Volume 68 Received 6 October 2012 | |||||||||||
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aUniversity High School, 421 N. Arcadia Avenue, Tucson, Arizona 85711-3032, USA,bCatalina Foothills High School, 4300 E. Sunrise Drive, Tucson, Arizona 85718-4300, USA, and cDepartment of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, Arizona 85721-0077, USA
Correspondence e-mail: mabadean@terra.com.br
The crystal structure of durangite, ideally NaAl(AsO4)F (chemical name sodium aluminium arsenate fluoride), has been determined previously [Kokkoros (1938). Z. Kristallogr. 99, 38-49] using Weissenberg film data without reporting displacement parameters of atoms or a reliability factor. This study reports the redetermination of the structure of durangite using single-crystal X-ray diffraction data from a natural sample with composition (Na0.95Li0.05)(Al0.91Fe3+0.07Mn3+0.02)(AsO4)(F0.73(OH)0.27) from the type locality, the Barranca mine, Coneto de Comonfort, Durango, Mexico. Durangite is isostructural with minerals of the titanite group in the space group C2/c. Its structure is characterized by kinked chains of corner-sharing AlO4F2 octahedra parallel to the c axis. These chains are cross-linked by isolated AsO4 tetrahedra, forming a three-dimensional framework. The Na+ cation (site symmetry 2) occupies the interstitial sites and is coordinated by one F- and six O2- anions. The AlO4F2 octahedron has symmetry -1; it is flattened, with the Al-F bond length [1.8457 (4) Å] shorter than the Al-O bond lengths [1.8913 (8) and 1.9002 (9) Å]. Examination of the Raman spectra for arsenate minerals in the titanite group reveals that the position of the band originating from the As-O symmetric stretching vibrations shifts to lower wavenumbers from durangite, maxwellite [ideally NaFe(AsO4)F], to tilasite [CaMg(AsO4)F].
For previous work on durangite, see: Brush (1869
); Des Cloizeaux (1875
); Kokkoros (1938
); Machatschki (1941
); Sumin de Portilla (1974
); Foord et al. (1985
). For minerals isostructural with or similar to durangite, see: Hawthorne (1990
); Groat et al. (1990
); Hawthorne et al. (1991
); Oberti et al. (1991
); Bermanec (1994
); Cooper & Hawthorne (1995
); Troitzsch et al. (1999
); Sebastian et al. (2002
). For Raman spectroscopic measurements on arsenate minerals and compounds, see: Yang et al. (2011a
,b
); Frost & Xi (2012
); Frost et al. (2012
). For the definition of polyhedral distortion, see: Robinson et al. (1971
).
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Data collection: APEX2 (Bruker, 2004
); cell refinement: SAINT (Bruker, 2004
); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008
); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008
); molecular graphics: XtalDraw (Downs & Hall-Wallace, 2003
); software used to prepare material for publication: publCIF (Westrip, 2010
).
Supplementary data and figures for this paper are available from the IUCr electronic archives (Reference: WM2690 ).
Support of this study was provided by the Arizona Science Foundation, CNPq 202469/2011-5 from the Brazilian government for MBA, and Bruker AXS for a summer work study by GWD and BNY. The durangite sample used in this study was kindly donated to the RRUFF Project by Michael Shannon.
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