“…Each layer of magnetic Fe 3+ ions ( 6 S 5/2 ground state) constitutes a two-dimensional, triangular lattice, which in combination with antiferromagnetic interactions represents a classical case of geometric frustration. Despite its electronic configuration, which prima facie suggests isotropic antiferromagnetic exchange interactions, CuFeO 2 adopts a collinear, Ising-like magnetic structure at low temperatures below 11 K. In zero magnetic field, two structural [13,14] and magnetic transitions are observed at T N1 ≈ 14 K and T N2 ≈ 11 K. Structurally, CuFeO 2 transforms to space group C2/m at T N1 and to lower monoclinic symmetry at T N2 . Above T N1 , CuFeO 2 is paramagnetic (PM), whereas the magnetic structure in the intermediate temperature phase (ITP), i.e., T N2 < T < T N1 , is usually considered a quasi-long-range ordered, sinusoidally amplitude modulated, incommensurate structure with a temperature-dependent propagation vector [15] and a potential, residual paramagnetic contribution [16].…”