Caracterización hidrogeológica de la Sierra de la Horna (Alicante)

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dc.contributor.authorAndreu Rodes, José Miguel
dc.contributor.authorGarcía Sánchez, Ernesto
dc.contributor.authorPulido Bosch, Antonio
dc.contributor.authorHernández, A.
dc.date.accessioned2015-02-13T12:35:49Z
dc.date.available2015-02-13T12:35:49Z
dc.date.issued1999
dc.description.abstractIn this paper we present the preliminary results ofthe'study of Sierra de Horna aquifer. There is a conection between Horna aquifer and the detritical aquifer of Rambla del Tarafa deduced from the piezometric data: The hydrochemistry results have shown .that most saline waters lie in the deepest parts of the aquifer, while those of lowest mineralization occupy the area of the saturated zone closest to the surfaceen_US
dc.identifier.urihttp://hdl.handle.net/10272/9925
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.otherKarstic aquiferen_US
dc.subject.otherHydrogeochemistryen_US
dc.subject.otherVertical zonationen_US
dc.subject.otherHornaen_US
dc.subject.otherAlicanteen_US
dc.titleCaracterización hidrogeológica de la Sierra de la Horna (Alicante)en_US
dc.titleHydrogeologie characterization of the Sierra de la Horna (Alicante)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 27, (1999)