Redetermination of the Crystal Structure of Vesignieite

Redetermination of the Crystal Structure of Vesignieite
  • 摘要
  • | |
  • 访问统计
  • | |
  • 相似文献
  • |
  • 引证文献
  • | |
  • 文章评论
    摘要:

    Vesignieite, Cu_3Ba(VO_4)_2(OH)_2, crystallizes in space group C_2 / m with a°=1.0270(2), b°=0.5911(1),c°=0.7711(2)nm and β=116.42(3)°. The intensity data were collected with the RIGAKU RASA-IISsingle-crystal four-circle diffractometer. The structure was determined by Patterson and Fourier methods andrefined by the least-square technique to a final R index of 0.051 for 614 independent diffraction points with|F? |>3σ|F?|. The crystal structure analysis shows that vesignieite has a layer structure parallel to (001). The powder diffraction lines were reindexed.

    Abstract:

    Vesignieite, Cu_3Ba(VO_4)_2(OH)_2, crystallizes in space group C_2 / m with a°=1.0270(2), b°=0.5911(1),c°=0.7711(2)nm and β=116.42(3)°. The intensity data were collected with the RIGAKU RASA-IISsingle-crystal four-circle diffractometer. The structure was determined by Patterson and Fourier methods andrefined by the least-square technique to a final R index of 0.051 for 614 independent diffraction points with|F? |>3σ|F?|. The crystal structure analysis shows that vesignieite has a layer structure parallel to (001). The powder diffraction lines were reindexed.

    参考文献
    相似文献
    引证文献
引用本文

.1991. Redetermination of the Crystal Structure of Vesignieite[J]. ACTA GEOLOGICA SINICA(English edition),65(2):

复制
分享
文章指标
  • 点击次数:1147
  • 下载次数: 81
  • HTML阅读次数: 0
  • 引用次数: 0
历史
文章二维码