In Ourilândia do Norte area are quartz-monzodiorites, tonalites and granodiorites, which have sanukitoid signature.
Besides, enclaves and (quartz) diorites that show BADR signature.
They are spatially and temporally associated and they were metasomatized by TTG-like melt and aqueous fluid, respectively.
Such contemporaneous and different geochemistry signatures suggest that they were generated during an active subduction.