@article{10272/12408,
year = {1996},
url = {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)},
publisher = {Sociedad Geológica de España},
title = {Tipología del plutón de Campanario-La Haba: implicaciones petrogenéticas},
title = {Campanario-La Haba pluton tipology: petrogenetic implications},
author = {Alonso Olazabal, Ainhoa and Aranguren, A. and Carracedo Sánchez, Manuel and Larrea Bilbao, F. J.},
}