Estructura en escamas del sector noroccidental de la Sierra de Cazorla (zona prebética) y del borde de la depresión del Guadalquivir (provincia de Jaén)
The succession of different stages of deformation, the last of them having taken place in the middle Miocene, has determined the imbricated structure of the Sierra de Cazorla and the easternmost boundary of the Guadalquivir Basin. The evolution of the structural features is analyzed and a tectonic i...
| Autores: | , |
|---|---|
| Tipo de documento: | artigo |
| Data de publicação: | 1970 |
| País: | España |
| Recursos: | Universidad Complutense de Madrid (UCM) |
| Repositório: | Docta Complutense |
| Idioma: | espanhol |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/64542 |
| Acesso em linha: | https://hdl.handle.net/20.500.14352/64542 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Tectónica regional Prebético Cuenca del Guadalquivir Geología estratigráfica Geodinámica 2506.19 Estratigrafía 2507 Geofísica |
| Resumo: | The succession of different stages of deformation, the last of them having taken place in the middle Miocene, has determined the imbricated structure of the Sierra de Cazorla and the easternmost boundary of the Guadalquivir Basin. The evolution of the structural features is analyzed and a tectonic interpretation of the resulting structure is attempted. |
|---|