The Junction is where the major fluid pathways, the Negri Fault and the Osmond Fault Zone, meet creating ideal areas for the magmatic and hydrothermal fluid flow. Coincident gravity and magnetic anomalies associated at the junction mapped mantle derived rocks (Woodward Dolerite) indicating a favourable tectono-magmatic environment for Ni-Cu-PGE.
Dolerite units have been mapped in the area as magmatic fluids preferentially intruded at the intersection of these structures. Ground gravity and detailed EM will be completed along the Negri Fault corridor as a priority to refine existing targets & delineate additional targets.