1978 Volume 9 Issue 1 Pages 1-15
Achmatovsk valuevite, Ca0.99(Mg2.20Fe2+0.14Al0.70) (Al2.77Si1.23)·O10(OH)2, a=5.21(1)Å, b=9.00(4)Å, c=9.83(4)Å, β=100°10(6)′ (for 1 M subcell), exhibits X-ray diffraction patterns which assume, unlike common xanthophyllites, a 2 M1 type. A salient feature was observed in the diffraction patterns that reflections with k≠3n are drawn out along c*, and that the diffuse maxima are slightly but significantly displaced from the positions expected for those of a regular 2 M1 structure, showing that the structure is based on a statistical mode of layer sequence. By comparing observed periodic intensity distribution function with ones calculated based on the computer-generated random models of long-period polytypes, which consist of around 100∼150 layers, we have been successful in deriving the probable model for the layer sequence. It is based on the 2 M1 type but faults based on the stacking mode of 1 M occur with a probability of ∼0.1. A notable feature of the model is that the stacking-fault vectors align in only one direction.