Características hidroquímicas de aguas carbogaseosas en los Guiraos (Sudeste de España)
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,...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1995 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13367 |
| Acesso em linha: | http://hdl.handle.net/10272/13367 |
| Access Level: | acceso abierto |
| Palavra-chave: | Hydrogeochemistry Thermomineral waters Neotectonics |
| Resumo: | 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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