The crystal structure of cronstedtite-3T from Kutna Hora (Bohemia, Cze
choslovakia), space group P3(1), was refined to R(w)(all) = 3.1% for 1
336 independent diffractions. There are two and three independent tetr
ahedral and octahedral positions, respectively, in this structure. The
tetrahedra are occupied by 0.75 Si and 0.25 Fe while the octahedra ar
e uniformly occupied by Fe. The refinement process was hindered by two
problems: a ''strong'' superposition structure (all atoms of the octh
aderal sheets, i.e., divided-by 70% of the total diffraction power con
tribute almost solely to the family diffractions with mod(h - k), 3) =
0), and a slight disorder of the investigated crystal. The first prob
lem was resolved by a preliminary block-diagonal refinement procedure
where the atoms coinciding in the superposition structure were separat
ed into individual blocks. The second problem was resolved by includin
g two scale factors into the final full-matrix refinement: one for fam
ily diffractions, the other for the remaining ones which are character
istic for this polytype.