GoldHaven Resources Corp. announced that assay results from the Three Guardsmen property have confirmed the presence of high-grade surface copper mineralisation on its 100% owned property located in Northern British Columbia. 126 surface rock samples collected, including 25 samples exceeding 10,000 ppm (1% Cu).
High-grade grab samples including: J647161 (15.85% Cu), J647629 (12.75% Cu) and J647753 (12.65 % Cu). The Three Guardsmen Project hosts high-grade copper mineralization in epidote?magnetite skarns, with extensive malachite-stained pods traced over more than 1 km of strike. Porphyritic intrusive textures with associated elevated Cu and Mo values have been identified at low elevations in the valley bottom, possibly indicative of an intrusive source for the skarn mineralization.
Geochemical transitions across the property (Cu?Ag ? Bi?Te?Au ? Mo) suggest a vector towards an intrusive heat source underlying the skarn system.
The Three Guardsmen property comprises 14 contiguous mineral tenures covering 16,234 hectares within the Atlin Mining Division of northwestern British Columbia. The claims are 100% owned by GoldHaven Resources Corp. Strategically located near Haines Junction, the Three Guardsmen Project sits in a highly prospective geological area known for copper-magnetite skarns with associated gold and molybdenum mineralization.
Observed transitions from copper- and silver-rich zones to bismuth, tellurium, and gold-rich areas, along with molybdenum in altered granites, suggest a possible nearby porphyry system. Importantly, the presence of altered granites carrying molybdenum?along with systematic geochemical transitions from Cu-Ag zones into Bi-Te-Au enrichment?suggests the presence of a nearby porphyry intrusion driving the metal system. The project lies within a Late Cretaceous tectonic setting that hosts several world-class porphyry deposits, including Casino and Red Mountain, further underscoring the exploration potential.
GoldHaven?s ongoing exploration strategy includes targeted geochemical surveys, structural mapping, and geophysical interpretation aimed at defining potential mineralized granitic intrusive centres.
