A number of compositions with general stoichiometry of Gd 2 Ce x Zr 2-x O 7 (0≤x≤2) ceramics have been synthesized and received irradiation test at room temperature with Xe 20+ ions in a broad fluence range. X-ray diffraction (XRD) measurements shows that Gd 2 Ce x Zr 2-x O 7 (0≤x≤0.2) samples adopt the pyrochlore structure, whereas Gd 2 Ce x Zr 2-x O 7 (0.2≤x≤2.0) samples predominantly displayed an anion deficient fluorite structure, indicating that the structures of Gd 2 Ce x Zr 2-x O 7 are determined by the content of doped Ce 4+ ion. XRD results of irradiated samples (Gd 2 Zr 2 O 7 , Gd 2 Ce 2 O 7 ) indicate that Gd 2 Zr 2 O 7 was transformed into a radiation resistant anion deficient fluorite structure with increasing fluence, whereas the Gd 2 Ce 2 O 7 was partially amorphized. It was found that the structural evolutions induced by irradiation are strongly dependent on the samples composition and ions fluence. In addition, SEM results show that the density and hardness of waste forms play an important role in the morphology modifications induced by irradiation. These results would be considered for design and elaboration of future matrices for actinide immobilization or transmutation. 2 actinide wastes. They have been considered as a key component in synroc-based pyrochlore ceramics for geological immobilization of surplus Pu in the US [1]. It is very important that suitable waste form materials should be radiation resistant in geological repository. During long term storage, nuclear waste forms are submitted to severe radiations which induce atomic rearrangements. These structural modifications lead to the deterioration of physic-chemical properties of waste form materials.The pyrochlores under consideration in this study typically exhibit the A 2 B 2 O 7 stoichiometry, where actinides or lanthanides can be incorporated into the eight-coordinated A-site and metals occupy the six-coordinated B-site. Ordered A 2 B 2 O 7 pyrochlores belong to the Fd-3m space group, which is a superstructure of the ideal fluorite structure (Fm-3 space group) with twice the lattice constant. A and B cations occupy the 16c (0,0,0) and 16d (0.5,0.5,0.5) sites, respectively, and oxygens are located at the 48f (x,0.125,0.125) and 8b (0.375,0.375,0.375) positions (using Wyckoff notation). The anion sublattice can be completed by adding missing oxygens in the 8a site to form the anion-deficient fluorite structure. It is well known that the stability of pyrochlore structure is governed by the ratio of the ionic radii of A and B cation (rA/rB). The range of pyrochlore stability extends from 1.46 for Gd 2 Zr 2 O 7 to 1.78 for Sm 2 Ti 2 O 7 . For smaller ionic radii ratios, rA/rB < 1.46, anion-deficient fluorite is a stable structure, whilst the monoclinic structure is stable for ionic radii ratios rA/rB >1.78 [2,3].Given that nuclear waste forms will be subject to considerable α-recoil radiation damage in geological repository, it is important to understand effect of radiation on the pyrochlore structure. Considerable work has been carri...