Relación entre la macroestructura del sector oriental de la Cuenca de Almazán y la ubicación de los manantiales termales de Deza, Embid, San (taquillo, Alhama y Jaraba (provincias de Soria y Zaragoza)
The Deza, Embid, San Roquillo, Alhama and Jaraba thermal springs are located in the contact between the Almazan Basin and the Iberian Chain (Aragonesa Branch). The study of deep-geophysics, surface geology and groundwater weels has permitted to interpret the macro-structure and to explain the ground...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1998 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/10192 |
| Acceso en línea: | http://hdl.handle.net/10272/10192 |
| Access Level: | acceso abierto |
| Palabra clave: | Thermal springs Macro-structure Groundwater-flow Hydrogeochemistry |
| Sumario: | The Deza, Embid, San Roquillo, Alhama and Jaraba thermal springs are located in the contact between the Almazan Basin and the Iberian Chain (Aragonesa Branch). The study of deep-geophysics, surface geology and groundwater weels has permitted to interpret the macro-structure and to explain the groundwater-flow, hydrogeochemistry and location of the thermal springs |
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