Isopiezas y direcciones del flujo regional en el acuífero carbonatado mesozoico del margen Ibérico de la Depresión del Ebro

dc.contributor.authorSánchez Navarro, José Ángel
dc.contributor.authorSan Román, J.
dc.contributor.authorMiguel, J. L. de
dc.contributor.authorPérez Muñoz, Antonio
dc.contributor.authorMartínez Gil, F. J.
dc.date.accessioned2020-05-18T10:02:11Z
dc.date.available2020-05-18T10:02:11Z
dc.date.issued1991
dc.description.abstractGroundwater discharge from the Iberian Chain into the Ebro tertiary basin takes place through the mesozoic carbonated rocks. These rocks extend from La Rioja to the Mediterranean sea. In this work, it is shown the Jurassic aquifer equipotential levels map as well as the groundwater flow directions. The recharge and discharge areas, the aquifer-river relationship, and the hydrogeological limits of the aquifer are also shownes_ES
dc.identifier.urihttp://hdl.handle.net/10272/17990
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.titleIsopiezas y direcciones del flujo regional en el acuífero carbonatado mesozoico del margen Ibérico de la Depresión del Ebroes_ES
dc.titleEquipotencial levels and groundwater flow directions in the mesozoic carbonated aquifer from the Iberian chain into the Thro Tertiary basineng
dc.typejournal articlees_ES
dspace.entity.typePublication
relation.isAuthorOfPublication4413386b-2903-47be-a5e2-2bd24f507b31
relation.isAuthorOfPublication.latestForDiscovery4413386b-2903-47be-a5e2-2bd24f507b31

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