El surco sedimentario de Elkuden (Albiense superior-Cenomaniense inferior, Navarra)
7he Elkuden sedimentary succession comprises mainly silty and marly facies with scarce intercalated calcarenitic gullies and breccias. Integrated fades and biostratigraphic analyses provide the basis for sedimentary environment reconstructions during the late Albian-early Cenomanian. A small sedimen...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2001 |
| 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:10272/9527 |
| Acceso en línea: | http://hdl.handle.net/10272/9527 |
| Access Level: | acceso abierto |
| Palabra clave: | Late Albian Cenomanian Sedimentary trough Tectonic activity Basque-Cantabrian Basin Navarra |
| Sumario: | 7he Elkuden sedimentary succession comprises mainly silty and marly facies with scarce intercalated calcarenitic gullies and breccias. Integrated fades and biostratigraphic analyses provide the basis for sedimentary environment reconstructions during the late Albian-early Cenomanian. A small sedimentary trough (4x1 km.) neighbouring a carbonate platform was formed by synsedimentary activity of the strike-slip Bilbao fault |
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