Díaz Azpiroz, ManuelCastro Dorado, AntonioFernández Rodríguez, Carlos2014-12-112014-12-112001http://hdl.handle.net/10272/9513Several 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 eventspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Iberian MassifMetaluminous graniteMultielement diagramTectono-magmatic discrimination diagramjournal articleopen access