The mineralization is structurally controlled, occurring within tensional Riedel-type fractures, shear zones, and veins developed in both intrusive and metamorphic host rocks. These structures acted as conduits for hydrothermal fluids, resulting in the deposition of polymetallic mineral assemblages, including silver-, lead-, zinc-, and copper-bearing phases, commonly associated with quartz veins and zones of hydrothermal alteration.