Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of movement. Later overturned north-vergent folds and brittle deformations associated...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 1992 |
| 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:10272/16337 |
| Acesso em linha: | http://hdl.handle.net/10272/16337 |
| Access Level: | acceso abierto |
| Palavra-chave: | Betic Cordilleras Extensional tectonic Detachment |
| Resumo: | The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of movement. Later overturned north-vergent folds and brittle deformations associated to normal faults with a top-to-the-westsouthwest sense of movement affect the previous structures. The normal fault (Alcaucm Fault) that separates the Sierra Tejeda Unit (footwall) from the Canillas and Sayalonga Units (hanging wall) is a detachment. Normal faults that separate the different units of the hanging wall joint the detachment and they do not penetrate into the footwall |
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