Baquer, E.Coloma, PabloSánchez Navarro, José Ángel2015-03-252015-03-251998http://hdl.handle.net/10272/10160The 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 BasinspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Isotopie ratios wO/u O and 2H/HGroundwater dischargeRegional aquiferIberian ChainCaspe - Maella sectorjournal articleopen access