Cation partitioning and substitution mechanisms in 1M phlogopite; a crystal chemical study

The crystal chemistry of 1M phlogopite was studied by single-crystal XRD and EPMA. Structural refinement was carried out in space group C2/m (R values between 0.021 and 0.052) on 24 samples of phlogopite from basic lamproites, leucitites, kimberlites and carbonatites.

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Bibliographic Details
Published in:The American mineralogist 1994-04, Vol.79 (3-4), p.289-301
Main Authors: Cruciani, Giuseppe, Zanazzi, Pier Francesco
Format: Article
Language:English
Subjects:
cations
Chemistry
Condensed matter: structure, mechanical and thermal properties
crystal chemistry
Crystals
electron probe data
Exact sciences and technology
Inorganic compounds
mica group
Mineralogy
Minerals
P-T conditions
partitioning
phase equilibria
phlogopite
Physics
sheet silicates
silicates
Structure of solids and liquids
crystallography
Structure of specific crystalline solids
substitution
Water, oxides, hydroxides, peroxides
X-ray absorption spectroscopy: exafs, nexafs, xanes, etc
X-ray diffraction
X-ray diffraction and scattering
X-ray diffraction data
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Description
Summary:The crystal chemistry of 1M phlogopite was studied by single-crystal XRD and EPMA. Structural refinement was carried out in space group C2/m (R values between 0.021 and 0.052) on 24 samples of phlogopite from basic lamproites, leucitites, kimberlites and carbonatites.
ISSN:0003-004X
1945-3027