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High pressure Raman spectroscopy of ferrite MgFe 2 O 4

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dc.contributor.authorWang, Z
dc.contributor.authorLazor, P
dc.contributor.authorSaxena, S.K.
dc.contributor.authorO'Neill, Hugh
dc.date.accessioned2015-12-13T22:24:34Z
dc.date.issued2002
dc.date.updated2015-12-11T08:07:35Z
dc.description.abstractAn in situ Raman spectroscopic study was conducted to explore the pressure-induced phase transformation of ferrite MgFe2O4 to 51.6 GPa. Results indicate that MgFe2O4 transforms to a high pressure polymorphism at a pressure of 27.7 GPa, which was assigned
dc.identifier.issn0025-5408
dc.identifier.urihttp://hdl.handle.net/1885/72789
dc.publisherPergamon-Elsevier Ltd
dc.sourceMaterials Research Bulletin
dc.subjectKeywords: Crystallization; Diffusion; Ferrites; High pressure effects; Inorganic compounds; Phase transitions; Quenching; Raman spectroscopy; Polymorphisms; Magnesium compounds A. Inorganic compound; C. High pressure; C. Raman spectroscopy; D. Phase transformation
dc.titleHigh pressure Raman spectroscopy of ferrite MgFe 2 O 4
dc.typeJournal article
local.bibliographicCitation.issue9
local.bibliographicCitation.lastpage1602
local.bibliographicCitation.startpage1589
local.contributor.affiliationWang, Z, Florida State University
local.contributor.affiliationLazor, P, Florida State University
local.contributor.affiliationSaxena, S.K., Florida State University
local.contributor.affiliationO'Neill, Hugh, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidO'Neill, Hugh, u8101317
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040306 - Mineralogy and Crystallography
local.identifier.ariespublicationMigratedxPub3429
local.identifier.citationvolume37
local.identifier.doi10.1016/S0025-5408(02)00819-X
local.identifier.scopusID2-s2.0-0037043638
local.type.statusPublished Version

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