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Distribución de las arenas eólicas de la Cuenca del Duero (Meseta Ibérica)

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dc.creator Martín Escorza, Carlos
dc.date 2008-03-11T07:22:29Z
dc.date 2008-03-11T07:22:29Z
dc.date 2004
dc.date.accessioned 2017-01-31T01:00:38Z
dc.date.available 2017-01-31T01:00:38Z
dc.identifier Miscelanea nº 4. Homenaje a E. Aguirre, Vol 1, Geología, 83-91
dc.identifier http://hdl.handle.net/10261/3196
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/3196
dc.description The data on the cartography of the existing eolic sands in the Duero Basin indicate that occupy a great extent from different levels from the north of the Cordillera Central until the Duero River. Their extension is about to the almost 2.000 km2 with a very variable thickness that arrives at least 30 m in some localities. They have been dated as formed from final times of the Upper Pleistocene until the Holocene. In this work is indicated a place (San Miguel del Arroyo) where 1 m of eolic sands covers to visigothic remains.
dc.description Peer reviewed
dc.format 1052230 bytes
dc.format application/pdf
dc.language spa
dc.publisher Madrid (Comunidad Autónoma)
dc.rights openAccess
dc.subject Arenas eólicas
dc.subject Holoceno
dc.subject Cuenca del Duero
dc.subject Meseta Ibérica
dc.subject Eolic sands
dc.subject Holocene
dc.subject Duero Basin
dc.subject Iberian Meseta
dc.title Distribución de las arenas eólicas de la Cuenca del Duero (Meseta Ibérica)
dc.type Artículo


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