Encyclopedia of Crystallographic Prototypes

AFLOW Prototype: A3B4C_cP8_215_c_e_b-001

This structure originally had the label A3B4C_cP8_215_d_e_a. Calls to that address will be redirected here.

If you are using this page, please cite:
M. J. Mehl, D. Hicks, C. Toher, O. Levy, R. M. Hanson, G. L. W. Hart, and S. Curtarolo, The AFLOW Library of Crystallographic Prototypes: Part 1, Comp. Mat. Sci. 136, S1-S828 (2017). (doi=10.1016/j.commatsci.2017.01.017)

Links to this page

https://aflow.org/p/WCVT
or https://aflow.org/p/A3B4C_cP8_215_c_e_b-001
or PDF Version

Sulvanite (Cu$_{3}$S$_{4}$V, $H2_{4}$) Structure: A3B4C_cP8_215_c_e_b-001

Picture of Structure; Click for Big Picture
Prototype Cu$_{3}$S$_{4}$V
AFLOW prototype label A3B4C_cP8_215_c_e_b-001
Strukturbericht designation $H2_{4}$
Mineral name sulvanite
ICSD 15490
Pearson symbol cP8
Space group number 215
Space group symbol $P\overline{4}3m$
AFLOW prototype command aflow --proto=A3B4C_cP8_215_c_e_b-001
--params=$a, \allowbreak x_{3}$

Other compounds with this structure

Cu$_{3}$S$_{4}$Nb,  Cu$_{3}$S$_{4}$Ta,  Cu$_{3}$Se$_{4}$Nb,  Cu$_{3}$Se$_{4}$Ta,  Cu$_{3}$Se$_{4}$V,  Cu$_{3}$Te$_{4}$Nb,  Cu$_{3}$Te$_{4}$Ta,  Cu$_{3}$Te$_{4}$V


  • This structure is very similar to lazarevićite (AsCu$_{3}$S$_{4}$), except that in this case the copper atoms are on the cubic edges [the (3d) sites] rather than the cubic faces [the (3c) sites].

\[ \begin{array}{ccc} \mathbf{a_{1}}&=&a \,\mathbf{\hat{x}}\\\mathbf{a_{2}}&=&a \,\mathbf{\hat{y}}\\\mathbf{a_{3}}&=&a \,\mathbf{\hat{z}} \end{array}\]

Basis vectors

Lattice coordinates Cartesian coordinates Wyckoff position Atom type
$\mathbf{B_{1}}$ = $\frac{1}{2} \, \mathbf{a}_{1}+\frac{1}{2} \, \mathbf{a}_{2}+\frac{1}{2} \, \mathbf{a}_{3}$ = $\frac{1}{2}a \,\mathbf{\hat{x}}+\frac{1}{2}a \,\mathbf{\hat{y}}+\frac{1}{2}a \,\mathbf{\hat{z}}$ (1b) V I
$\mathbf{B_{2}}$ = $\frac{1}{2} \, \mathbf{a}_{2}+\frac{1}{2} \, \mathbf{a}_{3}$ = $\frac{1}{2}a \,\mathbf{\hat{y}}+\frac{1}{2}a \,\mathbf{\hat{z}}$ (3c) Cu I
$\mathbf{B_{3}}$ = $\frac{1}{2} \, \mathbf{a}_{1}+\frac{1}{2} \, \mathbf{a}_{3}$ = $\frac{1}{2}a \,\mathbf{\hat{x}}+\frac{1}{2}a \,\mathbf{\hat{z}}$ (3c) Cu I
$\mathbf{B_{4}}$ = $\frac{1}{2} \, \mathbf{a}_{1}+\frac{1}{2} \, \mathbf{a}_{2}$ = $\frac{1}{2}a \,\mathbf{\hat{x}}+\frac{1}{2}a \,\mathbf{\hat{y}}$ (3c) Cu I
$\mathbf{B_{5}}$ = $x_{3} \, \mathbf{a}_{1}+x_{3} \, \mathbf{a}_{2}+x_{3} \, \mathbf{a}_{3}$ = $a x_{3} \,\mathbf{\hat{x}}+a x_{3} \,\mathbf{\hat{y}}+a x_{3} \,\mathbf{\hat{z}}$ (4e) S I
$\mathbf{B_{6}}$ = $- x_{3} \, \mathbf{a}_{1}- x_{3} \, \mathbf{a}_{2}+x_{3} \, \mathbf{a}_{3}$ = $- a x_{3} \,\mathbf{\hat{x}}- a x_{3} \,\mathbf{\hat{y}}+a x_{3} \,\mathbf{\hat{z}}$ (4e) S I
$\mathbf{B_{7}}$ = $- x_{3} \, \mathbf{a}_{1}+x_{3} \, \mathbf{a}_{2}- x_{3} \, \mathbf{a}_{3}$ = $- a x_{3} \,\mathbf{\hat{x}}+a x_{3} \,\mathbf{\hat{y}}- a x_{3} \,\mathbf{\hat{z}}$ (4e) S I
$\mathbf{B_{8}}$ = $x_{3} \, \mathbf{a}_{1}- x_{3} \, \mathbf{a}_{2}- x_{3} \, \mathbf{a}_{3}$ = $a x_{3} \,\mathbf{\hat{x}}- a x_{3} \,\mathbf{\hat{y}}- a x_{3} \,\mathbf{\hat{z}}$ (4e) S I

References

  • F. J. Trojer, Refinement of the Structure of Sulvanite, Am. Mineral. 51, 890–894 (1966).

Found in

  • R. T. Downs and M. Hall-Wallace, The American Mineralogist Crystal Structure Database, Am. Mineral. 88, 247–250 (2003).

Prototype Generator

aflow --proto=A3B4C_cP8_215_c_e_b --params=$a,x_{3}$

Species:

Running:

Output: