The Kyzylcheku deposit occurs within a fault-bounded block of Palaeozoic carbonate and volcanic rocks intruded by granitoid bodies, with widespread alteration including silicification, sericitisation and pyritisation.

Two principal styles of mineralisation are recognised. The first comprises gold-bearing quartz-carbonate veins forming the Main Mineralised Zone. The second consists of skarn-hosted, polymetallic sulphide bodies enriched in both gold and silver. This dual-style mineralisation provides a combination of vein-hosted and replacement-style targets within the same structural corridor.

Kyzylcheku has historically been exploited by open pit methods, and modelling indicates multiple mineralised zones of variable thickness and strike length.

The presence of both vein and skarn-hosted mineralisation offers scope for further delineation and potential resource expansion. Future programmes will prioritise data validation, improved geological modelling and targeted drilling to test extensions and better define grade continuity within both mineralisation styles.