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Refinement of the structure of ζ-Nb2O5and its relationship to the rutile and thoreaulite structures

机译:ζ-Nb2O5结构的细化及其与金红石和钴云母结构的关系

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The crystal structure of ζ-Nb2O5, space groupC2/c, a12.740(2),b4.8830(6),c5.5609(6)Å,β105.02(1)°, Z 4, has been refined toR1.6 for 457 observed reflections (MoKα). The coordination polyhedron of the niobium atom is a distorted octahedron; the crystal structure consists of two-octahedron-thick, rutile-like layers separated by crystallographic shear (CS) planes. Relative to the rutile structure, these planes are indexed (101) and adjacent layers are related by the CS vector. Members of the thoreaulite-foordite series have topologically identical two-octahedron-thick (101) sheets; however, here the CS vectorr, coupled with the translation vectorrresults in the insertion of a plane of square antiprism interstices between adjacent octahedral sh
机译:ζ-Nb2O5,空间群C2/c,a12.740(2),b4.8830(6),c5.5609(6)Å,β105.02(1)°,Z 4的晶体结构已在457次观测反射(MoKα)中精炼至R1.6%。铌原子的配位多面体是扭曲的八面体;晶体结构由两个八面体厚的金红石状层组成,由晶体剪切 (CS) 平面隔开。相对于金红石结构,这些平面被索引 (101),相邻层通过 CS 向量相关。thoreaulite-foordite 系列的成员具有拓扑学上相同的两个八面体厚 (101) 片;然而,这里 CS 向量与平移向量 r 相结合,导致在相邻的八面体 sh 之间插入方形反棱镜间隙平面

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  • 来源
    《mineralogy and petrology》 |1991年第3期|217-223|共页
  • 作者

    Dr.T.S.Ercit;

  • 作者单位

    Canadian Museum of Nature;

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  • 正文语种 英语
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