In the Fe/Gd multilayered system the magnetic moments are constrained
to be in the film plane owing to dominant shape anisotropy, provided t
he absence of crystal field effects upon the S state of Gd3+. The in-p
lane magnetic structure versus an external field applied parallel to t
he plane is studied through magnetization, magnetoresistance measureme
nts and Fe-57 Mossbauer spectroscopy. The transition from the ''aligne
d state'' to a ''twisted state'' is evidenced at a critical H field f
or a Fe(42angstrom)/Gd(84angstrom) sample. It turns out that H depend
s upon temperature and respective Fe-Gd submagnetizations. The ''twist
ed state'' is favoured at the compensation temperature.