Hidrogeología del Sector Caspe-Maeíla. Primeros Resultados

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dc.contributor.authorBaquer, E.
dc.contributor.authorColoma, Pablo
dc.contributor.authorSánchez Navarro, José Ángel
dc.contributor.authorMiguel, J. L. de
dc.date.accessioned2015-04-07T08:22:58Z
dc.date.available2015-04-07T08:22:58Z
dc.date.issued1997
dc.description.abstractThe existence of a structural high in the Caspe- Maella area, related with the palaeozoic outcrop of Puigmoreno provokes the groundwater discharge of the carbonate mesozoic aquifer (regional aquifer). 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/10272/10245
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.otherHigh structuralen_US
dc.subject.otherGroundwater dischargeen_US
dc.subject.otherRegional aquiferen_US
dc.subject.otherIberian Chainen_US
dc.subject.otherCaspe-Maella sectoren_US
dc.titleHidrogeología del Sector Caspe-Maeíla. Primeros Resultadosen_US
dc.titleHidrogeology Of Caspe-Maella Sector. First Outputseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 24, (1997)