Adakitic-like magmatism in western Ossa-Morena Zone (Portugal): Geochemical and isotopic constraints of the Pavia pluton

► Whole rock geochemistry shows that granitic rocks are independent pulses of magma. ► Whole rock isotopic data indicate a similar protolith for all granitic rocks. ► The different granitic phases are similar to Archean TTGs and modern adakites. ► The adakitic-like signature derived AFC of a mantle-derived magma.