Fin Resources Limited announced that it recently completed soil geochemical sampling and geological mapping program has confirmed the potential for the McKenzie Springs Project to host Voisey's bay-style Nickel-copper-cobalt sulfide mineralisation. In addition, newly released public domain Electromagnetic (EM) Survey Data has led to a re-interpretation with all other geophysical data along with the recently updated geochemical and geological datasets, yielding priority drill ready targets. Assay results have been received from the recently completed soil geochemical sampling program at McKenzie Springs Project. A total of 735 (minus 1.6mm sieved) soil samples were taken over a 11.5 kilometre strike of the McKenzie Spring intrusion on a 400m by 40m sample spacing. Samples assayed up to 1354ppm Nickel (Ni), 508ppm Copper (Cu), 140ppm Cobalt (Co), 41ppb Palladium (Pd), 39ppb Platinum (Pt), 25ppb Gold (Au) and 460ppb Silver (Ag). Statistical assessment of the soil geochemical data revealed 1) Ni, Cu and Co display a strong correlation; and 2) there is pronounced Ni-Cu-Magnesium-Co- Chromium (+/- Pd, Pt, Ag, Au, Tellurium, Bismuth, Selenium) geochemical association which compares favourably with the geochemical signature of the nearby Savannah Ni-Cu-Co sulfide deposit. The soil sampling identified two continuous to discontinuous belts of soil Ni-Cu-Co anomalism with a combined strike length of 9 kilometres along, or proximal to, the northwest and southeast margins of the mafic-ultramafic intrusion. These two geochemically anomalous belts coincide with lenses of ultramafic rocks (pyroxenite, peridotite) that host disseminated Ni-Cu-Co sulfides (pyrrhotite, pentlandite, chalcopyrite). Past exploration has identified Ni-Cu-Co gossans outcropping along the two belts returning high-grade rock chips of up to 12.8% Cu, 1.92% Ni and 0.17% Co. The two Ni-Cu geochemical belts are considered highly prospective for disseminated and massive Ni-Cu sulfide deposits. McKenzie Springs Project Background: The McKenzie Springs Project (51% interest, earning 70% interest) is located within the East Kimberley Region of Western Australia, 85km north-east of the township of Halls Creek. The Project covers an area of approximately 134km2 with identified nickel, copper, cobalt and graphite occurrences. The East Kimberley region has proven potential for hosting magmatic nickel-copper sulfide and PGM mineralisation. Two significant mineralised bodies have been discovered in this area to date within intrusive complexes of the Halls Creek Orogen. These are the Savannah Nickel-Copper Mine (Mineral Resources as at 30 June 2018 are 13.2 million tonnes at 1.65% Ni, 0.75% Cu and 0.11% Co for 218,300 tons contained nickel, 99,100 tonnes contained copper and 14,900 tons contained cobalt) and the Panton PGM Project (Mineral Resources as at 30 June 2018 are 14.3 million tonnes at 2.19g/t Pt and 2.39g/t Pd for 1.01 million ounces contained platinum and 1.10 million ounces contained palladium), both owned by Panoramic Resources Ltd. and are 9km and 30km away from Fin's McKenzie Springs Project respectively. Mineralisation within the McKenzie Springs Project is associated with the basal contact of mafic-ultramafic rocks in a similar geological setting to Panoramic's Savannah Nickel-Copper Mine. Over 25 gossans have been defined at different stratigraphic levels in the intrusion through the course of exploration, some with a strike length of more than 200m.