Contribución de los datos isotópicos al conocimiento hidrogeológico del sector Caspe-Maella

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dc.contributor.authorBaquer, E.
dc.contributor.authorColoma, Pablo
dc.contributor.authorSánchez Navarro, José Ángel
dc.date.accessioned2015-03-25T13:46:33Z
dc.date.available2015-03-25T13:46:33Z
dc.date.issued1998
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.identifier.urihttp://hdl.handle.net/10272/10160
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.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
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 25, (1998)