Larrea Bilbao, F. J.Carracedo Sánchez, ManuelTubía, José MaríaAranguren, A.Cuevas, Julia2014-12-112014-12-112001http://hdl.handle.net/10272/9515The northern edge of Los Pedroches granodioritic pluton is deformed by the Conquista fault, a right ductile shear zone with a normal component. Consecuently, the rocks of this sector show gradual texture-structural modifications, without any differences in their modal mineralogy. Chemically, the minimal variations observed, instead of the deformation are a cause of the diferentiation by fractional crystallization, of plagioclase, biotite, amphibole, apatite and ilmenite. The high-temperature deformational processes -near to the magmatic solidus- observed in the Los Pedroches granodiorite, have not related any significant chemical alterationspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Chemical variationHigh-temperature deformationLos Pedroches granodioritic plutonjournal articleopen access