PRESSURE-INDUCED PHASE TRANSITION IN MG0.8FE0.2O FERROPERICLASE

Простая страница элемента
dc.contributor.authorKantor I.
dc.contributor.authorDubrovinsky L.
dc.contributor.authorMcCammon C.
dc.contributor.authorKantor A.
dc.contributor.authorPascarelli S.
dc.contributor.authorAquilanti G.
dc.contributor.authorCrichton W.
dc.contributor.authorMattesini M.
dc.contributor.authorAhuja R.
dc.contributor.authorAlmeida J.
dc.contributor.authorUrusov V.
dc.date.accessioned2025-05-10T04:38:14Z
dc.date.available2025-05-10T04:38:14Z
dc.date.issued2006
dc.description.abstractCombined X-ray powder diffraction, Mössbauer, and XANES spectroscopy in situ experiments revealed the transformation of cubic (Mg0.8Fe0.2)O ferropericlase to a rhombohedrally distorted phase at 35(1) GPa and room temperature. The Mössbauer spectroscopy results show that the rhombohedral distortion does not involve magnetic ordering. Combined with data from the literature, our results imply that the cubic to rhombodedral transition occurs in (Mg,Fe)O under conditions of non-hydrostatic stress over a wide range of composition (0.2 ≤ xFe ≤ 1). © Springer-Verlag 2006.
dc.identifierhttps://elibrary.ru/item.asp?id=13503560
dc.identifier.citationPhysics and Chemistry of Minerals, 2006, 33, 1, 35-44
dc.identifier.doi10.1007/s00269-005-0052-z
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/49186
dc.subjectDIAMOND ANVIL CELL
dc.subjectFERROPERICLASE
dc.subjectHIGH PRESSURE
dc.titlePRESSURE-INDUCED PHASE TRANSITION IN MG0.8FE0.2O FERROPERICLASE
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Изображение-миниатюра
Имя:
Kant_06.pdf
Размер:
704.5 KB
Формат:
Adobe Portable Document Format
Скачать

Коллекции

ELibrary