“…1. The diffraction peaks observed at 2H=27.948 and 46.908 can be generated by the (112) and the (204, 220) CuInS 2 crystallographic planes in either the sphalerite or the chalcopyrite structure [5,6]. However, the samples exhibit also a prominent series of diffraction peaks at 2H=14.408, 28.988, 44.068 and 60.108 that are generated neither by sphalerite nor chalcopyrite CuInS 2 .…”