“…These features are partly related to the more ionic character of the F – anion, compared with the oxide anion. The perovskite structure affords the formation of several oxyfluorides with transition metals at the B -site, as found in KTiO 2 F, A NbO 2 F ( A = Na, K), Pb M O 2 F ( M = Sc, Mn), and A FeO 2 F ( A = Sr, − Pb, − Ba , ), and they are accessible via conventional solid-state reactions (e.g., A NbO 2 F), high-pressure reactions (e.g., KTiO 2 F and Pb M O 2 F), and topochemical fluorination reactions (e.g., A FeO 2 F).…”