Tipología del plutón de Campanario-La Haba: implicaciones petrogenéticas

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Tipologia.pdf (302.86 KB)

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1996

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http://hdl.handle.net/10272/12408

Abstract

The Campanario-La Haba pluton is located in the suothern part of the Central-Iberian Zone. It is a coarse-grained 5 type granitoid with cordierite. Typologicaly, this pluton is a peraluminous granitoid , CCA type. Mineralogy and petrologycally, the Campanario-La Haba pluton is closer to the Central Extremadura Bath olith ( Cabeza de Araya type) than to the granitic unit of the Los Pedrodres Batholith (Sta. Eufemia, El Guijo, Cerro Mogabar, Cardeña)

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Coarse grained peraluminous granitoid; 5 type granitoid ,; CCA type; Petrogenesis

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Geogaceta -- Nº 20-3, (1996)
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