La zona de cizalla del contacto entre el grupo de mantos del Mulhacén y la unidad del Veleta (Sierra Nevada y Sierra de los Filabres, Andalucía)
The existence of an important ductil shear-zone developed in relation with the emplacement of the Mulhacen nappes group on the Veleta Unit (Betic Cordilleras) is manifested. The overlaping in the ENE sense is over 200 km implying that most of the shortening in the Nevado Filabride occurred irrespect...
| Autores: | , , , |
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| Tipo de documento: | artigo |
| Data de publicação: | 1986 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositório: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | espanhol |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18498 |
| Acesso em linha: | http://hdl.handle.net/10272/18498 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Ductil shear Nappes Betic Cordilleras |
| Resumo: | The existence of an important ductil shear-zone developed in relation with the emplacement of the Mulhacen nappes group on the Veleta Unit (Betic Cordilleras) is manifested. The overlaping in the ENE sense is over 200 km implying that most of the shortening in the Nevado Filabride occurred irrespectively of the convergence between Africa and Europe |
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