Project
Tahami Center


Overview
- A significant, large-scale porphyry system identified with a 2.0 km × 1.4 km footprint.
- Features a high-sulfidation system at surface, defined by a preserved lithocap with advanced argillic alteration (alunite-pyrophyllite).
- Confirmed potassic (biotite-magnetite), quartz-sericitic and advanced argillic alteration zones, plus a full porphyry veinlet sequence (A, M, EB, B, D).
- Visible Cu-Mo-Au mineralization (chalcopyrite, molybdenite) confirmed at surface, with preliminary channels up to 2.10 m @ 0.12% Cu, 301 ppm Mo, 0.10 g/t Au.
- High-resolution LiDAR confirms key structural controls and large circular anomalies interpreted as possible porphyry “centers”.
- Active artisanal gold workings located within the system’s footprint, confirming near-surface gold mineralization.