Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/3196
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dc.creatorMartín Escorza, Carlos-
dc.date2008-03-11T07:22:29Z-
dc.date2008-03-11T07:22:29Z-
dc.date2004-
dc.date.accessioned2017-01-31T01:00:38Z-
dc.date.available2017-01-31T01:00:38Z-
dc.identifierMiscelanea nº 4. Homenaje a E. Aguirre, Vol 1, Geología, 83-91-
dc.identifierhttp://hdl.handle.net/10261/3196-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/3196-
dc.descriptionThe 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.descriptionPeer reviewed-
dc.format1052230 bytes-
dc.formatapplication/pdf-
dc.languagespa-
dc.publisherMadrid (Comunidad Autónoma)-
dc.rightsopenAccess-
dc.subjectArenas eólicas-
dc.subjectHoloceno-
dc.subjectCuenca del Duero-
dc.subjectMeseta Ibérica-
dc.subjectEolic sands-
dc.subjectHolocene-
dc.subjectDuero Basin-
dc.subjectIberian Meseta-
dc.titleDistribución de las arenas eólicas de la Cuenca del Duero (Meseta Ibérica)-
dc.typeArtículo-
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