Far-infrared study of the influence of the octahedral sheet composition on the K+-layer interactions in synthetic phlogopites

Clays and Clay Minerals

Volumn 58, Issue 2, 2010, Pages 263-271

  Diaz, Magali ^a   Robert, Jean Louis ^b   Schroeder, Paul A ^c   Prost, Rene ^a  

^a CEMAGREF   (France)

^b UMR 7327   (France)

^c UNIVERSITY OF GEORGIA   (United States)

Author keywords

Annite; Biotite; Compensating cation; Far infrared spectrometry; K+ layer interactions; Octahedral substitutions; Phlogopite; Synthetic; Tetrahedral rotation

Indexed keywords

B-PARAMETER; BIOTITE; CATION SITES; CAVITY GEOMETRY; FAR-INFRARED; FREQUENCY SHIFT; IN-PLANE; INTERLAYER CATION; IONIC RADIUS; IONIC SIZES; LATTICE PARAMETERS; LAYER INTERACTION; NEW APPROACHES; OCTAHEDRAL CATION; OCTAHEDRAL COMPOSITION; OCTAHEDRAL SHEETS; OXIDATION STATE; ROTATION ANGLES; STRUCTURAL DATA; STRUCTURAL FEATURE; VIBRATION BANDS; WAVE NUMBERS;

MICA; POSITIVE IONS; ROTATION; SILICATES; SPECTROMETRY; X RAY DIFFRACTION; X RAY DIFFRACTION ANALYSIS;

INFRARED SPECTROSCOPY;

BIOTITE; CATION; CHEMICAL COMPOSITION; CRYSTAL CHEMISTRY; CRYSTAL STRUCTURE; INFRARED SPECTROSCOPY; LATTICE DYNAMICS; OXIDATION; PARAMETERIZATION; PHLOGOPITE; PHYLLOSILICATE; SUBSTITUTION; X-RAY DIFFRACTION;

EID: 77953312529     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.2010.0580210     Document Type: Article

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