English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/82715
Share/Impact:
Statistics
logo share SHARE   Add this article to your Mendeley library MendeleyBASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:
Title

Cronoestratigrafía de los registros aluviales del tránsito Pleistoceno superior-Holoceno en la depresión de la Bardena Blanca (Navarra).

AuthorsMuñoz, Arsenio; Sancho, Carlos; Peña, José Luis; Benito, Gerardo ; Rhodes, Edward J.; McDonald, E.; Longares, L. A.
Issue Date2006
CitationGeogaceta, (40):263- 266 (2006)
AbstractIn this work, preliminary chronostratigaphic features of the Upper Pleistocene-Holocene morphosedimentary alluvial unit covering the bottom of the Bardena Blanca depression are described. This unit is made up by 1) gravels and sands related to a braided channel system, 2) laminated sands and clays accumulated in distal flats of alluvial fans and 3) clays and gypsums corresponding to a playa-lake environment. According the first chronological data supplied by OSL and 14C the age of this sequence ranges between 18 and 5 ka. The prevailed paleoclimatic conditions were cold and humid during Last Glacial Maximum-Oldest Dryas and arid during Lower Holocene.
URIhttp://hdl.handle.net/10261/82715
Identifiersissn: 0213-683X
Appears in Collections:(MNCN) Artículos
Files in This Item:
File Description SizeFormat 
405735.pdf273,91 kBUnknownView/Open
Show full item record
 


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.