Basin analysis and mineral endowment of the Proterozoic Itajaí Basin, south‐east Brazil

A basin evolution synthesis and an integration of geological and geophysical data, relevant as guides to the exploration of gold and lead–zinc deposits in the Itajaí Basin, are presented in this paper. The Itajaí Basin is interpreted as a collision‐related foreland basin consisting of weakly metamorphosed sediments deposited between the structural front of the Dom Feliciano fold and thrust belt and the proximal flank of the cratonic forebulge. Its sediments represent a second‐order depositional sequence deposited during a foreland transgression–regression cycle related to flexural subsidence. After deposition, the basin underwent a main late‐collisional compressional deformation phase followed by an extensional post‐orogenic relaxation. Known gold and lead–zinc deposits are associated with late‐orogenic faulting of the Itajaí Basin sediments. The gold‐bearing quartz veins are of filonean hydrothermal affiliation, while the lead–zinc deposits were formed by solution‐remobilization in a meteoric–connate–magmatic mineralizing fluid. Major trends of favourability for such deposits are recognized. The most favourable sites for lead–zinc deposits are near known mineralized areas and also along a NE‐orientated fault at the margin adjacent to the Dom Feliciano metamorphic belt. The higher favourability for gold deposits is assigned to an area along the same NE trend, and also around a small known deposit near the cratonic margin.