Generaciones de cabalgamientos y pliegues recumbentes en los Mantos Alpujárrides entre Ronda y Almería, Cordilleras Béticas
Synmetamorphic thrust nappes, related to the Los Reales Crustal Thrust within the Alpujarride Nappes, moved in an ENE or NE direction. A subsequent movement took place in a northerly direction and large fold nappes were formed. Finally N and NW brittle thrusting occurred, consistent with the Gibralt...
| Autores: | , , , , |
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| Formato: | artículo |
| Fecha de publicación: | 1987 |
| 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:10272/18456 |
| Acesso em linha: | http://hdl.handle.net/10272/18456 |
| Access Level: | acceso abierto |
| Palavra-chave: | Thrust nappes Fold nappes Shear zone Alpine belts Betic Cordilleras |
| Resumo: | Synmetamorphic thrust nappes, related to the Los Reales Crustal Thrust within the Alpujarride Nappes, moved in an ENE or NE direction. A subsequent movement took place in a northerly direction and large fold nappes were formed. Finally N and NW brittle thrusting occurred, consistent with the Gibraltar Crustal Thrust and the N-S convergence of Iberia and Africa |
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