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Geology, petrology and geochronology of the Lago Grande layered complex: Evidence for a PGE-mineralized magmatic suite in the Carajás Mineral Province, Brazil
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文摘

The Lago Grande Complex is a PGE-mineralized layered intrusion.

PGE mineralizations occur in chromitites and associated with base metal sulfides.

U–Pb zircon crystallization age of the layered intrusion is 2722 ± 53 Ma.

Metamorphic alteration is heterogeneous and characterized by an extensive hydration.

2.55 Ga zircon ages suggest the influence of the regional IOCG hydrothermal event.

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