Tlapallite H6(Ca,Pb)2(Cu,Zn)3SO4(TeO3)4TeO6, a multi-anion mineral: A Raman spectroscopic study

被引:22
作者
Frost, Ray L. [1 ]
机构
[1] Queensland Univ Technol, Inorgan Mat Res Program, Sch Phys & Chem Sci, Brisbane, Qld 4001, Australia
基金
澳大利亚研究理事会;
关键词
Tellurate; Tellurite; Tlapallite; Raman spectroscopy; Rodalquilarite; CENTENNIAL-EUREKA MINE; JUAB COUNTY; MOCTEZUMA; SONORA; MEXICO; UTAH;
D O I
10.1016/j.saa.2008.12.008
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
Tellurates may be subdivided according to formula and structure. There are three types of tellurate minerals: type (a) (AB)(m)(TeO4)(p)Z(q), type (b) (AB)(m)(TeO6)center dot xH(2)O and type (c), compound tellurates in which a second anion is involved. Tlapallite, a mufti-anion mineral containing both tellurate and tellurite units, as well as sulphate, is an example of type (a). Tellurates are rare minerals as the tellurate ion is easily reduced to the tellurite ion. Raman bands at 691, 708, 764 and 796cm(-1) are attributed to (TeO6)(2-) and (TeO3)(2-) stretching bands. The intense sharp Raman band at 973 cm(-1) is assigned to the nu(1) (SO4)(2-) symmetric stretching mode, whilst the two bands at 1062 and 1104cm(-1) are assigned to the nu(3) (SO4)(2-) antisymmetric stretching mode. The spectral region 100 to 600 cm(-1) displays the bands which are attributable to the (SO4)(2), (TeO3)(2) and (TeO6)(4-) bending modes. Some evidence from very low intensity Raman bands in the 2800-3600 cm(-1) region provides evidence of proton-tellurate/tellurite anion interactions. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:903 / 906
页数:4
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