THE CRYSTAL STRUCTURE OF VASILYEVITE, (HG22+10 O6 I3 (BR, CL )3 (CO3)

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dc.contributor.author Cooper M.A.
dc.contributor.author Hawthorne F.C.
dc.date.accessioned 2022-02-19T06:47:09Z
dc.date.available 2022-02-19T06:47:09Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=14099954
dc.identifier.citation The Canadian Mineralogist, 2003, 41, 5, 1173-1181
dc.identifier.issn 0008-4476
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35558
dc.description.abstract The crystal structure of vasilyevite, ideally (Hg22+10 O6 I3 Br2 Cl (CO3), triclinic, a 9.344(2), b 10.653(2), c 18.265(4) Å, α 93.262(5), β 90.548(4), Υy 115.422(4)°, V 1638.3(9) Å3, space group P1̄, Z = 2, D(calc) = 9.57 g cm-3, has been solved by direct methods and refined to an R1, index of 8.9% for 3400 unique reflections measured with MoKα X-radiation on a four-circle diffractometer equipped with a CCD detector. There are twenty unique Hg sites that are associated as pairs of sites with pair separations of 2.533 to 2.593 Å; this association of Hg atoms is typical of Hg+ cations pairing to form (Hg2)2+ dimers. Each (Hg2)2+ dimer is extended at each end by bonding to axial O atoms with Hg-O distances in the range 2.00 to 2.32 Å, with one dimer showing a terminal I atom with a very short Hg-I distance of 2.75 Å. These [φ-Hg-Hg-φ] tetramers form near-linear arrangements that are surrounded by several meridional anions, O atoms at distances from 2.44 to 2.85 Å, mixed (Cl,Br) sites at distances from 2.89 to 3.78 Å. and I atoms at distances from 3.11 to 4.02 Å. Bonds to axial anions make angles of <23° with the Hg-Hg axis, involving the Hg atoms to which they are bonded; bonds to meridional anions make angles of <31° with the perpendicular to the Hg-Hg axis, involving the Hg atoms to which they are bonded. There is one site, labeled C,S, that is surrounded by a triangle of O atoms at a mean distance of 1.25 Å: the presence of S in the chemical composition and the refined scattering at the C,S site indicates that this site is occupied by both (CO3) and S2- in the ratio 0.85 : 0.15. There are three distinct I sites occupied solely by I- anions that are [8]- or [9]-coordinated by Hg cations. There are three X sites that are occupied by 0.73 Br + 0.27 Cl, 0.69 Br + 0.31 Cl, and 0.22 Br + 0.78 Cl and are [7]- and [8]-coordinated by Hg cations. The fundamental building block of the vasilyevite structure is the strongly bonded [φ-Hg-Hg-φ] tetramer. These groups link together at their anion vertices to form a complex interpenetrating framework of two discrete three- and four-connected nets. The halogen atoms and the (CO3) and S2- anions occur in the interstices of the two nets and serve to stabilize the nets via additional weak linkages to Hg atoms.
dc.subject vasilyevite
dc.subject crystal structure
dc.subject Hg–Hg dumbbells
dc.subject electron-microprobe analysis
dc.subject mercurous oxide iodide bromidechloride carbonate mineral
dc.title THE CRYSTAL STRUCTURE OF VASILYEVITE, (HG22+10 O6 I3 (BR, CL )3 (CO3)
dc.type Статья


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