El drenaje subterráneo de la cordillera Ibérica en la depresión terciaria del Ebro (sector Riojano)

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dc.contributor.authorColoma, Pablo
dc.contributor.authorSánchez Navarro, José Ángel
dc.contributor.authorMartínez Gil, F. J.
dc.date.accessioned2017-06-05T11:32:52Z
dc.date.available2017-06-05T11:32:52Z
dc.date.issued1994
dc.description.abstractAlong 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 characteristics and the hydrogeological groundwater flow of the springs situated in the nortwestern part of this contact (La Rioja sector, Spain)en_US
dc.identifier.urihttp://hdl.handle.net/10272/13786
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherRegional groundwater flowen_US
dc.subject.otherJurassic aquiferen_US
dc.subject.otherHydrogeochemical characteristicsen_US
dc.subject.otherLa Riojaen_US
dc.subject.otherSpainen_US
dc.titleEl drenaje subterráneo de la cordillera Ibérica en la depresión terciaria del Ebro (sector Riojano)en_US
dc.titleThe regional goundwater discharge from the Iberian Chain into the Ebro Tertiary basin (La Rioja sector, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 17, (1994)