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Sedimentary filling and destruction of a small fluvio-lacustrine basin in the Sierra Sur of Jaén (Betic Cordilleras)

dc.contributor.authorGarcía García, Fernando
dc.contributor.authorSánchez Gómez, Mario
dc.date.accessioned2014-11-06T10:13:33Z
dc.date.available2014-11-06T10:13:33Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9124
dc.description.abstractThe sedimentary infill of a small continental basin and the processes involved in its transformation into an erosionaI basin have been studied. The Otíñar basin is a fluvio-lacustrine basin developed during the Quaternary (?) on the Subbetic rocks at the south of Jaén city. Its sedimentary infill is made up of three stratigraphic units representing different stages as exorheic and endorheic basin. The destruction of the basin took place when the axial fluvial system base level occupied a relatively lower position and the fluvial system entrenched in the sedimentary infill leaving at least three terraces levels. Climatic and tectonic factors are discussed as controls of the sedimentary and erosional evolution of the Otíñar basinen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherContinental basinen_US
dc.subject.otherFluvio-lacustrine sedimentationten_US
dc.subject.otherBetic Cordillerasen_US
dc.titleRelleno sedimentario y destrucción de una pequeña cuenca fluvio-lacustre en la Sierra Sur de Jaén (Cordilleras Béticas)en_US
dc.titleSedimentary filling and destruction of a small fluvio-lacustrine basin in the Sierra Sur of Jaén (Betic Cordilleras)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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