Características hidroquímicas de aguas carbogaseosas en los Guiraos (Sudeste de España)
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Abstract
The 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.
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