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Isotopie data contribution to the higrogeology knowledge of Caspe-Maella sector

dc.contributor.authorBaquer, E.
dc.contributor.authorColoma, Pablo
dc.contributor.authorSánchez Navarro, José Ángel
dc.description.abstractThe isotopie ratios of 180/16 O and 2H/1H, confirms the discharge of a regional carbonate aquifer in the Caspe - Maella area. The recharge area of this aquifer takes place in the Iberian Chain and the discharge takes place through low permeable tertiary detritical material of Ebro Basinen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherIsotopie ratios wO/u O and 2H/Hen_US
dc.subject.otherGroundwater dischargeen_US
dc.subject.otherRegional aquiferen_US
dc.subject.otherIberian Chainen_US
dc.subject.otherCaspe - Maella sectoren_US
dc.titleContribución de los datos isotópicos al conocimiento hidrogeológico del sector Caspe-Maellaen_US
dc.titleIsotopie data contribution to the higrogeology knowledge of Caspe-Maella sectoreng

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