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Peako’s East Kimberley Tenement Package is located in the Halls Creek Orogen near the southern margin of the Kimberley Basin in Western Australia.
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Peako’s tenements host a diverse Palaeoproterozoic succession that is widely intruded by multiple granitoid phases and deformed by multiple orogenic episodes. The area represents the western-most window of the Halls Creek Orogen, where volcanic successions of the bimodal Koongie Park Formation Volcanic Belt(c. 1845 Ma) and the Lamboo Ultramafic Intrusive Belt (c. 1850-1835 Ma) are well developed.
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The geological diversity within Peako’s tenement package has driven the search for a wide range of commodities, with the Koongie Park Formation having demonstrated prospectivity for base (Cu-Pb-Zn) and precious (Ag, Au) metals mineralisation, whilst the Lamboo Ultramafic belt has demonstrated prospectivity for base (Ni, Cu) and precious metal (Au, PGE and REE) mineralisation.

Peako’s flagship project is the Eastman PGE project which lies within a large under explored intrusive complex that Peako considers prospective for a major PGE resource. The Eastman Intrusive Complex is located within the Central Zone of the Halls Creek Oregon, where an array of mineralised layered mafic-ultramafic intrusive complexes are defined with an established mineral endowment. Known endowment from layered intrusions in the Halls Creek Oregon includes:


Savannah – Ni-Cu 13.5Mt resource @ 1.56% Ni, 0.7%Cu, 0.1% Co

Copernicus – Ni-Cu 0.825 Mt @ 1.24% Ni, 0.81% Cu