Herrero, A.2014-10-232014-10-232004http://hdl.handle.net/10272/8960They are defined four sort of associations of fades that are interpreted as fluvial channel landfills: low sinuosity with gravel and sands load, high sinuosity with gravel and sands load. For each one of they are provided their characteristic sedimentologicas. It is analyzed fluvial channel deposit's and the tectonic control of the paleocurrentsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Duero BasinMioceneMansilla FormationFadesFluvial channelTectonic controlSedimentologia e interpretación paieoambiental de los canales fluviales de la Formación Mansilla en el Mioceno de la provincia de LeónSedimentology and interpretation paleoenvironmental of the fluvial channels of the Mansilla Formation in the Miocene of the Leon provincejournal articleopen access