La asociación magmática del batolito de los Pedroches: ensayo de caracterización59-61

  1. Antonio García Casco 1
  2. Emilio Pascual Martínez 1
  3. A. Castro 1
  1. 1 Universidad de Sevilla. Sección de Geología de La Rábida. Palos de la Frontera.Huelva.
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1987

Issue: 2

Pages: 59-61

Type: Article

DIALNET GOOGLE SCHOLAR lock_openOpen access editor

More publications in: Geogaceta

Abstract

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

Data source: Dialnet