The crystal structure of murataite, space group <F(4)over bar 3m>, a 1
4.886(2) Angstrom, has been solved by Patterson methods and refined to
an R of 4.91 (wR 4.71%) for 265 observed reflections (MoK alpha radia
tion). The ideal formula is (Y,Na)(6)(Zn,Fe)(5)Ti12O29(O,F)(10)F-4 wit
h Z = 4, but its simple appearance conceals extensive cation disorder
within the structure. There are four distinct cation sires: the X site
is [8]-coordinated and contains (Y,HREE,Na,Ca,Mn); the T site is tetr
ahedrally coordinated and contains (Zn,Si); the M1 site is octahedrall
y coordinated and contains (Ti,Nb,Na); the M2 sire is [5]-coordinated
by a triangular bipyramid and contains (Zn,Fe3+,Ti,Na). Three M1 octah
edra share edges to form a compact M(3) phi(13) group. Four of these M
(3) phi(13) groups link by sharing corners to form a tetrahedral cage
in the center of which is the T site. The resulting Keggin-structured
[M(12)T phi(40)](n-) unit may be considered as the fundamental buildin
g block of the structure. The net formed by linkage of the M1 polyhedr
a is topologically the same as the B net of UB12, which accounts for t
he similarity of X-ray properties of murataite and this compound.