This is a distortion of the rock salt ($B1$) structure, and GeTe undergoes a phase transition to the rock salt structure above 300°C. When $\alpha = 60° (c/a = \sqrt{6})$ and $z_{2}-z_{1} = 1/2$ this becomes the rock salt structure.
Space group $R3m$ #160 does not specify the origin of the $z$-axis. Here we arbitrarily set $z_{1} = 0$.
Hexagonal settings of this structure can be obtained with the option --hex.
T. Nonaka, G. Ohbayashi, Y. Toriumi, Y. Mori, and H. Hashimoto, Crystal structure of GeTe and Ge$_{2}$Sb$_{2}$Te$_{5}$ meta-stable phase, Thin Solid Films 370, 258–261 (2000), doi:10.1016/S0040-6090(99)01090-1.
First cited in
H. Eckert, S. Divilov, M. J. Mehl, D. Hicks, A. C. Zettel, M. Esters, X. Campilongo, and S. Curtarolo, The AFLOW Library of Crystallographic Prototypes: Part 4, Comp. Mat. Sci. 240, 112988 (2024). (doi=10.1016/j.commatsci.2021.110450)