The magnetic properties of double perovskite oxide RE 2 FeCrO 6 (RE = GD, Tb, Dy, Er) were systematically studied, and the Griffiths phase evolution was observed. In Tb 2 FeCrO 6 , Dy 2 FeCrO 6 , and Er 2 FeCrO 6 , there are antiferromagnetic (AFM)-ferromagnetic (FM) first-order phase transition and the Griffiths phase with coexistence of FM and paramagnetic (PM) was observed by the EPR spectra. Gd 2 FeCrO 6 has an AFM–PM second-order phase transition, and there is no first-order phase transition in the range of ∆ H = 0–50 kOe. As the temper...