CRYSTAL STRUCTURE OF MAHNERTITE

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dc.contributor.author Pushcharovsky D.Yu.
dc.contributor.author Zubkova N.V.
dc.contributor.author Teat S.J.
dc.contributor.author MacLean E.J.
dc.contributor.author Sarp H.
dc.date.accessioned 2022-03-30T02:31:52Z
dc.date.available 2022-03-30T02:31:52Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13467521
dc.identifier.citation European Journal of Mineralogy, 2004, 16, 4, 687-692
dc.identifier.issn 0935-1221
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/36740
dc.description.abstract Mahnertite, (Na0.88Ca0.12)Cu-2.75[AsO4](2)Cl-0.62.3.63H(2)O, M = 565.17, is tetragonal, with space group I4/mmm, a = 10.037(1), c = 23.739(1) Angstrom, V = 2391.5(4) Angstrom(3), Z = 8, rho(o) = 3.32, rho(c) = 3.14 g/cm(3), mu 9.78 mm(-1). The crystal structure of mahnertite was solved and refined against data collected at the Daresbury Synchrotron Radiation Source, using a 20 x 20 x 2 mum(3) single crystal, lambda = 0.6898 Angstrom, F(000) = 2150, R = 0.049 for 639 reflections with I > 2sigma(I). The structure consists of sheets parallel to (001), which comprise two symmetrically independent distorted Cu 5-vertex square pyramids Cuphi5 (phi = O, Cl or H2O) as well as AsO4 tetrahedra. Four Cuphi(5) pyramids located around the 4-fold axis share edges to form clusters linked by AsO4 tetrahedra. The sheets are linked by the common apical vertex of the Cu(2)phi(5) polyhedra. As a result, a heterogeneous framework is formed. (Na,Ca) atoms, additional Cu(3) cations and H2O molecules are located in the interlayers. The mineral is structurally related to zdenekite, NaPbCu5(AsO4)(4)Cl.5H(2)O.
dc.subject Mahnertite
dc.title CRYSTAL STRUCTURE OF MAHNERTITE
dc.type Статья


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