Show simple item record

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.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.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
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

Files in this item

This item appears in the following Collection(s)

Show simple item record

Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

Copyright © 2008-2010. ARIAS MONTANO. Repositorio Institucional de la Universidad de Huelva
Contact Us | Send Feedback |