Evolución paleogeógráfica de la Cuenca Ibérica en el Cretácico Superior
In the Iberian Basin, during Upper Albian - Middle Campanian, several shallow carbonate platforms were developed. These platforms grade landwards, westwards to the Hesperian Massif, to silicidastic, littoral and coastal sediments. Two major depositional megasequences (2nd order) and 12 depositional...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2004 |
| 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:10272/8937 |
| Acceso en línea: | http://hdl.handle.net/10272/8937 |
| Access Level: | acceso abierto |
| Palabra clave: | Palaeogeography Iberian Basin Upper Cretaceous |
| Sumario: | In the Iberian Basin, during Upper Albian - Middle Campanian, several shallow carbonate platforms were developed. These platforms grade landwards, westwards to the Hesperian Massif, to silicidastic, littoral and coastal sediments. Two major depositional megasequences (2nd order) and 12 depositional sequences (3rd order) have been recognized. Detailed paleogeographical maps for the eleven basal depositional sequences are presented in this paper. Temporal ranging of these maps is about 2 My, from Upper Albian (102 My) to Lower Campanian (83 My) |
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