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Hydrochemical characteristics of CO2-rich waters in Guiraos (Southeast of Spain)

dc.contributor.authorCerón García, Juan Carlos 
dc.contributor.authorPulido Bosch, Antonio
dc.date.accessioned2017-02-22T10:22:05Z
dc.date.available2017-02-22T10:22:05Z
dc.date.issued1995
dc.identifier.urihttp://hdl.handle.net/10272/13367
dc.description.abstractThe groundwater from the Guiraos are calcium-sodium-magnesium sulfate-chloride types and have a high temperature (close to 35 °C) and conductivity (3800 ¡uS/cm). The waters are oversaturated in quartz, dolomite and albite; saturated in calcite, aragonite and chalcedony; and undersaturated in gypsum, anhydrite, barite, halite, cristobalite and fluorite. Silica-quartz and Na-K-Ca geothermometers show a base temperatures between 104 y 112 °C.en_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherHydrogeochemistryen_US
dc.subject.otherThermomineral watersen_US
dc.subject.otherNeotectonicsen_US
dc.titleCaracterísticas hidroquímicas de aguas carbogaseosas en los Guiraos (Sudeste de España)en_US
dc.titleHydrochemical characteristics of CO2-rich waters in Guiraos (Southeast of Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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