The use of electron optical methods to determine the crystal structure of a modulated phyllosilicate; parsettensite

The crystal structure of parsettensite, approximately (Mn,Mg)49- (Si64.5,Al7.5)O168(OH)50nH2O where M+ is an exchangeable cation such as K, Na, or Ca, was solved by trial-and-error methods based on high-resolution TEM images and electron diffraction data.

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Bibliographische Detailangaben
Veröffentlicht in:	The American mineralogist 1994-06, Vol.79 (5-6), p.426-437
Hauptverfasser:	Eggleton, R. A, Guggenheim, Stephen
Format:	Artikel
Sprache:	eng
Schlagworte:	chemical analysis Condensed matter: structure, mechanical and thermal properties crystal structure Crystals data processing Electron, ion, and scanning probe microscopy ELNES method Exact sciences and technology Fourier analysis Geology Inorganic compounds Mineralogy Minerals parsettensite Physics Salts Scientific imaging sheet silicates silicates Structure of solids and liquids crystallography Structure of specific crystalline solids Transmission, reflection and scanning electron microscopy(including ebic) X-ray diffraction data
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Beschreibung
Zusammenfassung:	The crystal structure of parsettensite, approximately (Mn,Mg)49- (Si64.5,Al7.5)O168(OH)50nH2O where M+ is an exchangeable cation such as K, Na, or Ca, was solved by trial-and-error methods based on high-resolution TEM images and electron diffraction data.
ISSN:	0003-004X 1945-3027