Evolución del sistema fluvial Jarama-Lozoya-Guadalix durante el Plioceno final y el Cuaternario

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dc.contributor.authorTorres, Trinidad de
dc.contributor.authorCobo, R.
dc.contributor.authorGarcía Alonso, P.
dc.contributor.authorGrün, R.
dc.contributor.authorHoyos, M.
dc.contributor.authorJulià, Ramón
dc.contributor.authorLlamas, J.
dc.contributor.authorSoler, Vicente
dc.date.accessioned2017-06-06T08:56:19Z
dc.date.available2017-06-06T08:56:19Z
dc.date.issued1994
dc.description.abstractThis paper deals with the Jarama-Lozoya-Guadalix fluvial system evolution during the Pliocene and Pleistocene times. Duringt the Upper Pliocene and Lower Pleistocene time the Lozoya river was under incission and fluviokarst regimen; at the Middle Pleistocene beginning time (Cromer) after a local tectonic event, the jarama river shifted northwards and Lozoya river filled the "Huesos" cave with large amounts of mammal remains. Redueña alluvial fans were still active during the Upper Riss time, but because of local titling later became unactiveen_US
dc.identifier.urihttp://hdl.handle.net/10272/13787
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPlioceneen_US
dc.subject.otherPleistoceneen_US
dc.subject.otherNeotectonicsen_US
dc.subject.otherPalaeoenvironmental evolutionen_US
dc.subject.otherFluvialen_US
dc.subject.otherAlluvial fansen_US
dc.titleEvolución del sistema fluvial Jarama-Lozoya-Guadalix durante el Plioceno final y el Cuaternarioen_US
dc.titleUpper Pliocene-Pleistocene evolution of the Jarama-Lozoya-Guadalix fluvial systemeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 17, (1994)