@article{10272/9513,
year = {2001},
url = {http://hdl.handle.net/10272/9513},
abstract = {Several late leucogranite small plutons appear in the high grade zone of the continental domain (CD), in the Aracena metamorphic belt (AMB). These leucogranites cross-cut the structures due to the main tectono-metamorphic events. The main ferromagnesian minerals in these granites are clinopiroxene and amphibole, the geochemical patterns are characteristics of metaluminous granites. Multielement and tectono-magmatic discrimination diagrams suggest that these metaluminous granites were intruded in the last stages or after a continental collision event},
publisher = {Sociedad Geológica de España},
title = {Caracterización petrológica y geoquímica de los granitos metaluminosos tardíos del dominio continental de la banda metamorfica de Aracena (Macizo Ibérico meridional)},
title = {Petrological and geochemical characterization of the late metaluminous granites from the continental domain of the Aracena metamorphic belt (southern Iberian Massif)},
author = {Díaz Azpiroz, Manuel and Castro Dorado, Antonio and Fernández Rodríguez, Carlos},
}