“…For example, magnetite, Fe 3 O 4 , is ferrimagnet with anomalously high Curie temperature ~ 850 K. The band-structure calculations (see, e.g., [30]) have predicted that Fe 3 O 4 is a half-metal with only one spin subband at the Fermi level. Experimentally, the spin-resolved photoemission on epitaxial thin films indeed indicated a spin polarization about 80% at room temperature [31] However, below a Verwey transition at about 120 K, single crystal Fe 3 O 4 shows a nonmetallic (polaronic) type of conductivity (see, e.g., [32]), and, in fact, the PCAR method cannot be used.…”