Crystal chemistry of aeschynite-(Y) from the Western Alps: residual electron density on difference-Fourier map

Citation
P. Bonazzi et S. Menchetti, Crystal chemistry of aeschynite-(Y) from the Western Alps: residual electron density on difference-Fourier map, EUR J MINER, 11(6), 1999, pp. 1043-1049
Citations number
26
Categorie Soggetti
Earth Sciences
Journal title
EUROPEAN JOURNAL OF MINERALOGY
ISSN journal
09351221 → ACNP
Volume
11
Issue
6
Year of publication
1999
Pages
1043 - 1049
Database
ISI
SICI code
0935-1221(199911/12)11:6<1043:CCOAFT>2.0.ZU;2-N
Abstract
Crystal structure and chemical composition of five crystals of non-metamict aeschynite-(Y) from the Western Alps were investigated. In the whole the s tructure previously determined on heat-treated crystals of aeschynite was c onfirmed. Nevertheless an interesting feature emerged from the structure re finements concerning the-presence of a residual density maximum of approxim ately 3 divided by 5 e(-)/Angstrom(3) (C site) in the difference Fourier ma p. The addition of the C site to the structural model significantly improve d the final R factors in all refined samples. The C site is asymmetrically located within an eight-fold cavity, similar in shape to that occupied by A cations. The short A-C distances led to the assumption that the presence o f atoms in the C-site is coupled with structural vacancies in A. The implic ations in the calculation of chemical formulae are discussed.