Cartografía y petrografía de un sector del sistema filoniano N120-130E asociado al batolito de Los Pedroches (Córdoba, Zona Centro-Ibérica)
The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large granodioritic intrusion and smaller monzogranitic plutons. This batholith is cross cut by a dyke complex of lamprophyres, trachyandesites, dacites, aplites, aplopegmatites, dykes of quartz and rhyolites. This last type of...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2001 |
| 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:10272/9518 |
| Acceso en línea: | http://hdl.handle.net/10272/9518 |
| Access Level: | acceso abierto |
| Palabra clave: | Rhyolite dykes Los Pedroches batholith Central Iberian Zone Late-Hercynian magmatism |
| Sumario: | The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large granodioritic intrusion and smaller monzogranitic plutons. This batholith is cross cut by a dyke complex of lamprophyres, trachyandesites, dacites, aplites, aplopegmatites, dykes of quartz and rhyolites. This last type of rocks has been studied in this paper from the cartographic and petrological point of view, recognizing five different types, according to observed textures |
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