Epitaxial layers of iron oxides have been grown on a MgO(001) substrat
e by evaporating natural Fe or Fe-57 from Knudsen cells in the presenc
e of a NO2 flow directed to the substrate. The resulting layers have b
een investigated in situ with LEED, RHEED, AES and XPS and ex situ wit
h GEMS and ion beam analysis. For substrate temperatures between 200 a
nd 400 degrees C we observe RHEED oscillations during deposition, indi
cative of layer-by-layer growth. By adjusting the flux of NO2 at the s
urface, all stable and metastable cubic phases in the Fe-O system coul
d be grown: FeO (wustite), Fe3O4 (magnetite), gamma-Fe2O3 (maghemite)
and solid solutions between the latter two phases. Rutherford backscat
tering spectra show a relatively high minimum yield in the channel dir
ections.