“…It is well established that in the M-type LaFe 12 O 19 phase, the complete substitution of Sr 2 þ for La 3 þ leads to a change of the valence state of iron ions in the 2a site from Fe 3 þ to Fe 2 þ due to the introduction of La 3 þ ion instead of Sr 2 þ ion to compensate for the excess of positive charges [26][27][28]; analogous conclusions arise from the analysis of NMR measurements in M-type hexaferrites with partial or full substitution of La 3 þ in the heavy cations sites [29]. Fe 2 þ ions being thus located in the 2a octahedral sites of the S-blocks in the M-type ferrite, we assumed by comparing the crystal structure of the three phases, that the Fe 2 þ ions occupy four magnetic a sites corresponding to the 4f VI (or 4f 3 ) and 6g octahedral sites in the SS and S-S blocks of the W unit cell and six magnetic a sites corresponding to the 3b VI, 9e VI and 6c VI octahedral sites in the S-, S-S-and SS-blocks of the X-unit cell, respectively.…”