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Depositional style variations in the alluvial Scala Dei Group, Ebro Basin (Tarragona and Lleida provinces):Characteristics and sedimentological significance

dc.contributor.authorPérez Lacunza, E.
dc.contributor.authorColombo Piñol, Ferrán
dc.date.accessioned2015-01-28T10:15:46Z
dc.date.available2015-01-28T10:15:46Z
dc.date.issued2001
dc.identifier.urihttp://hdl.handle.net/10272/9751
dc.description.abstractThe Scala Dei Croup, which is composed mainly of conglomerates, is located in the SE sector of the Ebro Basin. Many alluvial fans were developed in this area during the Eocene-Oligocene time span. The clastic materials were transported and accumulated by hydraulic currents in braided-style rivers. However, there is a conglomeratic lithosome with a characteristic medium angle cross bedding continuous from the basal scar up to the medial part of the body. This is interpreted as a deposited in a sinuous channel with characteristics of coarse-grained meandering, and represents an important variation in depositional style. These variations can be associated with the a real shifting of the technically active basin borderen_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.otherAlluvial fansen_US
dc.subject.otherBraided riversen_US
dc.subject.otherCoarse-grained meandering riversen_US
dc.subject.otherEbro Basinen_US
dc.titleVariaciones del estilo deposicional en el grupo aluvial Scala Dei, Cuenca del Ebro (Provincias de Tarragona y Lleida): Características y significado sedimentológicoen_US
dc.titleDepositional style variations in the alluvial Scala Dei Group, Ebro Basin (Tarragona and Lleida provinces):Characteristics and sedimentological significanceeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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