| Geological Assessment |
The team documented geological indicators of hydrothermal activity, including quartz-vein systems, altered host rocks, and sulfide oxidation textures. Remote sensing further supported our findings, revealing alteration signatures that matched mapped structural corridors. Geochemical sampling showed mostly background levels, but some samples exhibited significant gold, silver, and copper anomalies. These findings highlight a focused mineralized system that merits further exploration, while other areas remained at background levels. geochemical characteristics, helping us refine priorities and optimize future resource allocation. |