@article{10272/9515,
year = {2001},
url = {http://hdl.handle.net/10272/9515},
abstract = {The 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 alteration},
publisher = {Sociedad Geológica de España},
title = {Caracterización mineralógica y química de la granodiorita de Los Pedroches en la zona de cizalla dúctil de Conquista},
title = {Mineralógica! and chemical features of the Los Pedroches granodiorite in the ductile shear zone of Conquista},
author = {Larrea Bilbao, F. J. and Carracedo Sánchez, Manuel and Tubía, José María and Aranguren, A. and Cuevas, Julia},
}