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Guadalete river paleochannel characterization and evolution in the Bay of Cádiz during the late quaternary

dc.contributor.authorLlave, Estefanía
dc.contributor.authorHernández Molina, F. Javier
dc.contributor.authorAlonso, C.
dc.contributor.authorGallardo, M.
dc.contributor.authorVázquez Garrido, Juan Tomás
dc.contributor.authorLópez Aguayo, F.
dc.description.abstractLate Quaternary paleochannel and fluvial deposits characterization in the Bay of Cadiz have been carried out by geophysical, cores, and archeological data. They are located over alluvial deposits of regressive and lowstands systems tracts, and below the coastal deposits of transgressive systems tracts belong to the last depositional sequence. Paleochannels were generated during the sea level fall and lowstand position in the last glaciation stage, but fluvial sedimentary infill was produced after, as the sea level rose, during the transgression. Paleochannel and fluvial deposits have been also affected by several tectonic episodes which influence its position, internal structure and lateral movement, during and after its sedimentationen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherSeismic stratigraphyen_US
dc.subject.otherLate Pleistocene-Holoceneen_US
dc.subject.otherMorphosedimentary evolutionen_US
dc.subject.otherBay of Cadizen_US
dc.titleCaracterización y evolución del paleocauce del río Guadalete en la bahía de Cádiz durante el cuaternario terminalen_US
dc.titleGuadalete river paleochannel characterization and evolution in the Bay of Cádiz during the late quaternaryeng

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Atribución-NoComercial-SinDerivadas 3.0 España
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