BRADACZEKITE, NACU4(ASO4)3, A NEW MINERAL SPECIES FROM THE TOLBACHIK VOLCANO, KAMCHATKA PENINSULA, RUSSIA

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dc.contributor.author Filatov S.K.
dc.contributor.author Vergasova L.P.
dc.contributor.author Gorskaya M.G.
dc.contributor.author Krivovichev S.V.
dc.contributor.author Burns P.C.
dc.contributor.author Ananiev V.V.
dc.date.accessioned 2021-02-20T08:18:57Z
dc.date.available 2021-02-20T08:18:57Z
dc.date.issued 2001
dc.identifier https://elibrary.ru/item.asp?id=13374180
dc.identifier.citation The Canadian Mineralogist, 2001, 39, 4, 1115-1119
dc.identifier.issn 0008-4476
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/25316
dc.description.abstract Bradaczekite, NaCu4(ASO(4))(3), was discovered in a fumarole in the North Breach of the Great fissure Tolbachik eruption (GFTE) in 1975-1976, Kamchatka Peninsula, Russia. Bradaczekite forms allregates of dark blue plates elongate along [102]. The well-developed forms are {010}, {(3) over bar 11}, {111} and {(1) over bar 12}. The forms {301}, {001}, {(3) over bar 21}, {101}, {100}, {021}, {110}, {131}, {(1) over bar 11} and {341} are common. Associated minerals are hematite, tenorite, lammerite, urusovite, orthoclase and johillerite. The mineral has an adamantine luster and a light blue to white streak. No cleavage has been observed. The mineral is transparent, biaxial, optically negative, alpha 1.76(1), beta 1.92(1), gamma 1.96(1), 2V(calc) 50.0 degrees. The optical orientation is Z = b, X Lambda c = 23 degrees in the obtuse beta angle. Bradaczekite shows strong pleochroism: X violet-red, Y green, Z greenish blue. The mineral is monoclinic, space group C2/c, a 12.051(1), b 12.434(1), c 7.2662(7) Angstrom, beta 117.942(1)degrees, V 961.8(2) Angstrom (3), Z = 4, D-calc = 4.77(1) g/cm(3) (for the empirical formula). The strongest eight lines of the X-ray powder-diffraction pattern [d in Angstrom (l)(hkl)] are: 6.22(13)(020), 3.60(21)((2) over bar 02, (1) over bar 31), 3.43(100)((1) over bar 12, 310), 3.21(35)(002), 2.791(24)((4) over bar 02), 2.696(18)(330), 2.683(30)(240), and 2.665(17)(400). Electron-microprobe analyses yielded: Na2O 5.17 (4.37-5.78), K2O 0.35 (0.14-0.80), CuO 43.13 (41.31-45.22), ZnO 0.79 (0.19-1.18), Fe2O3 0.38 (0.03-1.05), As2O5 49.62 (48.61-50.66), V2O5 0.13 (0-0.90), total 99.55 (97.69-101.56) wt.%. The empirical formula, normalized to O = 12 apfu (atoms per formula unit), is (Na1.6K0.05)(Sigma1.21)(Cu3.74Zn0.07Fe0.033+)(Sigma3.84)(As3.00V0.01)(Sigma3.01)O-12, close to the ideal NaCu4(AsO4)(3) confirmed by crystal-structure analysis. The mineral is named in honor of Hans Bradaczek, crystallographer at the Free University of Berlin.
dc.subject bradaczekite
dc.subject new mineral species
dc.subject arsenate
dc.subject Tolbachik volcano
dc.subject Kamchatka Peninsula
dc.subject Russia
dc.title BRADACZEKITE, NACU4(ASO4)3, A NEW MINERAL SPECIES FROM THE TOLBACHIK VOLCANO, KAMCHATKA PENINSULA, RUSSIA
dc.type Статья


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