“…MF 2 phases can dissolve up to dozens percents rare earth fluorides as well as alkali metal fluorides and oxygen (dissolving of the latter results in formation of oxyfluorides). Heterovalent replacement of fluorine by oxygen is known to cause formation of the relatively broad areas of homogeneity for the fluorite-type solid solutions based on Ca, Sr, Ba, Pb difluorides; and this is especially common for the systems that also contain rare earth cations (MF 2 -ROF systems) [309][310][311]231] and/or NaRF 4 [312]. Substitution of fluorine of oxygen in the crystal lattices of these phases results in essential variations of the unit cell parameters.…”