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Rio Maria granodiorite and associated rocks of Ourilândia do Norte - Carajás province: Petrography, geochemistry and implications for sanukitoid petrogenesis
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文摘

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.

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