CRYSTAL STRUCTURE OF NA4[CU4O2(SO4)4]·MECL (ME: NA, CU, []) - THE SYNTHETIC NA-ANALOGUE OF PIYPITE (CARATIITE)

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dc.contributor.author Kahlenberg V.
dc.contributor.author Piotrowski A.
dc.contributor.author Giester G.
dc.date.accessioned 2021-01-30T12:24:32Z
dc.date.available 2021-01-30T12:24:32Z
dc.date.issued 2000
dc.identifier https://elibrary.ru/item.asp?id=13995580
dc.identifier.citation Mineralogical Magazine, 2000, 64, 6, 1099-1108
dc.identifier.issn 0026-461X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/24074
dc.description.abstract The crystal structure of Na4[Cu4O2(SO4)4] MeCl (Me: Na, Cu, Box) has been solved by direct methods and refined to R1 = 0.028 using 2466 independent reflections. The compound is tetragonal with space group P4/n, a = 18.451(1) Å, c = 4.9520(2) Å, Z = 4. The two main building units running parallel to the c-axis comprise: (1) slabs containing SO4 and OCu4 tetrahedra; and (2) chains of corner sharing Me(Cl,O)6 octahedra. The displacement ellipsoids of the atoms occupying the Me sites and of the Cl ions indicate a short-range static disorder. Copper in the slabs exhibits a (4+1) coordination. Both elements form a tunnel structure in which additional Na atoms are incorporated for charge compensation. The structure is closely related to the mineral piypite (K4Cu4O2(SO4)4 MeCl (Me: Na, Cu, Box)): a ≈ √ 2 . apiy.; c ≈ cpiy.. Furthermore, the structure has a pronounced pseudo-translational symmetry: apart from some of the oxygen sites, all of the nineteen crystallographically distinct positions are related by a pseudo F centring.
dc.title CRYSTAL STRUCTURE OF NA4[CU4O2(SO4)4]·MECL (ME: NA, CU, []) - THE SYNTHETIC NA-ANALOGUE OF PIYPITE (CARATIITE)
dc.type Статья


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