0000000000886765

AUTHOR

Caterina Liccioli

showing 2 related works from this author

Carbon dioxide diffuse emission and thermal energy release from hydrothermal systems at Copahue-Caviahue Volcanic Complex (Argentina)

2015

Fil: Chiodini, Giovanni. Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna. Bologna, Italia. Fil: Cardellini, Carlo. Università degli Studi di Perugia, Dipartimento di Fisica e Geologia. Perugia, Italy. Fil: Lamberti, María C. Universidad de Buenos Aires. Instituto de Estudios Andinos. Buenos Aires, Argentina. Fil: Agusto, Mariano. Universidad de Buenos Aires. Instituto de Estudios Andinos. Buenos Aires, Argentina. Fil: Caselli, Alberto Tomás Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro. Argentina. Fil: Liccioli, Caterina. Universidad de Buenos Aires. Instituto de Estudios Andinos. Buenos Aires, Argentina. Fil: Tambure…

Earth scienceGeochemistrychemistry.chemical_elementThermal energyCO2 DIFFUSETHERMAL ENERGYHydrothermal circulationCiencias de la Tierra y relacionadas con el Medio AmbienteCopahue Volcano CO2 Diffuse Degasingchemistry.chemical_compoundVulcanologíaGeochemistry and PetrologyCalderaCaviahue Calderageographygeography.geographical_feature_categorybusiness.industryFumaroleCopahue Volcano CO2 diffuse degasingSettore GEO/08 - Geochimica E VulcanologiaGeophysicschemistryVolcanoCAVIAHUE CALDERASoil waterCarbon dioxideCaviahue Caldera Copahue Volcano CO2 diffuse degasing Thermal energyCOPAHUE VOLCANObusinessCO2 fluxCarbonThermal energyGeologyCIENCIAS NATURALES Y EXACTAS
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The hydrothermal system of the Domuyo volcanic complex (Argentina): A conceptual model based on new geochemical and isotopic evidences

2016

The Domuyo volcanic complex (Neuquén Province, Argentina) hosts one of the most promising geothermal systems of Patagonia, giving rise to thermal manifestations discharging hot and Cl−-rich fluids. This study reports a complete geochemical dataset of gas and water samples collected in three years (2013, 2014 and 2015) from the main fluid discharges of this area. The chemical and isotopic composition (δD-H2O and δ18O-H2O) of waters indicates that rainwater and snow melting are the primary recharge of a hydrothermal reservoir located at relative shallow depth (400–600 m) possibly connected to a second deeper (2–3 km) reservoir. Reactive magmatic gases are completely scrubbed by the hydrotherm…

Alternative Energy Source010504 meteorology & atmospheric sciencesHydrothermal FluidGeochemistryAquifer010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationRainwater harvestingDomuyo Volcanic ComplexCiencias de la Tierra y relacionadas con el Medio AmbienteGeothermometryGeochemistry and PetrologyGeomorphologyGeothermal gradientCiencias Exactas y NaturalesGeothermal System0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryGroundwater rechargeDilutionGeophysicsVolcanoMagmaMeteorología y Ciencias AtmosféricasGeologyCIENCIAS NATURALES Y EXACTAS
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