Mineralogical Journal
Online ISSN : 1881-4174
Print ISSN : 0544-2540
ISSN-L : 0544-2540
 
The crystal structure of a germanate mica KMg2.5+xGe4−2xAl2xO10F2 (x≈0.14) and distortion of (Ge, Al)O4 tetrahedra
Hideo TORAYAFumiyuki MARUMO
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1983 Volume 11 Issue 5 Pages 222-231

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Abstract
The system KMg2.5Ge4O10F2–KMg3Ge3AlO10F2 forms a complete solid solution. The analyzed specimen has a structure of the 1 M mica with cell dimensions of a=5.413(1), b=9.368(2), c=10.531(6)Å and β=99.88(5)° and the experimental composition of KMg2.64Ge3.72Al0.28O10F2. The structure was refined with the full-matrix least-squares procedure to the final R value of 0.042 for 1568 observed reflections. The structural features are the intermediate between the two opposite end members. The Mg2+ ions and vacancies are partially ordered in two independent octahedral sites. The distortion of the (Ge, Al)O4 tetrahedra has been discussed in comparison with that of the (Si, Al)O4 in silicate micas.
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© 1983 Japan Association of Mineralogical Sciences
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