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Browsing by Author "Martínez Gil, F. J."
Now showing items 1-6 of 6
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El drenaje subterráneo de la Cordillera Ibérica en la depresión del Ebro: aspectos geológicos
(Sociedad Geológica de España, 1990)Six hydrogeologic cross-sections, all of them placed along the contact between the Iberian Chain and the Tertiary Ebro Basin, are presented in this work. These cross-sections avoid us to establish a «geometric model» which ... -
El drenaje subterráneo de la cordillera Ibérica en la depresión terciaria del Ebro (sector Riojano)
(Sociedad Geológica de España, 1994)Along the contact between the Iberian Chain from the Ebro tertiary Basin takes place the regional groundwater flow discharge trhough the mesozoic carbonate rocks (Jurassic aquifer), in this work, it is shown the hydrogeochemical ... -
El drenaje subterráneo de la Sierra de Cameros en la Cuenca del Ebro y su implicación en la génesis de depósitos marginales evaporíticos miocenos
(Sociedad Geológica de España, 1996)In the northern margin of the Cameros Basin miocene evaporitics units are found related with shallow saline lakes. The lakes were fed principal)/ by groundwater loaded with dissolved salts (calcicsulphate waters) from the ... -
Isopiezas y direcciones del flujo regional en el acuífero carbonatado mesozoico del margen Ibérico de la Depresión del Ebro
Sánchez Navarro, José Ángel; San Román, J.; Miguel, J. L. de; Pérez Muñoz, Antonio
; Martínez Gil, F. J. (Sociedad Geológica de España, 1991)
Groundwater discharge from the Iberian Chain into the Ebro tertiary basin takes place through the mesozoic carbonated rocks. These rocks extend from La Rioja to the Mediterranean sea. In this work, it is shown the Jurassic ... -
La Laguna de Añavieja. Funcionamiento y génesis
(Sociedad Geológica de España, 1996)The Ahavieja pool (located in Northern Soria Province, Spain) is a wetland (actually drainig) feeded by a mesozoic karstic aquifer; the resources of this aquifer are 8 ,2 hm3/year. The size of the pool is maller than 7 km ... -
Procesos geotérmicos causados por la circulación del agua subterránea en el contacto entre ¡a Sierra de Cameros y la Depresión Terciaria del Ebro
(Sociedad Geológica de España, 1996)The practically important part of geothermal systems belong to the convective type where the termal energy is transported by movement of groundwater. Both geothermics and hydrology (aquifer geometry and groundwater flow ...
