La asociación magmática del batolito de los Pedroches: ensayo de caracterización59-61
- Antonio García Casco 1
- Emilio Pascual Martínez 1
- A. Castro 1
- 1 Universidad de Sevilla. Sección de Geología de La Rábida. Palos de la Frontera.Huelva.
ISSN: 0213-683X
Année de publication: 1987
Número: 2
Pages: 59-61
Type: Article
D'autres publications dans: Geogaceta
Résumé
A typical gianitoid association of the Hercyno-type suite occurs in the los Pedroches batholith, composed mainly of biotite ± amphibole granodiorites, biotite-cordierite porphyri tic monzogranites and cordierite leucogranites, with minar basic rocks. Plotting of major-element chemical data of these types of rocks on multicationic diagrams (Deban & Le Fort, 1982; Batchelor & Bowden, 1985) indicates a c/ear distinction of at /east two different series throughout the batholith