Geology, geochemistry and tectonomagmatic affinities of the granitoid complex from Bannach, Rio Maria Domain, Carajás Metallogenetic Province, Northern Brazil
DOI:
https://doi.org/10.11606/issn.2316-9095.v21-173364Keywords:
Archean, Geochemistry, Granitoids, CarajásAbstract
Bannach northern area is formed by trondhjemites, leucogranodiorites, biotite granodiorites, amphibole bearing tonalites (± quartz diorites), biotite tonalites (enclaves) and fine grained granitoids. The high silica rocks, with > 70% SiO2, are represented by trondhjemites, leucogranodiorites and fine grained granitoids presenting high levels of Al2O3, CaO and Na2O in detriment of Fe2O3, MgO, Ni and Cr. They also present high La/Yb and Gd/Er ratios, absence of negative Eu anomalies and strongly fractionated rare earth elements (REE) patterns. The low-silica granitoids, represented by biotite ranodiorite, amphibole bearing and tonalite enclaves present high content of Fe2O3, MgO, Ni and Y. The biotite granodiorites present high levels of Ba- Sr-K and moderate to high La/Yb ratios, while the others have low La/Yb ratios. The origin of the trondhjemites is attributed to the partial fusion of garnet amphibolites in a subduction environment and the leucogranodiorites have their compositional control associated with different degrees of melting of basalt enriched from the base of the crust. The ambiguous geochemical character of the biotite granodiorites (high content of Rb, Ba, Sr and Y and high La/Y and Sr/Y ratios), approximates them to Closepet-type granites. On the other hand, the less evolved character of the amphibole bearing tonalites, as well as the low La/Yb and Sr/Y ratios indicate that these have mantle affinity, and are probably formed at low depths. It is assumed that the origin of these rocks is related to a metassomatized mantle by slab fluids in a subduction environment.
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