The mapping units comprise intercalations of quartzites and phyllites of Traíras Fm.–Araí Group.
The structures comprise two deformational phases, each subdivided in two stages.
The formation of the three different vein types comprises distinct structural mechanisms.
The ore deposition is controlled by structures and chemical interaction with phyllites.
The Buracão area is an orogenic gold occurrence developed during Brasiliano–Pan African Orogeny.