Multiple outcropping mineralised structures with Cu-Pb-Ag epithermal metal zonation evident in the geochemistry.
Multi-element geochemistry from soil, rock chip and RC drill samples demonstrate metal zonation consistent with intermediate to high sulphidation mineralisation, which is consistent with the tectonic setting for Wertago.
Epithermal Cu-Ag mineralisation is controlled by a complex array of structures formed during the Siluro-Devonian extensional tectonics forming the Mt Daubney Basin. The complex fault architecture generally conforms to a Riedel fault system, with the mineralised structures aligning along the NE-oriented R-shears. The potential for shoots to form in dilatant zones at both structural intersection points and jogs within the shears within the 30km long Mt Daubney Basin is considered high.
