Sedimentología de los materiales terciarios de la cubeta intramontañosa de El Rásilio.(Sierra de Cameros, La Rioja)

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dc.contributor.authorMolinero Huguet, J.
dc.contributor.authorColombo Piñol, Ferrán
dc.date.accessioned2017-03-09T12:09:06Z
dc.date.available2017-03-09T12:09:06Z
dc.date.issued1995
dc.description.abstractEl Rasillo intramountainous basin, with 300 m of minimun thickness of Oligocene-Miocene alluvial sediments, is located in Cameros Mesozoic Unit and next to La Demandai Paleozoic Unit. The sedimentological analysis of the sedimentary rocks allows us to make out four alluvial systems, coming from different source areas during the filling of this basin. No features of synsedimentary tectonics have been found, suggesting that the main allocyclic control, of these alluvial systems was the climateen_US
dc.identifier.urihttp://hdl.handle.net/10272/13438
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.otherCameros Rangeen_US
dc.subject.otherIntramountainous basinen_US
dc.subject.otherOligocene-Mioceneen_US
dc.subject.otherAlluvial fanen_US
dc.titleSedimentología de los materiales terciarios de la cubeta intramontañosa de El Rásilio.(Sierra de Cameros, La Rioja)en_US
dc.titleSédimentology of the Tertiary deposits of the El Rasillo intramountainous basin (Cameros Range, La Rioja)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 19, (1995)