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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

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.