Vesuvianite can contain significant amounts of boron (up to similar to
4 wt% B2O3). The crystal structures of five boron-bearing vesuvianite
crystals have been refined using MoK alpha X-ray data. Although the c
rystals are significantly biaxial (2V < 20 degrees), Very careful exam
ination of the diffraction data shows no deviation from 4/mmm Laue sym
metry. All crystals show many reflections apparently violating the ext
inction criteria for P4/nnc symmetry, but these are due to double diff
raction, not true Bragg diffraction; hence the space group P4/nnc was
used for all of the refinements. The structure of all specimens of bor
on-bearing vesuvianite (similar 3+,Mg,Fe2+,Mn,Ti](13+x)[Si]O-18-y(68)[
O,OH,F](10), x > y, Z = 2, a approximate to 15.70, c approximate to 11
.75 Angstrom, V approximate to 2895 Angstrom(3)) was refined to an R i
ndex in the range 3-4%. Two new sites were identified and are common t
o all the refined structures; these are designated as T sites. T(1) is
at the special position 8h (similar to 0.05, similar to 0.05, 1/4), a
nd is surrounded by a disordered array of anions that can adopt a tetr
ahedral configuration around the central position. T(2) is at the spec
ial position 2a (1/4, 1/4, 1/4) and is surrounded by an array of disor
dered anions that can adopt a triangular configuration about the centr
al position. The T(1) position is very close to the H(1) position in b
oron-free vesuvianite, and the T(2) position is very close to the H(2)
position in boron-free vesuvianite; hence occupancy of T(1) and T(2)
precludes occupancy of two H(1) and the H(2) positions, in agreement w
ith the substitution B + Mg reversible arrow 2H + Al proposed by Great
et al. (1992) for boron-bearing vesuvianite.