Abstract
The composition of galkhaite from the Gal-Khaya deposit (Yakutia, Russia) and Chauvay Mine (Kyrgyzstan) has been examined by electron microprobe. A significant Cs content (up to 6.64 wt %) has been established in the mineral from both deposits; earlier, it had been not detected by either chemical or spectral analyses. The empirical formulas of galkhaite are (Hg4.89Cu0.92Zn0.07)5.88(Cs0.71Tl0.17)0.88(As3.98Sb0.17)4.15 S12.10 and (Hg4.64Cu0.98Zn0.34)5.96 (Cs0.85Tl0.04)0.89(As3.68Sb0.42)4.10S12.05 at the Gal-Khaya deposit and Chauvay Mine, respectively. The crystal structure of galkhaite from the Chauvay Mine (cubic, I43m, a = 10.4144(1) Å, V = 1129.5(2) Å3, Z = 2) for the composition [Hg4.83(Cu,Zn)0.98□](Cs0.71Tl0.14□) (As3.44Sb0.56)S12 has been determined by direct methods and refined to R = 0.0203. The structure of galkhaite is a framework consisting of vertex-shared [(Hg,Cu)-S4 2.5068(3) Å] tetrahedrons of the same orientation as large cavities formed in the initial sphalerite structural type due to eight anion vacancies: two [S4]-tetrahedrons at the point of origin and at the center of the I-cell and 12 cation vacancies as 2 cation octahedrons around the 000 and \( {\raise0.5ex\hbox{$\scriptstyle 1$} \kern-0.1em/\kern-0.15em \lower0.25ex\hbox{$\scriptstyle 2$}}{\raise0.5ex\hbox{$\scriptstyle 1$} \kern-0.1em/\kern-0.15em \lower0.25ex\hbox{$\scriptstyle 2$}}{\raise0.5ex\hbox{$\scriptstyle 1$} \kern-0.1em/\kern-0.15em \lower0.25ex\hbox{$\scriptstyle 2$}} \) sites.
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Original Russian Text © V.I. Vasil’ev, N.V. Pervukhina, S.V. Borisov, S.A. Magarill, 2009, published in Zapiski RMO (Proceedings of the Russian Mineralogical Society), 2009, No. 2, pp. 83–91.
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Vasil’ev, V.I., Pervukhina, N.V., Borisov, S.V. et al. New data on the composition and crystal structure of galkhaite (Hg,Cu)6(Cs,Tl)(As,Sb)4S12 . Geol. Ore Deposits 52, 662–668 (2010). https://doi.org/10.1134/S1075701510070196
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DOI: https://doi.org/10.1134/S1075701510070196