We synthesized the solid solutions Cu3Bi(Se1–x
Te
x
O3)2O2Br (x = 0, 0.25,
0.5, 0.75,
1) for the first time and characterized their structures by X-ray
diffraction (XRD) measurements and their magnetic properties by electron
spin resonance (ESR), magnetic susceptibility, magnetization, and
specific heat measurements as well as by density functional theory
(DFT) calculations. The Néel temperature T
N and the critical field μ
0
H
C needed for the metamagnetic
transition increase with x, while the magnetization
at a given magnetic field and the Curie–Weiss temperature Θ
decrease with x. We show that the tendency for the
interlayer antiferromagnetic (AFM) coupling in francisites is not
explained by interlayer spin exchange but by the interlayer high-spin
orbital interaction that occur across the van der Waals (vdW) gaps,
hence indicating that francisites are vdW ferromagnets. This is surprising
because, so far, well-established vdW ferromagnets are either layered
tellurides or layered iodides. The trends in T
N, μ
0
H
C, and the magnetization of Cu3Bi(Se1–x
Te
x
O3)2O2Br as a function of x are well
explained by the interlayer AFM interactions, and that in the Θ
is explained by the intralayer spin exchanges. We proposed how one
might modify francisites to make their interlayer interactions ferromagnetic
(FM), hence leading to oxide vdW ferromagnets.