Boevskite, Pb<sub>4</sub>(TeO<sub>3</sub>)<sub>2</sub>(SO<sub>4</sub>)(S<sub>2</sub>O<sub>3</sub>), the first mixed sulfate–thiosulfate mineral from the Boevskoe deposit, Southern Urals, Russia

The new mineral boevskite Pb 4 (TeO 3 ) 2 (SO 4 )(S 2 O 3 ) was found at the Boevskoe W-Be deposit, Chelyabinsk Oblast, Southern Urals, Russia.It occurs as very rare 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.Other associated minerals include anglesite, cerussite, chalcopyrite, empressite, hessite, ingodite, josite-B, matildite and pyrrhotite.Boevskite is colourless and transparent with an adamantine lustre.It is brittle, with uneven fracture.No cleavage or parting are observed.The Vickers' micro-indentation hardness (VHN, 10 g load) is 110 kg/mm 2 , corresponding to a Mohs' hardness of 2.5-3.D calc.= 6.599 g/cm 3 .Boevskite is optically biaxial, colourless and nonpleochroic.The mean refractive index calculated using the Gladstone-Dale equation is 2.08.The empirical formula

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Publication Details

Journal
Mineralogical Magazine
Published
2025-09-19
DOI
https://doi.org/10.1180/mgm.2025.10143
Primary Topic
Crystal Structures and Properties
Type
article
Field-Weighted Citation Impact
0.00

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article

Boevskite, Pb4(TeO3)2(SO4)(S2O3), the first mixed sulfate–thiosulfate mineral from the Boevskoe deposit, Southern Urals, Russia

Cristian Biagioni, Natalia V. Zubkova, Anatoly V. Kasatkin, Fabrizio Nestola et al.
Mineralogical Magazine
Crystal Structures and Properties
article

Boevskite, Pb4(TeO3)2(SO4)(S2O3), the first mixed sulfate–thiosulfate mineral from the Boevskoe deposit, Southern Urals, Russia

Cristian Biagioni, Natalia V. Zubkova, Anatoly V. Kasatkin, Fabrizio Nestola, Radek Škoda, Aleksey M. Kuznetsov, Vladislav V. Gurzhiy, Sergey N. Britvin, Jakub Plášil, Atali A. Agakhanov
article en

Abstract

The new mineral boevskite Pb 4 (TeO 3 ) 2 (SO 4 )(S 2 O 3 ) was found at the Boevskoe W-Be deposit, Chelyabinsk Oblast, Southern Urals, Russia.It occurs as very rare 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.Other associated minerals include anglesite, cerussite, chalcopyrite, empressite, hessite, ingodite, josite-B, matildite and pyrrhotite.Boevskite is colourless and transparent with an adamantine lustre.It is brittle, with uneven fracture.No cleavage or parting are observed.The Vickers' micro-indentation hardness (VHN, 10 g load) is 110 kg/mm 2 , corresponding to a Mohs' hardness of 2.5-3.D calc.= 6.599 g/cm 3 .Boevskite is optically biaxial, colourless and nonpleochroic.The mean refractive index calculated using the Gladstone-Dale equation is 2.08.The empirical formula

Mineralogical Magazine
University of Pisa (IT), Russian Academy of Sciences (RU), University of Padua (IT), St Petersburg University (RU), Lomonosov Moscow State University (RU), Masaryk University (CZ), Institute of Physics (HR), Institute of Physics of the Slovak Academy of Sciences (SK)
University of Cambridge
Openalex Percentile: Top 83%
Crystal Structures and Properties
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