Tennantite-(Hg), Cu6(Cu4Hg2)As4S13, a new tetrahedrite-group mineral from the Lengenbach quarry, Binn, Switzerland

被引:10
作者
Biagioni, Cristian [1 ]
Sejkora, Jiri [2 ]
Raber, Thomas [3 ]
Roth, Philippe [4 ]
Moelo, Yves [5 ]
Dolnicek, Zdenek [2 ]
Pasero, Marco [1 ]
机构
[1] Univ Pisa, Dipartimento Sci Terra, Via Santa Maria 53, I-56126 Pisa, Italy
[2] Natl Museum, Dept Mineral & Petrol, Cirkusova 1740, Prague 19300 9, Czech Republic
[3] FGL Forschungsgemeinschaft Lengenbach, Edith Stein Str 9, D-79110 Freiburg, Germany
[4] Swiss Fed Inst Technol, FGL Forschungsgemeinschaft Lengenbach, Swiss Seismol Serv, CH-8092 Zurich, Switzerland
[5] Univ Nantes, CNRS, Inst Mat Jean Rouxel, IMN, F-44000 Nantes, France
关键词
tennantite-(Hg); new mineral; sulfosalt; copper; mercury; arsenic; crystal structure; Lengenbach; Binn Valley; Switzerland; LEAD-ANTIMONY SULFOSALTS; CRYSTAL-STRUCTURE; COMPOSITIONAL VARIATION; SYNTHETIC TETRAHEDRITE; SOLID-SOLUTION; CHEMISTRY; VALLEY; SUBSTITUTIONS; ROUTHIERITE; REFINEMENT;
D O I
10.1180/mgm.2021.59
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
Tennantite-(Hg), Cu-6(Cu4Hg2)As4S13, was approved as a new mineral species (IMA2020-063) from the Lengenbach quarry, Imfeld, Binn Valley, Canton Valais, Switzerland. It was identified as an aggregate of black metallic tetrahedral crystals, less than 0.1 mm in size, intimately associated with sinnerite, and grown on realgar. In reflected light, tennantite-(Hg) is isotropic, grey in colour, with creamy tints. Minimum and maximum reflectance data for COM wavelengths in air are [lambda (nm): R (%)]: 470: 29.1; 546: 29.1; 589: 28.5; 650: 27.7. Electron microprobe analysis gave (in wt.% - average of 7 spot analyses): Cu 32.57(42), Ag 6.38(19), Tl 0.29(14), Zn 0.04(5), Hg 17.94(2.27), Pb 0.70(51), As 17.83(61), Sb 0.34(8), S 24.10(41), total 100.19(1.04). The empirical formula of the sample studied, recalculated on the basis of Sigma Me = 16 atoms per formula unit, is (Cu4.69Ag1.04Tl0.03)(Sigma 5.76)(Cu4.35Hg1.58Pb0.06Zn0.01)(Sigma 6.00)(As4.20Sb0.05)(Sigma 4.25)S-13.26. Tennantite-(Hg) is cubic, I (4) over bar 3m, with a = 10.455(7) angstrom, V = 1143(2) angstrom(3) and Z = 2. The crystal structure of tennantite-(Hg) has been refined by single-crystal X-ray diffraction data to a final R-1 = 0.0897 on the basis of 214 unique reflections with F-o > 4 sigma(F-o) and 22 refined parameters. Tennantite-(Hg) is isotypic with other members of the tetrahedrite group. Mercury is hosted at the tetrahedrally coordinated M(1) site, in accord with the relatively long M(1)-S(1) distance (2.389 angstrom), similar to that observed in tetrahedrite-(Hg). Minor Ag is located at the triangularly-coordinated and split M(2) site. Other occurrences of tennantite-(Hg) are briefly reviewed and the Lengenbach finding is described within the framework of previous knowledge about the Hg mineralogy at this locality.
引用
收藏
页码:744 / 751
页数:8
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