X-ray intensity data for olshanskyite, Ca-2[B3O3(OH)(6)]OH . 3H(2)O, were c
ollected from a crystal from the Fuka mine, Okayama Prefecture, Japan, usin
g a PW1100 Philips single-crystal diffractometer. Olshanskyite is triclinic
, a 7.953(4), b 9.873(9), c 7.362 (6) Angstrom, alpha 111.00(7), beta 94.65
(7), gamma 107.53(7)degrees, space group P (1) over bar, Z = 2. The crystal
structure was solved and refined to R = 0.017 for 3833 observed reflection
s and to R = 0.022 for all unique reflections (4419). The anionic group in
the structure is a three-membered ring of boron-oxygen tetrahedra [B3O3(OH)
(6)](3-). Two independent calcium atoms occur in a distorted square-antipri
sm coordination with five oxygen atoms from the berate group and three hydr
oxyl or H2O groups external to the berate cluster. The apparent discrepanci
es between the unit-cell parameters and the formula unit of olshanskyite re
sulting from the present research and those previously determined are attri
buted to two alternative interpretations of the same chemical and X-ray pow
der data. Analogies and differences between the crystal structure of olshan
skyite and that of the analogous berate nifontovite Ca-3[B3O3(OH)(6)](2). 2
H(2)O also are discussed. Olshanskyite must be classified as a neso-tribora
te, and its structure is based on finite berate clusters (FBB = 3 rectangle
).