Resumen de Sedimentología e interpretación paleoambiental de los canales fluviales de la Formación Mansilla en el Mioceno de la provincia de León
They are defined four sort of associations of facies 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 sedimentológicas. It is analyzed fluvial channel deposits and the tectonic control of the paleocurrents.
