On the Crystallographic Polytypes SrAl12O19 (BaFe12O19)–BaFe18O27
- Авторы: Borisov S.V.1, Magarill S.A.1, Pervukhina N.V.1,2
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Учреждения:
- Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences
- Novosibirsk State University
- Выпуск: Том 64, № 4 (2019)
- Страницы: 566-569
- Раздел: Theory of Crystal Structures
- URL: https://journals.rcsi.science/1063-7745/article/view/194064
- DOI: https://doi.org/10.1134/S1063774519040060
- ID: 194064
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Аннотация
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.
Об авторах
S. Borisov
Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: borisov@niic.nsc.ru
Россия, Novosibirsk, 630090
S. Magarill
Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences
Email: borisov@niic.nsc.ru
Россия, Novosibirsk, 630090
N. Pervukhina
Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University
Email: borisov@niic.nsc.ru
Россия, Novosibirsk, 630090; Novosibirsk, 630090
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