Thanks mate. I'm intrigued by this paragraph...
The mineralisation style continues to be hydrothermal and the sulphide mineral assemblage appears the same. This new mineralisation may represent a sulphide-fluid conduit between Onça Preta and the Puma Layered Mafic Ultramafic Complex, which is located 200m north of Onça Preta and interpreted to be the potential source of the hydrothermal nickel sulphide plumbing and an outstanding target for more high-grade mineralisation.
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