Petermegawite, Al6(Se4+O3)3[SiO3(OH)](OH)9⋅10H2O, a New AI-Bearing Selenite Mineral, from the El Dragón Mine, Potosí, Bolivia

IF 1.3
Hexiong Yang, X. Gu, Michael M. Scott, R. Jenkins, R. Gibbs, J. McGlasson, R. Downs
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Abstract

A new mineral species, petermegawite, ideally Al6(Se4+O3)3[SiO3(OH)](OH)9⋅10H2O, was discovered at the El Dragón mine, Potosí Department, Bolivia. It occurs as aggregates of bladed or tabular crystals. Associated minerals are Co-bearing krut′aite–penroseite (matrix), chalcomenite, ‘clinochalcomenite’ (not IMA approved), molybdomenite, lepidocrocite, goethite, ahlfeldite, and calcite. Petermegawite is colorless in transmitted light and transparent with a white streak and vitreous luster. It is brittle and has a Mohs hardness of 2–2½. Cleavage is perfect on {001}. The measured and calculated densities are 2.27(5) and 2.32 g/cm3, respectively. Optically, petermegawite is biaxial (+), with α = 1.545(5), β = 1.554(5), γ = 1.567(5) (white light). An electron microprobe analysis yielded an empirical formula (based on 10 non-H cations pfu) of Al6.00[(Se0.89S0.11)Σ1.00O3]3[(Si0.90Al0.07)Σ0.97O2.81(OH)1.19](OH)9⋅10H2O, which can be simplified to Al6[(Se,S)O3]3[(Si,Al)O3(OH)](OH)9⋅10H2O. Petermegawite is orthorhombic, space group Cmc21 with unit-cell parameters a = 16.2392(2), b = 10.96370(10), c = 15.3367(2) Å, V = 2730.57(5) Å3, and Z = 4. Its crystal structure is characterized by clusters of six-membered rings of edge-sharing AlO6 octahedra with an SiO3(OH) tetrahedron situated at the center of each ring and three Se4+O3 triangular pyramids appended outside the ring. These clusters are joined together by hydrogen bonds to form heteropolyhedral layers parallel to (001). The H2O molecules that are not bonded to any non-H cations are sandwiched between the layers. The cluster formed by a six-membered AlO6 octahedral ring with an SiO3OH tetrahedron at the center of the ring in petermegawite has the composition [Al6(SiO3OH)O6(OH)9(H2O)6]6−. It is topologically identical to the clusters of composition [Al6(AsO4)O7(OH)9(H2O)5]8− that are found in bettertonite and penberthycroftite. As a new polyoxometalate building block, this type of cluster may be expressed with a general chemical formula [TM6X25], where T = tetrahedrally coordinated cation, M = octahedrally coordinated cation, and X = O, OH, H2O.
玻利维亚Potosí El Dragón矿Al6(Se4+O3)3[SiO3(OH)](OH)9⋅10H2O:一种新型含ai亚硒酸盐矿物
在玻利维亚Potosí省El Dragón矿发现了一种新的矿物,名为petermegawitte,理想状态为Al6(Se4+O3)3[SiO3(OH)](OH)9⋅10H2O。它以片状或板状晶体的聚集体形式出现。伴生矿物有含钴的金榴辉石(基质)、黄铜矿、斜铜矿(未获IMA批准)、辉钼矿、绢云母、针铁矿、铁长石和方解石。透射光无色,透明,有白色条纹和玻璃光泽。它很脆,莫氏硬度为2-2½。乳沟是完美的{001}。实测密度和计算密度分别为2.27(5)和2.32 g/cm3。光学上,petermegawhite是双轴(+),α = 1.545(5), β = 1.554(5), γ = 1.567(5)(白光)。电子探针分析得到了Al6.00[(Se0.89S0.11)Σ1.00O3]3[(Si0.90Al0.07)Σ0.97O2.81(OH)1.19](OH)9⋅10H2O的经验式(基于10个非h阳离子pfu),可简化为Al6[(Se,S)O3]3[(Si,Al)O3(OH)](OH)9⋅10H2O。Petermegawite为正交空间群Cmc21,单元胞参数a = 16.2392(2), b = 10.96370(10), c = 15.3367(2) Å, V = 2730.57(5) Å3, Z = 4。其晶体结构的特点是由六元环组成的共边AlO6八面体簇,每个环的中心有一个SiO3(OH)四面体,环外有三个Se4+O3三角形金字塔。这些团簇通过氢键连接在一起,形成平行于(001)的异多面体层。没有与非氢离子结合的水分子夹在两层之间。由六元AlO6八面体环和SiO3OH四面体在petermegawitte环中心形成的团簇的组成为[Al6(SiO3OH)O6(OH)9(H2O)6]6−。它在拓扑结构上与较长石和笔长石中发现的[Al6(AsO4)O7(OH)9(H2O)5]8−组成簇相同。该类簇作为一种新型的多金属氧酸盐构建块,可以用一般的化学式[TM6X25]来表示,其中T =四面体配位阳离子,M =八面体配位阳离子,X = O, OH, H2O。
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