“…In addition, the two different values of quadrupole shift were connected with different trigonal distortions of the octahedral environment of iron sites as concluded by De Sitter et al[31]. In fact, this is linked to a non-collinear magnetic structure of the cycloid type as confirmed by neutron diffraction and Mössbauer spectroscopy studies performed by Sosnowska et al[32,33].For doped ceramics (x = 0.1, 0.2 and 0.3), the best fits were performed by adding a third sextets that could be assigned to a change of the magnetic nearest neighbors of Fe 3+[34][35], as substituted by Yb 3+ /Nb 5+ /Ti 4+ leading to a distortion of FeO 6 octahedral origin of structural transition. This could lead to modulation spin structure which contributed to the improvement of magnetization.According to table 2, The isomer shift of all the sextets was around 0.38 -0.42 mms -1 .…”