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Hydrochemistry of closed depressions in the Antequera evaporite Karst (Malaga)

dc.contributor.authorBenavente Herrera, José
dc.contributor.authorAlmécija Ruiz, Carmen
dc.contributor.authorCarrasco Cantos, Francisco
dc.contributor.authorRodríguez Jiménez, P.
dc.contributor.authorCruz Sanjulián, J. J.
dc.date.accessioned2019-06-12T09:52:30Z
dc.date.available2019-06-12T09:52:30Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16400
dc.description.abstractSome small temporary and permanent lakes near Antequera (Malaga) have been monitored in order to identify their main hydrochemical features. They display a wide variety both in chemical facies and salinity. The origin of these wetlands is related to triassic evaporite karst: closed depressions induced by dissolution and collapse. The results show in general a close similarity between these waters and those of the most significative springs that drain this karst, with a overimposed effect of saline concentration due to evaporationes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherHydrochemistryes_ES
dc.subject.otherWetlandses_ES
dc.subject.otherEvaporite Karstes_ES
dc.titleReconocimiento hidroquímico de zonas endorreicas del Karst evaporítico de Antequera (Málaga)es_ES
dc.titleHydrochemistry of closed depressions in the Antequera evaporite Karst (Malaga)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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