Iron–manganese
oxide (Mn
x
Fe1–x
O) nanoplates were prepared by the
thermal decomposition method. Irregular development of crystalline
phases was observed with the increase of annealing temperature. Magnetic
properties are in accordance with their respective crystalline phases,
and the selective magnetic evolution from their rich magnetism of
Mn
x
Fe1–x
O and MnFe2O4 is achieved by controlling the
annealing conditions. Rock-salt structure of Mn
x
Fe1–x
O (space group Fm3̅m) is observed in as-synthesized
nanoplates, while MnFe2O4 and Mn
x
Fe1–x
O with significant
magnetic interactions between them are observed at 380 °C. In
nanoplates annealed at 450 °C, soft ferrites of Mn0.48Fe2.52O4 with Mn
x
Fe1–x
O are observed. It is assumed
that the differential and early development of crystalline phase of
Mn
x
Fe1–x
O and the inhomogeneous cation mixing between Mn and Fe cause this
rather extraordinary magnetic development. In particular, the prone
nature of divalent metal oxides to cation vacancy and the prolonged
annealing time of 15 h which enables ordering are also thought to
contribute to these irregularities.