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.