Relleno de canales abandonados en la Formación Areniscas de Cabrerizos (Eoceno, Salamanca)

Two models of the channels fills deposits we are identified in the Cabrerizos Sandstone Formation (Eoceno), A): Channel fill associated a slowly abandoned of the system and rapid infilling next active channels and B): channel fill associated a swift abandoned and slowly infilling far a active channe...

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Detalhes bibliográficos
Autor: Alonso Gavilán, G.
Formato: artículo
Fecha de publicación:1989
País:España
Recursos:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/18341
Acesso em linha:http://hdl.handle.net/10272/18341
Access Level:acceso abierto
Palavra-chave:Channel fill deposits
Fluvial systems
Duero basin
Eoceno
Descrição
Resumo:Two models of the channels fills deposits we are identified in the Cabrerizos Sandstone Formation (Eoceno), A): Channel fill associated a slowly abandoned of the system and rapid infilling next active channels and B): channel fill associated a swift abandoned and slowly infilling far a active channels