On the Crystallographic Polytypes SrAl12O19 (BaFe12O19)–BaFe18O27


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A crystallographic analysis of SrAl12O19 (isostructural to BaFe12O19) and BaFe18O27 showed that the structures of both polytypes contain almost identical cationic and anionic (with participation of a large cation) sublattices, whose geometry is consistent with the high symmetry P63/mmc of these compounds. The presence of unified “skeletal” sublattices is considered to be the main condition for the formation of polytype structures.

Sobre autores

S. Borisov

Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences

Autor responsável pela correspondência
Email: borisov@niic.nsc.ru
Rússia, Novosibirsk, 630090

S. Magarill

Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences

Email: borisov@niic.nsc.ru
Rússia, Novosibirsk, 630090

N. Pervukhina

Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University

Email: borisov@niic.nsc.ru
Rússia, Novosibirsk, 630090; Novosibirsk, 630090

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