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Hassan, Ishmael, Kudoh, Yasuhiro, Buseck, Peter R., Ito, Eui (1996) MgSiO3 perovskite: a HRTEM study. Mineralogical Magazine, 60 (402) 799-804 doi:10.1180/minmag.1996.060.402.10

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Reference TypeJournal (article/letter/editorial)
TitleMgSiO3 perovskite: a HRTEM study
JournalMineralogical MagazineISSN0026-461X
AuthorsHassan, IshmaelAuthor
Kudoh, YasuhiroAuthor
Buseck, Peter R.Author
Ito, EuiAuthor
Year1996 (October)Volume60
Issue402
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_60/60-402-799.pdf+
DOIdoi:10.1180/minmag.1996.060.402.10Search in ResearchGate
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Mindat Ref. ID98Long-form Identifiermindat:1:5:98:1
GUID0
Full ReferenceHassan, Ishmael, Kudoh, Yasuhiro, Buseck, Peter R., Ito, Eui (1996) MgSiO3 perovskite: a HRTEM study. Mineralogical Magazine, 60 (402) 799-804 doi:10.1180/minmag.1996.060.402.10
Plain TextHassan, Ishmael, Kudoh, Yasuhiro, Buseck, Peter R., Ito, Eui (1996) MgSiO3 perovskite: a HRTEM study. Mineralogical Magazine, 60 (402) 799-804 doi:10.1180/minmag.1996.060.402.10
In(1996, October) Mineralogical Magazine Vol. 60 (402) Mineralogical Society
Abstract/NotesAbstractSelected-area electron diffraction patterns for the [110] zone of MgSiO3 perovskite are consistent with the orthorhombic unit cell obtained by X-ray diffraction (a = 4.775, b = 4.929, c = 6.897 Ã…). Various areas of a crystal fragment show diffuse streaking along c*, and well-developed satellite reflections that give a 3-fold repeat along [10]*. Another fragment shows doubled cell dimensions when viewed down [30]. The variable occurrence of the satellite reflectioncs and diffuse streaking indicate subtle variations in ordering, chemistry, or both. Images obtained by high-resolution transmission electron microscopy contain perfectly ordered regions, out-of-phase boundaries, and intergrowths of the two orthorhombic forms of perovskite.


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