It has recently been shown that well-ordered Fe3O4(111) films can be p
repared epitaxially on clean Pt(111) surfaces; various techniques have
indicated that these multilayer films are chemically identical to bul
k single crystals. We have studied the electronic structure of such an
ordered Fe3O4(111) film using angle-resolved photoemission in conjunc
tion with synchrotron radiation. The valence-band structure along the
Gamma(L) symmetry line and the resonant emission enhancement across th
e Fe 3p-->3d excitation threshold have been examined in detail both ab
ove (at 300 K) and below (at 90 K) the Verwey transition temperature (
similar to 120K) for magnetite. The observed band dispersion agrees re
asonably well with band-structure calculations for the high-temperatur
e phase, particularly near the Fermi level, suggesting that Fe3O4, sho
uld be treated with band theory. Subtle differences in the valence-ban
d structure are observed between the two temperatures, which may be at
tributed to a structural change and/or a charge ordering associated wi
th the Verwey transition. The resonant behavior shows, however, no tem
perature dependence, indicating that resonant photoemission in Fe3O4 r
emains a localized process and is not influenced by the Verwey transit
ion.