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Fanfani, L., Nunzi, A., Zanazzi, P. F., Zanzari, A. R. (1973) The crystal structure of buttgenbachite. Mineralogical Magazine, 39 (303) 264-270 doi:10.1180/minmag.1973.039.303.02

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Reference TypeJournal (article/letter/editorial)
TitleThe crystal structure of buttgenbachite
JournalMineralogical Magazine
AuthorsFanfani, L.Author
Nunzi, A.Author
Zanazzi, P. F.Author
Zanzari, A. R.Author
Year1973 (September)Volume39
Issue303
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_39/39-303-264.pdf+
DOIdoi:10.1180/minmag.1973.039.303.02Search in ResearchGate
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Mindat Ref. ID6686Long-form Identifiermindat:1:5:6686:4
GUID0
Full ReferenceFanfani, L., Nunzi, A., Zanazzi, P. F., Zanzari, A. R. (1973) The crystal structure of buttgenbachite. Mineralogical Magazine, 39 (303) 264-270 doi:10.1180/minmag.1973.039.303.02
Plain TextFanfani, L., Nunzi, A., Zanazzi, P. F., Zanzari, A. R. (1973) The crystal structure of buttgenbachite. Mineralogical Magazine, 39 (303) 264-270 doi:10.1180/minmag.1973.039.303.02
In(1973) Mineralogical Magazine Vol. 39 (303) Mineralogical Society
Abstract/NotesSummaryThe crystal structure of buttgenbachite from Likasi (Congo) was solved by a three- dimensional Patterson function, computed using intensity data collected photographically by the Weissenberg method, and refined by successive Fourier maps and least-squares refinement to an R index 0·055 for 328 independent observed reflections. The cell content resulting from the structural analysis is Cu36·6Cl6·7(NO3)2·6(OH)63·9.2·1 H2O. The space group is P63/mmc with a = 15·750 Å and c = 9·161Å. The buttgenbachite structure is not completely ordered. It consists of a rigid three-dimensional skeleton formed by Cu co-ordination polyhedra sharing edges and corners. The large channels in the framework show a zeolite-like nature; inside the channels the disorder is caused by the different orientations of nitrate groups and by the occurrence of the substitution . The crystal structure of buttgenbachite is closely related to that of connellite. The mechanism of forming an isomorphous series is discussed: the present study shows that the replacement is more complicated than was supposed in the literature.

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Buttgenbachite


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