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Climbing sructures generated by surges in carbonated shallow lakes. An example from the upper Oligocene of the Ebro Basin

dc.contributor.authorLuzón, Aránzazu
dc.contributor.authorSoria, Ana Rosa
dc.date.accessioned2015-04-08T12:03:26Z
dc.date.available2015-04-08T12:03:26Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10281
dc.description.abstractDuring the upper Oligocene a carbonated shallow lacustrine system developed in the central sector of the Ebro Basin. The lacustrine system was closely related to alluvial systems spreading from the margins to the centre of the basin. The periods with important surge dynamics in the lacustrine area caused the reworking of the materials deposited in the lake and the creation of sand bars basically formed by climbing structures of different types and scalesen_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.otherClimbing structuresen_US
dc.subject.otherLacustrine systemsen_US
dc.subject.otherUpper Oligoceneen_US
dc.subject.otherEbro Basinen_US
dc.titleDesarrollo de estructuras agradacionales generadas por oleaje en lagos someros carbonatados. Un ejemplo del Oligoceno superior de la Cuenca del Ebroen_US
dc.titleClimbing sructures generated by surges in carbonated shallow lakes. An example from the upper Oligocene of the Ebro Basineng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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