Fallas normales de bajo ángulo a gran escala en las Béticas occidentales
Low angle normal faults (LANF) related with extensional detachments are mapped in the Western Betics. They developed during the Middle and Late Miocene on continental crust which was previously thickened by fold- and thrust-nappes and the Gibraltar Crustal Thrust. The LANF thinned the basement of th...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1990 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18107 |
| Acceso en línea: | http://hdl.handle.net/10272/18107 |
| Access Level: | acceso abierto |
| Palabra clave: | Low angle normal fault Detachment Crustal thinning Betics |
| Sumario: | Low angle normal faults (LANF) related with extensional detachments are mapped in the Western Betics. They developed during the Middle and Late Miocene on continental crust which was previously thickened by fold- and thrust-nappes and the Gibraltar Crustal Thrust. The LANF thinned the basement of the Alborán basin. Superimposed folds and strike-slip faults have modified the geometry of the extensional system |
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