The crystal structure of Pd3HgTe3, the synthetic analogue of temagamite

被引:2
|
作者
Laufek, Frantisek [1 ]
Vymazalova, Anna [1 ]
Drabek, Milan [1 ]
Dusek, Michal [2 ]
Navratil, Jiri [3 ]
Cernoskova, Eva [4 ,5 ]
机构
[1] Czech Geol Survey, Geologicka 6, Prague 15200 5, Czech Republic
[2] AS CR, Vvi, Inst Phys, Cukrovarnicka 10-112, Prague 16200 6, Czech Republic
[3] Acad Sci Czech Republ, Inst Macromol Chem, Heyrovsky Sq 2, Prague 12006, Czech Republic
[4] CAS, Vvi, Joint Lab Solid State Chem, IMC, Studentska 84, Pardubice 53210, Czech Republic
[5] Univ Pardubice, Fac Chem Technol, Studentska 84, Pardubice 53210, Czech Republic
关键词
temagamite; crystal structure; crystal-structure solution; Pd-Hg telluride; PLATINUM-GROUP MINERALS; MERENSKY REEF; TISCHENDORFITE; DEPOSIT;
D O I
10.1127/ejm/2016/0028-2547
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The crystal structure of the synthetic analogue of the mineral temagamite, Pd3HgTe3, was solved and refined to an R-factor of 0.0522 from single-crystal X-ray diffraction data. The structure is trigonal, space group P3m1, with a = 7.8211(6) angstrom, c = 17.281(1) angstrom, V = 917.8(1) angstrom(3) (hexagonal setting) and Z = 6. Layer modules (A-F) stacked along the c-axis form the crystal structure of Pd3HgTe3. Module A is composed of isolated octahedra [PdTe6], which share faces with adjacent octahedra from neighbouring modules. The edge-sharing [PdTe6] octahedra and [PdTe4] squares form the modules B and F, whereas the corner-sharing [PdTe4] squares constitute modules C, D and E. The Hg atoms occupy the anti-cubooctahedral voids formed by Te atoms. The Pd-Pd and Pd-Hg bonds are also present in the structure. The symmetry of temagamite was revised based on the structural results of this study.
引用
收藏
页码:825 / 834
页数:10
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