The crystal structure of mineral bussenite, Na
2Ba
2Fe[TiSi
2O
7][CO
3]O(OH)(H
2O)F, found in the Khibiny massif (the Kola Peninsula) has been determined. The parameters of the triclinic unit-cell are
a = 5.399(3) Å,
b = 7.016(9) Å,
c = 16.254(14) Å, α = 102.44(8)°, β = 93.18(6)°, γ = 90.10(7)°, sp. gr.
P[`1]P\bar 1
,
R = 0.054 for 1418 reflections with |
F| > 2.5σ(
F). The mineral studied belongs to the family of layered titanosilicates, in which, unlike the sulfate-and phosphate-containing
representatives of this family, the interlayer spaces are filled with carbonate groups.
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Translated from Kristallografiya, Vol. 47, No. 1, 2002, pp. 50–53.
Original Russian Text Copyright © 2002 by Zhou, Rastsvetaeva, Khomyakov, Ma, Shi.