The difference in the internal parameter $z_{3}$ between CuFeO$_{2}$ and CrNaS$_{2}$ causes a large change in the bonding of the two crystals, so we present them as different structures.
The structures are generated by the same symmetry operations with different sets of parameters (--params) specified in their corresponding CIF files.
Hexagonal settings of this structure can be obtained with the option --hex.
F. Engelsman, G. Wiegers, F. Jellinek, and B. V. Laar, Crystal structures and magnetic structures of some metal(I) chromium(III) sulfides and selenides, J. Solid State Chem. 6, 574–582 (1973), doi:10.1016/S0022-4596(73)80018-0.
A. Okada and K. Keil, Caswellsilverite, NaCrS$_2$: a new mineral in the Norton County enstatite achondrite, Am. Mineral. 67, 132–136 (1982).
Found in
R. T. Downs and M. Hall-Wallace, The American Mineralogist Crystal Structure Database, Am. Mineral. 88, 247–250 (2003).
First cited in
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)