Alonso Olazabal, AinhoaAranguren, A.Carracedo Sánchez, ManuelLarrea Bilbao, F. J.2016-06-222016-06-221996http://hdl.handle.net/10272/12408The 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)spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Coarse grained peraluminous granitoid5 type granitoid ,CCA typePetrogenesisjournal articleopen access