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Procesos geotérmicos causados por la circulación del agua subterránea en el contacto entre ¡a Sierra de Cameros y la Depresión Terciaria del Ebro
Geothermal processes caused by groundwater circulation along the contact between the Cameros Chain and the Ebro Tertiary Basin
| dc.contributor.author | Coloma, Pablo | |
| dc.contributor.author | Sánchez Navarro, José Ángel | |
| dc.contributor.author | Martínez Gil, F. J. | |
| dc.date.accessioned | 2016-06-20T10:59:54Z | |
| dc.date.available | 2016-06-20T10:59:54Z | |
| dc.date.issued | 1996 | |
| dc.identifier.uri | http://hdl.handle.net/10272/12390 | |
| dc.description.abstract | 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 patterns) should be in very close cooperation at the Interpretation of geothermal anomalies. In this work it is show an example: the geothermal processes along the Cameros Chain/Ebro Tertiary Basin contact | en_US |
| dc.language.iso | spa | en_US |
| dc.publisher | Sociedad Geológica de España | en_US |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
| dc.subject.other | Geothermal systems | en_US |
| dc.subject.other | Convective | en_US |
| dc.subject.other | Groundwater | en_US |
| dc.subject.other | Cameros Chain/Ebro Tertiar | en_US |
| dc.subject.other | Basin contact | en_US |
| dc.title | Procesos geotérmicos causados por la circulación del agua subterránea en el contacto entre ¡a Sierra de Cameros y la Depresión Terciaria del Ebro | en_US |
| dc.title | Geothermal processes caused by groundwater circulation along the contact between the Cameros Chain and the Ebro Tertiary Basin | eng |
| dc.type | info:eu-repo/semantics/article | en_US |
| dc.rights.accessRights | info:eu-repo/semantics/openAccess | en_US |
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