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 |
|