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dc.contributor.authorHidalgo Estévez, Mari Carmen
dc.contributor.authorRey Arrans, Javier
dc.contributor.authorRedondo, L.
dc.date.accessioned2015-04-13T11:11:43Z
dc.date.available2015-04-13T11:11:43Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10324
dc.description.abstractThe hydrogeological context of the San Andrés spa (province of Jaén) is analysed in this work. Piezometric data, hydrochemical analysis and groundwater quality trends are discussed for groundwater samples obtained from the main aquifer units in the region (jurassic carbonatic aquifer and miocene detrital aquifer) in order to stablish the origin of the San Andrés spring. Considering altitude, discharge rate, temperature and hydrochemical features of the spring, it seems to be related to the miocene hydrogeological uniten_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherHydrogeologyen_US
dc.subject.otherHydrochemistryen_US
dc.subject.otherJurassic aquiferen_US
dc.subject.otherMiocene aquiferen_US
dc.subject.otherSan Andrés spaen_US
dc.titleOrigen de la surgencia del Balneario de San Andrés (Provincia de Jaén)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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