groups - of fluids. The Volcanic Logudoro Waters (VLW) is a group of cold to hypothermal Na–HCO3 waters characterised by high CO2 contents and mantle-derived He, that are localized in the volcanic-dominated Tertiary grabens. The He mantle signature within the VLW waters is associated with Plio-Pleistocene Quaternary volcanism where the outgassing of mantle-derived fluids is reasonably due recently active magma sources at depth. The currently active emission of mantle-derived gas linked to cold and hypothermal waters, provides evidence that the heat diffusion associated with the Plio-Pleistocene volcanism has already ended. In contrast, the Granite Variscan Basement Waters (GBW) group is characterised by hot-NaCl-rich waters, containing high concentrations of both dissolved N2 and radiogenic 4He. The high contribution of 4He produced by radiogenic decay of U and Th in the crust indicates a supply of radiogenic heat to the hydrothermal system localized within the granitic basement or in the tectonic contact between granite and Tertiary covers.en
dc.language.isoEnglishen
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries/336 (2017)en
dc.titleGeochemistry of two contrasting deep fluids in the Sardinia microplate (western Mediterranean): Relationships with tectonics and heat sourcesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber108-117en
dc.subject.INGV04.08. Volcanologyen
dc.identifier.doi10.1016/j.jvolgeores.2017.02.011en
dc.description.obiettivoSpecifico1TR. Studi per le Georisorseen
dc.description.journalTypeJCR Journalen
dc.contributor.authorPaternoster, Micheleen
dc.contributor.authorOggiano, Giacomoen
dc.contributor.authorSinisi, Rosaen
dc.contributor.authorCaracausi, Antonioen
dc.contributor.authorMongelli, Giovannien
dc.contributor.departmentDepartment of Sciences, University of Basilicata, Viale dell'Ateneo Lucano 10, 85100 Potenza, Italyen
dc.contributor.departmentDepartment of Sciences for Nature and Environmental Resources, University of Sassari, Via Piandanna 4, 07100 Sassari, Italyen
dc.contributor.departmentDepartment of Sciences, University of Basilicata, Viale dell'Ateneo Lucano 10, 85100 Potenza, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentDepartment of Sciences, University of Basilicata, Viale dell'Ateneo Lucano 10, 85100 Potenza, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità della Basilicata, Potenza, Italy-
crisitem.author.deptDepartment of Sciences for Nature and Environmental Resources, University of Sassari, Via Piandanna 4, 07100 Sassari, Italy-
crisitem.author.deptDepartment of Sciences, University of Basilicata, Viale dell'Ateneo Lucano 10, 85100 Potenza, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptDepartment of Sciences, University of Basilicata, Viale dell'Ateneo Lucano 10, 85100 Potenza, Italy-
crisitem.author.orcid0000-0003-1236-1498-
crisitem.author.orcid0000-0003-4439-3419-
crisitem.author.orcid0000-0003-2510-2890-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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