Disappearance of peculiarly large atomic displacement in the high-temperature phase of magnetite with substitution of Fe2+ by Ni2+ and Mn2+

Kitamura, T.; Niimi, T.; Okudera, H.

doi:10.1107/S2052520625009928

Acta Crystallographica Section B
Acta Crystallographica
Section B STRUCTURAL SCIENCE, CRYSTAL ENGINEERING AND MATERIALS

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Figure 5
Selected m.s.d.s (Å²) in mgt#2, Mn10 and natural magnetite #14 (Okudera et al., 1996

) in heating cycle. Dashed lines in red and blue are linear regressions of observations. The thin black line starting from Bp-mgt#2 was drawn as 88.5% of the regression line for Bp-#14, and the line from Bp-Mn10 was its parallel translation.

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 82| Part 1| February 2026| Pages 98-107

https://doi.org/10.1107/S2052520625009928

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