Quaternary Ln−M−O−Q oxychalcogenides with structures containing 2D [Ln 2 O 2 ] 2+ layers including (a) ZrCuSiAs structure for LnMOQ phases, (b) Ln 2 O 2 M 2 OQ 2 phases, and (c) MQ 2 layers (from above) in cation-ordered ZrCuSiAs-related phases Ln 2 O 2 MQ 2 containing M 2+ ions, with Ln, M, O, and Q ions shown in blue, cyan, pink, and yellow, respectively.

Quaternary Ln−M−O−Q oxychalcogenides with structures containing 2D [Ln 2 O 2 ] 2+ layers including (a) ZrCuSiAs structure for LnMOQ phases, (b) Ln 2 O 2 M 2 OQ 2 phases, and (c) MQ 2 layers (from above) in cation-ordered ZrCuSiAs-related phases Ln 2 O 2 MQ 2 containing M 2+ ions, with Ln, M, O, and Q ions shown in blue, cyan, pink, and yellow, respectively.

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Mixed-anion systems have garnered much attention in the past decade with attractive properties for diverse applications such as energy conversion, electronics, and catalysis. The discovery of new materials through mixed-cation and single-anion systems proved highly successful in the previous century, but solid-state chemists are now embracing an ex...

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... 2+ sheets are separated by chalcogenide-rich layers (of net negative charge), and the layered structures of these materials ( Figure 5) can have a significant role in determining physical properties. 30 ZrCuSiAs structured materials are composed of alternating fluorite-like [Ln 2 O 2 ] 2+ layers and anti-fluorite-like [M 2 Q 2 ] 2− (M = transition metal) layers of edge-linked M + Q 4 tetrahedra (e.g., LnCuOQ (Ln = Bi, lanthanide). ...

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... 38 It is becoming clear that the structures of rare-earth oxychalcogenides cannot be extrapolated in a simple way from chalcogenides and that more complex structurebuilding principles are at play in these mixed-anion systems. 44,45 In particular, there is a preference for the RE and O atoms to be bonded together in recurring structural motifs involving RE 4 O tetrahedra. Furthermore, in contrast to the observation that sulfides and selenides are often isostructural, the assumption does not necessarily extend to oxysulfides and oxyselenides; for example, notwithstanding their identical compositions, LaGaS 2 O and LaGaSe 2 O have different structures. ...
... These coordination geometries are similar to those found in Sm 3 GaSe 5 O. 38 The longer RE−Se distances The edge-sharing RE 4 O tetrahedra, which are fragments of the fluorite-type structure, are a recurring theme in rare-earth oxychalcogenides. 44,45 They are usually manifested as twodimensional slabs, as found in many layered oxychalcogenides (e.g., LaCuSO 20 and RE 4 Ga 2 S 5 O 4 29,34,35 ) but can be excised further into strips of varying widths, 64 as found here and other instances (e.g., Sm 3 GaSe 5 O 38 and La 4 Ga 2 Se 6 O 3 40 ). The strips of RE 4 O tetrahedra in RE 4 Ga 2 Se 7 O 2 are arranged in the same herringbone pattern as in an orthorhombic polymorph of LaInS 2 O, which also crystallizes in space group Pnma with an identical Wyckoff sequence (c 15 ), 33 but the connectivity of the group-13 and chalcogen atoms is quite different (Figure 3). ...
... When surveying the database, no RE 3 BO 6 or RE 3 BS 6 compounds can be found, suggesting that the title compounds cannot be obtained via straightforward O/S substitution. When compared with other RE-Q-B x O y or RE oxychalcogenide compounds [32,34,[43][44][45][46][47][48][49][50][51], apart from the B-O units, RE 3 S 3 BO 3 also show unique REO x Q y polyhedral units. In fact, all the three types of REO x Q y units REOS 6 , REO 4 S 3 , and REO 3 S 6 are present in other RE oxychalcogenides, however, RE 3 S 3 BO 3 is the only case that these three types of units coexist in one structure. ...
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