Sedimentologia e interpretación paieoambiental de los canales fluviales de la Formación Mansilla en el Mioceno de la provincia de León
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Abstract
They 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 paleocurrents
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