“…High peak intensity with the same plane group indicates high crystalline quality of the flakes with the growth orientation perpendicular to the substrate. Note that although trigonal Cr 5 Te 8 adopts a (2 × 2) supercell of CrTe 2 by self-intercalating a secondary Cr atomic layer into the CrTe 2 backbones, ,, the lattice constants of Cr 5 Te 8 ( a = b = 0.782–792 nm, c = 1.199–1.186 nm) do not show an exactly double relation with those of 1T-CrTe 2 ( a = b = 0.377–0.385 nm, c = 0.617–0.610 nm). ,,,, In addition to the diffraction peaks of CrTe 2 (001), (002), and (003) planes at 14.89°, 29.87°, and 45.41°, additional peaks of the (004) and (006) planes of Cr 5 Te 8 can be observed at ∼29.94° and 45.58° near the CrTe 2 (002) and (003) peaks in the enlarged view of Figure d and Figure S2, suggesting the coexistence of Cr 5 Te 8 and CrTe 2 in the flakes. Besides, the diffraction peaks have an obvious upshift compared to bulk 1T-CrTe 2 and tri-Cr 5 Te 8 , ,, indicating the existence of compressive strain along the c- axis, thus in-plane tensile strain.…”