Emplazamiento en una zona de cizalla dúctil - frágil transtensiva para el Plutón de Pájara, Fuerteventura, Islas Canarias
The mésostructures within the host-rocks as well as the internal deformation ofthé Pájara Pluton in Fuerteventura, allow the definition of a N 5-15 E directed ductile-brittle transtensive shear-zone, that conditioned the emplacement of the intrusive core represented by this ptutonic body. We ha ve i...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1996 |
| 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:10272/11083 |
| Acceso en línea: | http://hdl.handle.net/10272/11083 |
| Access Level: | acceso abierto |
| Palabra clave: | Ductile-brittle shear-zone Magmatic emplacement Pluton of Pájara Fuerteventura Canary Islands |
| Sumario: | The mésostructures within the host-rocks as well as the internal deformation ofthé Pájara Pluton in Fuerteventura, allow the definition of a N 5-15 E directed ductile-brittle transtensive shear-zone, that conditioned the emplacement of the intrusive core represented by this ptutonic body. We ha ve indirectly estimated an age of 22-21 Aia for this shear-zone, which is considered as coeval to the thermal metamorphism |
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