Burgunda is a structurally controlled gold-silver deposit located within the western Tien Shan belt of northern Tajikistan. The deposit was historically classified by Soviet geologists as a steeply dipping epithermal sulphide-vein system and comprises multiple mineralised bodies hosted within faulted volcanic and sedimentary sequences.

Gold mineralisation is associated with northeast-striking fault systems and occurs in quartz-sulphide veins and mineralised shear zones. Importantly, the principal veins are surrounded by broader halos of disseminated mineralisation in the wall rocks, presenting potential for additional resource upside beyond the historically defined high-grade structures.

Both open pit and underground development have been undertaken historically, and the project benefits from established access and proximity to the Kansai processing facility. Mineral inventory estimates are based largely on Soviet-era data, supplemented by more recent reinterpretation and modelling. These estimates are currently regarded as non-JORC compliant and are expressed as mineralised inventory ranges pending full validation.

Future work at Burgunda will focus on confirmation drilling, improved geological modelling and testing of the broader disseminated zones. The combination of structurally controlled high-grade veins and potential bulk-tonnage targets provides a balanced exploration and production profile within the portfolio.