MOSSBAUER AND ELNES SPECTROSCOPY OF (MG,FE)(SI,AL)O3 PEROVSKITE: A HIGHLY OXIDISED COMPONENT OF THE LOWER MANTLE

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dc.contributor.author Lauterbach S.
dc.contributor.author McCammon C.A.
dc.contributor.author van Aken P.
dc.contributor.author Langenhorst F.
dc.contributor.author Seifert F.
dc.date.accessioned 2021-01-25T02:42:44Z
dc.date.available 2021-01-25T02:42:44Z
dc.date.issued 2000
dc.identifier https://elibrary.ru/item.asp?id=984759
dc.identifier.citation Contributions to Mineralogy and Petrology, 2000, 138, 1, 0017-0026
dc.identifier.issn 0010-7999
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/23733
dc.description.abstract (Mg,Fe)(Si,Al)O3 perovskite samples with varying Fe and Al concentration were synthesised at high pressure and temperature at varying conditions of oxygen fugacity using a multianvil press, and were characterised using ex situ X-ray diffraction, electron microprobe, Mossbauer spectroscopy and analytical transmission electron microscopy. The Fe3+/ΣFe ratio was determined from Mossbauer spectra recorded at 293 and 80 K, and shows a nearly linear dependence of Fe3+/ΣFe with Al composition of (Mg,Fe)(Si,Al)O3 perovskite. The Fe3+/ΣFe values were obtained for selected samples of (Mg,Fe)(Si,Al)O3 perovskite using electron energy-loss near-edge structure (ELNES) spectroscopy, and are in excellent agreement with Mossbauer data, demonstrating that Fe3+/ΣFe can be determined with a spatial resolution on the order of nm. Oxygen concentrations were determined by combining bulk chemical data with Fe3+/ΣFe data determined by Mossbauer spectroscopy, and show a significant concentration of oxygen vacancies in (Mg,Fe)(Si,Al)O3 perovskite.
dc.title MOSSBAUER AND ELNES SPECTROSCOPY OF (MG,FE)(SI,AL)O3 PEROVSKITE: A HIGHLY OXIDISED COMPONENT OF THE LOWER MANTLE
dc.type Статья


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