Una modificación al modelo genético para la Formación Molicias (Tortoniense superior, Depresión de Guadix, S de España)
The Molicias Formation has traditionally been interpreted as being a basinward prograding, platform-talus-basin system, deposited in a relatively rising-sea-level environment. The proposed modification to this model is that the greater part of the turbidite ar the result of brusque drops in sea leve...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1988 |
| 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:10272/18390 |
| Acceso en línea: | http://hdl.handle.net/10272/18390 |
| Access Level: | acceso abierto |
| Palabra clave: | Bioclastic calcarenites Tortonian Shelf Turbidites |
| Sumario: | The Molicias Formation has traditionally been interpreted as being a basinward prograding, platform-talus-basin system, deposited in a relatively rising-sea-level environment. The proposed modification to this model is that the greater part of the turbidite ar the result of brusque drops in sea level which caused erosion of part of the platform and the consequent redeposition of reworked material within the deeper parts of the basin |
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