Depósitos cuaternarios en el Bajo Ebro: características estratigráficas y deposicíonales

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dc.contributor.authorArasaTuliesa, A.
dc.date.accessioned2017-07-26T10:19:28Z
dc.date.available2017-07-26T10:19:28Z
dc.date.issued1994
dc.description.abstractIn the Bajo Ebro quaternary deposits different lithostratigraphic units are distinguished. Fluvial facies with tabular character: Ford Gravels, Colada Sandstones and Aldover Poligenic Gravels all with siliceous elastics. Alluvial facies with calcareous elastics: the Aldover Monogenic Gravels. These units are attributed to the lower and middle Quaternary. Other units that constitutes fluvial terraces, whith calcareous monogenic elastics are differenciated by their textural character: Xerta Blocks, Llop Gravels and the Assud Sands; these units are attributed to the Thyrrhenian. The fluvial river basin is filled with the Ebro Muds attributed to Holocenees_ES
dc.identifier.urihttp://hdl.handle.net/10272/13986
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherLower and Middle Quaternaryes_ES
dc.subject.otherThyrrhenianes_ES
dc.subject.otherHolocenees_ES
dc.subject.otherBajo Ebroes_ES
dc.subject.otherCataloniaes_ES
dc.subject.otherNE Spaines_ES
dc.titleDepósitos cuaternarios en el Bajo Ebro: características estratigráficas y deposicíonaleses_ES
dc.titleQuaternary deposits in the Bajo Ebro: stratigraphic and depositional characteristicseng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 15, (1993)