El paleokarst de Nazaré (Cretácico Superior de la Cuenca Lusitana, Portugal)
In the Nazare region, (west Portuguese coast) there is an exceptionally well exposed paleokarst associated with the Upper Cenomanian carbonate succession and the overlying siliciclastics series of probable Turonian-Campanian age. The progradational trend of this succession as well as its depositiona...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1997 |
| 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:10272/10542 |
| Acceso en línea: | http://hdl.handle.net/10272/10542 |
| Access Level: | acceso abierto |
| Palabra clave: | Paleokarst Stable isotopes Sedimentation Cretaceous Lusitanian Basin |
| Sumario: | In the Nazare region, (west Portuguese coast) there is an exceptionally well exposed paleokarst associated with the Upper Cenomanian carbonate succession and the overlying siliciclastics series of probable Turonian-Campanian age. The progradational trend of this succession as well as its depositional geometries show that sinsedimentary tectonic activity influenced the different diagenetic and paleokarstic features |
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