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The Chapada Cu-Au deposit, Mara Rosa magmatic arc, Central Brazil: Constraints on the metallogenesis of a Neoproterozoic large porphyry-type deposit
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文摘

We propose a two-stage genetic model for the Chapada deposit: an early porphyry Cu-Au and shear zone-hosted Cu-Au events;

The Chapada Cu–Au deposit is an example of a metamorphosed Porphyry-type copper–gold deposit of Neoproterozoic age;

Kyanite-rich rocks are interpreted as products of metamorphosed argillic hydrothermal alteration halo.

Sulfide δ34S values indicate that both mineralization stages were generated by sulfur of magmatic composition.

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