Estructura profunda de la cuenca de Cameros (Cordillera Ibérica) a partir de datos gravimétricos
The Cameros basin (Iberian Chain) developed under a very subsident extensional regime during the latest Jurassic-early Cretaceous. Its fill constitutes a magasequence o f more than 5000 m of vertical thickness. That would produce a gravity low. Nevertheless, the gravity map of this area draws a grav...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1996 |
| 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:10272/13196 |
| Acceso en línea: | http://hdl.handle.net/10272/13196 |
| Access Level: | acceso abierto |
| Palabra clave: | Gravity data Iberian range Cameros basin |
| Sumario: | The Cameros basin (Iberian Chain) developed under a very subsident extensional regime during the latest Jurassic-early Cretaceous. Its fill constitutes a magasequence o f more than 5000 m of vertical thickness. That would produce a gravity low. Nevertheless, the gravity map of this area draws a gravity high in the eastern part of the basin. We propose an explanation to this contradiction |
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