首页> 外文期刊>The American mineralogist >Vasilseverginite, Cu9O4(AsO4)(2)(SO4)(2), a new fumarolic mineral with a hybrid structure containing novel anion-centered tetrahedral structural units
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Vasilseverginite, Cu9O4(AsO4)(2)(SO4)(2), a new fumarolic mineral with a hybrid structure containing novel anion-centered tetrahedral structural units

机译:Vasilsevergite,Cu9O4(ASO4)(2)(SO4)(2),一种新的富马隆矿物质,具有含有新型阴离子的四面体结构单元的混合结构

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摘要

The new mineral vasilseverginite, ideally Cu9O4(AsO4)(2)(SO4)(2), was found in the Arsenatnaya fumarole at the second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. It is associated with tenorite, lammerite, stranskiite, lammerite-beta, langbeinite, dolerophanite, sanidine, hematite, and gahnite. Vasilseverginite occurs as prismatic crystals up to 0.02 x 0.02 x 0.06 mm(3) combined in groups or interrupted crusts up to 1 x 2 cm(2) in area and up to 0.1 nun thick. It is transparent, bright green, with vitreous luster. D-calc is 4.41 g.cm(-3). Vasilseverginite is optically biaxial (-), alpha 1.816(5), beta 1.870(5), gamma 1.897(5), estimated 2V is 30(15)degrees. Chemical composition (wt%, electron-microprobe) is: CuO 64.03, ZnO 0.79, Fe2O3 0.25, P2O5 0.05, As2O5 20.83, SO 3 14.92, total 100.87. The empirical formula calculated on O = 20 apfu is (Cu8.78Zn0.11Fe0.033+)(Sigma 8).92As1.98P0.01S2.03O20. Vasilseverginite is monoclinic, P2(1)/n, a = 8.1131(4), b = 9.9182(4), c = 11.0225(5) angstrom, beta = 110.855(2)degrees, V = 828.84(6) angstrom(3), and Z = 2. The strongest reflections in the powder XRD pattern [d,angstrom(I)(hkl)] are: 7.13(41)(10 (1) over bar), 5.99(70)(110, 11 (1) over bar), 5.260(100)(101), 4.642(46)(111), 3.140(31)(03 (1) over bar), 2.821(35)(02 (3) over bar), 2.784(38)(13 (2) over bar, 03 (2) over bar), 2.597(35)(20 (4) over bar), and 2.556(50) (23 (1) over bar, 212). The crystal structure, solved using single-crystal X-ray diffraction data, R-1 = 0.025, is based upon complex [O4Cu9](10+) layers parallel to ((1) over bar 01) that are composed of edge- and corner-sharing (OCu4) tetrahedra. The topology is unprecedented in inorganic structural chemistry. The crystal structure can be considered a hybrid of the structures of popovite Cu5O2(AsO4)(2) and dolerophanite Cu2O(SO4) according to the scheme Cu9O4(AsO4)(2)(SO4)(2) = Cu5O2(AsO4)(2) + 2Cu(2)O(SO4). The chemical hybridization does not result in a significant increase in chemical complexity of vasilseverginite compared to the sum of those of popovite and dolerophanite, whereas the structural hybridization leads to the doubling of structural information per unit cell. The mineral is named in memory of the outstanding Russian mineralogist, geologist, and chemist Vasiliy Mikhailovich Severgin (1765-1826).
机译:在俄罗斯堪察加半岛托尔巴契克大裂缝喷发北部突破点的第二个火山渣锥处的Arsenatnaya喷气孔中发现了新矿物凡士林石,理想情况下为Cu9O4(AsO4)(2)(SO4)(2)。它与透闪石、透闪石、透闪石、透闪石β、蓝闪石、白云石、透闪石、赤铁矿和辉石有关。Vasilseverginite以高达0.02 x 0.02 x 0.06 mm(3)的棱柱状晶体或面积达1 x 2 cm(2)且厚度达0.1 mm的间断结壳形式出现。透明,亮绿色,有玻璃光泽。D-calc为4.41克厘米(-3)。Vasilseverginite在光学上为双轴(-),α1.816(5),β1.870(5),γ1.897(5),估计2V为30(15)度。化学成分(重量百分比,电子探针)为:CuO 64.03,ZnO 0.79,Fe2O3 0.25,P2O5 0.05,As2O5 20.83,SO 3 14.92,总计100.87。O=20 apfu时计算的经验公式为(Cu8.78Zn0.11Fe0.033+)(σ8)。92As1。98P0。01S2。03O20。Vasilseverginite为单斜,P2(1)/n,a=8.1131(4),b=9.9182(4),c=11.0225(5)埃,β=110.855(2)度,V=828.84(6)埃(3),Z=2。粉末XRD图谱[d,埃(I)(hkl)]中最强的反射为:7.13(41)(10(1)超过棒材)、5.99(70)(110,11(1)超过棒材)、5.260(100)(101)、4.642(46)(111)、3.140(31)(03(1)超过棒材)、2.821(35)(02(3)超过棒材)、2.784(38)(13(2)超过棒材、03(2)超过棒材)、2.597(35)(20(4)超过棒材)和2.556(50)(23(1)超过棒材、212)。使用单晶X射线衍射数据(R-1=0.025)求解的晶体结构基于复杂的[O4Cu9](10+)层,平行于棒01上方的((1)层,该层由边角共享(OCu4)四面体组成。这种拓扑结构在无机结构化学中是前所未有的。根据方案Cu9O4(AsO4)(2)(SO4)(2)=Cu5O2(AsO4)(2)+2Cu(2)O(SO4),晶体结构可被视为popovite Cu5O2(AsO4)(2)和白云闪长岩Cu2O(SO4)结构的混合体。与popovite和Doleropanite的化学复杂性之和相比,化学杂交不会导致Vasilverginite的化学复杂性显著增加,而结构杂交会导致每个单位细胞的结构信息加倍。该矿物的命名是为了纪念杰出的俄罗斯矿物学家、地质学家和化学家瓦西里·米哈伊洛维奇·塞韦金(Vasily Mikhailovich Severgin,1765-1826)。

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