The Padre Paraiso tenements are strategically situated within the Eastern Brazilian Pegmatite Province, closely associated with the Neoproterozoic Araçuaí orogeny. Characterized by granite and sedimentary rocks dating back to the Neoproterozoic era, these regions hold promising potential for mineral exploration. Pegmatite formation, a result of magmatic fluids separating from peraluminous S-type granitoids, is intricately linked to the geological events of the Araçuaí Orogen, offering favorable conditions for valuable resource discovery. Moreover, Padre Paraiso stands within 20km of significant Sigma holdings in underexplored areas with rich artisanal mining history, further enhancing its appeal for exploration upside.

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Exploration:​

Stream sediment campaign planned for Q2/Q3

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Key Milestones:

Widespread pegmatites confirmed. (refer to ASX Announcement) 

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