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

• Antonio García Casco ^[1] ; Emilio Pascual Martínez ^[1] ; A. Castro ^[1]
  1. [1] Universidad de Sevilla

     Universidad de Sevilla

     Sevilla, España

     
• Localización: Geogaceta, ISSN 0213-683X, Nº. 2, 1987, págs. 59-61
• Idioma: español
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• Resumen

  • 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