Edad y significado de las tufas sobre el río Dúrcal en Cónchar (Granada, Andalucía, España)

dc.contributor.authorTorres, Trinidad de
dc.contributor.authorOrtiz, José Eugenio
dc.contributor.authorArribas, Isabel
dc.contributor.authorMoreno, Laura
dc.contributor.authorSoler, Vicente
dc.date.accessioned2014-04-14T10:38:34Z
dc.date.available2014-04-14T10:38:34Z
dc.date.issued2009
dc.description.abstractThe ages of the tufa terraces of the Dúrcal River, in the vicinity of Cónchar, were obtained through the amino acid racemization method, which define the begining of the fluvial incision and the successive periods of carbonate accumulation and destruction/incision. These processes are related with the evolution of the nearby Padul peat bog, in which the deactivation of the alluvial fans that fed this mire was produced at 400 ka coinciding with the uppermost tufa level formation at Cónchar and, therefore, with the dynamics of the Dúrcal river, which are probably linked to neotectonicsen_US
dc.identifier.urihttp://hdl.handle.net/10272/7963
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherAminoacid racemizationen_US
dc.subject.otherTufasen_US
dc.subject.otherOstracodesen_US
dc.subject.otherPadul peat bogen_US
dc.subject.otherDúrcal riveren_US
dc.titleEdad y significado de las tufas sobre el río Dúrcal en Cónchar (Granada, Andalucía, España)en_US
dc.titleAge and significance of the Dúrcal River tufa deposits in Cónchareng
dc.typejournal articleen_US
dspace.entity.typePublication

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