El complejo deltaico de Sant Llorenç del Munt (Eoceno del borde suroriental de la depresión del Ebro)
St. Llorenç del Munt fan delta is situated in the Northeast of the Ebre basin. Three main stratigraphic units, equivalent to depositional sequences are distinguished and plotted in figure 2. In proximal fan delta areas these units are separated by erosive unconformities. In distal areas carbonate pl...
| Autores: | , |
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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:10272/18296 |
| Acceso en línea: | http://hdl.handle.net/10272/18296 |
| Access Level: | acceso abierto |
| Palabra clave: | Fan delta Eocene Ebro basin |
| Sumario: | St. Llorenç del Munt fan delta is situated in the Northeast of the Ebre basin. Three main stratigraphic units, equivalent to depositional sequences are distinguished and plotted in figure 2. In proximal fan delta areas these units are separated by erosive unconformities. In distal areas carbonate platforms which represent a maximum highstand sea level, exist between them. Sedimentary instabilities, which have an effect moreover on delta front and upper prodelta, have been found in Middle Fan delta unit |
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