Year: 2026
Pages: 193–204
UDC: 549.334; 549.086
Number: 2
Type: scientific article
Topic: Petrology, mineralogy, geochemistry, isotope geology
Authors: Chumakov Aleksandr V., Leibham Polina N., Saveliev, Dmitry E., Alikin Oleg V., Rudashevsky Vladimir N.
This article presents, for the first time, the results of a detailed study of telluride mineralisation in ores from a gold-sulphide deposit in the Middle Urals. The study was carried out on a representative composite sample using a combined methodology involving electric pulse disaggregation, hydroseparation and scanning electron microscopy with energy-dispersive microanalysis. During the work, seven tellurium-bearing mineral phases were identified: melonite (NiTe2), colarite (PbTeCl2), altaite (PbTe), tellurobismuthite (Bi2Te3), tellurium-bearing galena (Pb(S, Te)), coloradoite (HgTe) and calaverite (AuTe2). The mineral balance revealed an anomalous predominance of melonite, accounting for 78.45% of the total tellurides. The telluride inclusions are micrometre in size (4–100 µm) and are predominantly associated with pyrite, sulphide grain boundaries and quartz-carbonate veins, which indicates their formation during the final stages of ore formation. Geochemical analysis revealed a consistent association of Te with Ni, Pb and Zn, whereas Au and As demonstrate relative independence, indicating a multi-stage nature of mineralisation. The application of a combined sample preparation technique ensured a statistically representative sample of heavy minerals without over-grinding or contamination.
telluride mineralisation; gold-sulphide deposit; tellurides; micromineralogy; electric pulse disaggregation; hydroseparation