Go Metals Corp. announced results from the HSP project, a polymetallic property with nickel, copper, and PGE mineralization in eastern Quebec. Highlights: 4 New nickel-copper showings discovered, Grab samples with up to 1.78% Ni and 3.97% Cu, Program showcases accuracy of the GeoDL artificial intelligence engine, Average Nickel equivalent of 0.54% over 25 samples, Anomalous to enriched cobalt, gold, silver, platinum, palladium and 50 new HSP claims staked to increase total land package to 8,250 Hectares. Geological context: The HSP property is in the Quebec Havre St. Pierre Anorthosite Complex. All showings but the Gem showings are in structurally controlled semi- to massive sulphides in mafic- to ultramafic units that occur on the edge of the anorthosite complex. The PGE Zone is characterized by massive to semi massive sulphides adjacent to ultramafic pyroxenite dykes and typically has higher PGE concentrations. The Chamber Zone is characterized by large pods of massive pyrrhotite and chalcopyrite within EM anomalies up to 400m wide at surface. These are interpreted as potential pockets or irregularities in the magma chamber where immiscible sulphide rich melt accumulated within the anorthosite complex. The Red Mountain showing exhibits traits of both the PGE and the chamber zones. It is characterized by a large body of massive sulphides but also seems to be related to adjacent pyroxenite dykes. The Gem showing overlies a magnetic high interpreted as a possible magmatic conduit within the anorthosite complex.