“…Crystallinity is defined by the combination of local point symmetry and long‐range translational symmetry. Relatively simple and high‐symmetry parent structures that participate in high‐entropy systems include rocksalt (general formula AO; space group symmetry
),
3,25 fluorite (
;
),
15,30 bixbyite (or C‐type rare‐earth oxide structure; A 2 O 3 ;
),
15,16 perovskite (ABO 3 ;
,
, or
),
31–34 spinel (AB 2 O 4 or A 3 O 4 ; typically
or
),
17,26,35,36 and pyrochlore (A 2 B 2 O 7 ; typically
or
)
37,38 . Fundamental studies on phase stability, cation site occupancy, and properties employing these simple structures continue to guide research and development of HEOs with other, more complex structures, including Ruddlesden–Popper phases,
39 silicate phases,
40–42 aluminates,…”