Cerón García, Juan CarlosPulido Bosch, Antonio2017-02-222017-02-221995http://hdl.handle.net/10272/13367The 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.spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/HydrogeochemistryThermomineral watersNeotectonicsjournal articleopen access