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Henderson, Rachel R., Yang, Hexiong, Downs, Robert T., Jenkins, Robert A. (2008) Redetermination of conichalcite, CaCu(AsO4)(OH). Acta Crystallographica Section E Structure Reports Online, 64 (9). i53-i54 doi:10.1107/s1600536808024173

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Reference TypeJournal (article/letter/editorial)
TitleRedetermination of conichalcite, CaCu(AsO4)(OH)
JournalActa Crystallographica Section E Structure Reports Online
AuthorsHenderson, Rachel R.Author
Yang, HexiongAuthor
Downs, Robert T.Author
Jenkins, Robert A.Author
Year2008 (August 6)Volume<   64   >
Page(s)i53-i54Issue<   9   >
PublisherInternational Union of Crystallography (IUCr)
URL
DOIdoi:10.1107/s1600536808024173Search in ResearchGate
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Original EntryHenderson, R.R., Yang, H., Downs, R.T., Jenkins, R.A. (2008) Redetermination of conichalcite, CaCuAsO4)(OH). Acta Crystallographica: E64: i53-i54.
Classification
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Mindat Ref. ID16106370Long-form Identifiermindat:1:5:16106370:2
GUID0
Full ReferenceHenderson, Rachel R., Yang, Hexiong, Downs, Robert T., Jenkins, Robert A. (2008) Redetermination of conichalcite, CaCu(AsO4)(OH). Acta Crystallographica Section E Structure Reports Online, 64 (9). i53-i54 doi:10.1107/s1600536808024173
Plain TextHenderson, Rachel R., Yang, Hexiong, Downs, Robert T., Jenkins, Robert A. (2008) Redetermination of conichalcite, CaCu(AsO4)(OH). Acta Crystallographica Section E Structure Reports Online, 64 (9). i53-i54 doi:10.1107/s1600536808024173
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Abstract/NotesThe crystal structure of conichalcite [calcium copper(II) arsenate(V) hydroxide], with ideal formula CaCu(AsO4)(OH), was redetermined from a natural twinned specimen found in the Maria Catalina mine (Chile). In contrast to the previous refinement from photographic data [Qurashi & Barnes (1963). Can. Mineral.
7, 561–577], all atoms were refined with anisotropic displacement parameters and with the H atom located. Conichalcite belongs to the adelite mineral group. The Jahn–Teller-distorted [CuO6] octahedra share edges, forming chains running parallel to [010]. These chains are cross-linked by eight-coordinate Ca atoms and by sharing vertices with isolated AsO4 tetrahedra. Of five calcium arsenate minerals in the adelite group, the [MO6] (M = Cu, Zn, Co, Ni and Mg) octahedron in conichalcite is the most distorted, and the donor–acceptor O—H...O distance is the shortest.

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