La asociación magmática del batolito de los Pedroches: ensayo de caracterización
A typical granitoid association of the Hercyno-type suite occurs in the los Pedroches batholith, composed mainly of biotite ± amphibole granodiorites, biotîte-cordierite porphyritic monzogranites and cordierite leucogranites, with minor basic rocks. Plotting of major-element chemical data of these t...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1987 |
| 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:10272/18459 |
| Acceso en línea: | http://hdl.handle.net/10272/18459 |
| Access Level: | acceso abierto |
| Palabra clave: | Magmatic series Multicationic diagrams Enclaves Los Pedroches batholith Magmatic association Hercynian belt S-type granitoids I-type granitoids |
| Sumario: | A typical granitoid association of the Hercyno-type suite occurs in the los Pedroches batholith, composed mainly of biotite ± amphibole granodiorites, biotîte-cordierite porphyritic monzogranites and cordierite leucogranites, with minor basic rocks. Plotting of major-element chemical data of these types of rocks on multicationic diagrams (Debon & Le Fort, 1982; Batchelor & Bowden, 1985) indicates a clear distinction of at least two different series throughout the batholith |
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