Peru 0009
Peru 0009: A High-Potential Epithermal System in Huancavelica
Located in the prolific Miocene belt of the Huancavelica region, Peru 0009 spans 500 hectares of highly prospective ground.
This property hosts a deeply eroded high-sulfidation (HS) epithermal system, with remnants of silica ledges indicating strong mineralization. Localized zones exhibit intense quartz-sericite-tourmaline alteration, pointing to significant hydrothermal activity.
Additionally, sheeted and stockworked Mo-bearing B- and Maricunga-type veinlets highlight the potential for further discovery within this dynamic mineralizing system.
