Ikkizelon is an underground gold-silver vein system situated within the mineral-rich Tien Shan belt of northern Tajikistan. The deposit comprises four principal north-westerly striking, steeply dipping vein systems developed along a major fault corridor between two regional fault structures.

Mineralisation is hosted in Palaeozoic volcanic and sedimentary rocks intruded by diorite dykes, with sulphide-bearing quartz veins carrying the majority of the gold and silver values. Historic Soviet exploration defined the main vein system as containing the majority of the mineralised material, and more recent modelling suggests the system remains open at depth.

Ikkizelon has historically been mined by underground methods, targeting high-grade vein material.

The deposit’s structural continuity, high-grade character and depth potential make Ikkizelon a strategically important asset. Planned work includes underground mapping, data verification and targeted drilling to test down-dip extensions and support the future declaration of compliant mineral resources.