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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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1989 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18341 |
| Acceso en línea: | http://hdl.handle.net/10272/18341 |
| Access Level: | acceso abierto |
| Palabra clave: | Channel fill deposits Fluvial systems Duero basin Eoceno |
| Sumario: | 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 |
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