  Weak first-order phase transitions from axial to oblique spin ordering in
FeBr2 are evidenced by SQUID magnetometry in axial fields H1(T) above the
multicritical point, Hm = 2.4 MA/m, Tm = 4.6 K, and below the
antiferro-to-paramagnetic phase line, Hc(T), in agreement with recent specific
heat data (Aruga Katori et al., 1996). The ordering of the in-plane moments is
probably due to non-diagonal coupling to the longitudinal ones, both of which
increase dis-continuously at H1(T) only under an additional symmetry-breaking
transverse field.
