La zona de falla de Torres Cartas, conjunto de fallas normales de bajo ángulo entre Nevado-Filábrides y Alpujárrides (Sierra Alhamilla, Béticas Orientales)
The Torres Cartas Fault Zone is a large low-angle extensional structure, strongly thinning the Nevado-Filabride and Alpujarride nappes. These nappe complexes form the basement of the Alboran sea southwest Sierra Alhamilla. The fault zone, being already probably active in Burdigalian times, was folde...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 1986 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18499 |
| Acesso em linha: | http://hdl.handle.net/10272/18499 |
| Access Level: | acceso abierto |
| Palavra-chave: | Extensional structure Nappes Betic Cordilleras |
| Resumo: | The Torres Cartas Fault Zone is a large low-angle extensional structure, strongly thinning the Nevado-Filabride and Alpujarride nappes. These nappe complexes form the basement of the Alboran sea southwest Sierra Alhamilla. The fault zone, being already probably active in Burdigalian times, was folded during the Upper Miocene |
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