Boevskite

boevskite

empressite

ingodite

matildite

Images

Formula: Pb4(TeO3)2(SO4)(S2O3)
Valence: Pb2+4(Te4+O3)2(S6+O4)(S6+O3S2-)
Thiosulphate, tellurium-bearing mineral
Crystal system: Orthorhombic
Specific gravity: 6.599 calculated
Hardness: 2½ to 3
Streak: White
Colour: Colourless
Luminescence: No fluorescence under UV
Environments

Hydrothermal environments

Boevskite is a new mineral, approved in 2024 and to date (January 2026) reported only from thr type locality.

Localities

At the type locality, the Boevskoe Be deposit, Kaslinsky District, Chelyabinsk Oblast, Russia, boevskite was found as euhedral grains up to 0.25 mm at the contact of galena and pyrite, as inclusions in galena up to 0.2 mm, and as thin veinlets up to 0.2 × 0.03 mm filling cracks in sphalerite. The presence of sulphides in the ores of the deposit along with fluorite led to the formation of sulphuric and hydrofluoric acids in the oxidation zone and the active development of supergene processes to a depth of 100 meters. The boevskite was formed as a result of the supergene alteration of the co-existing galena and tellurides (empressite, hessite, ingodite and joséite-B) in the oxidation zone. Associated minerals include anglesite, cerussite, chalcopyrite, empressite, galena, hessite, ingodite, joséite-B, matildite, pyrite, pyrrhotite and sphalerite (Mindat).

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