The Crystal Structure of Synchysite-(Y), YCa(CO3)F
DOI:
CSTR:
Author:
Affiliation:

Clc Number:

Fund Project:

  • Article
  • |
  • Figures
  • |
  • Metrics
  • |
  • Reference
  • |
  • Related
  • |
  • Cited by
  • |
  • Materials
  • |
  • Comments
    Abstract:

    The monoclinic space group of synchysite-(Y) was determined as C2/c by single-crystal crystallographic research using W eissenberg method. The unit cell parameters obtained and refined on a four-circle diffractometer are a 12.039(3),b 6.950(1),c 18.436 (6)A,and β 102.45 (2)°.From 1350 independent reflections collected by means of MoKa radiation on the same instrument, 1019 reflections with I>3σ (I) were corrected for Lorentz and polarization factors; however,no absorption correction was conducted. After the refinement with anisotropic temperature factors by the full matrix least square method, the residual index for the 1019 reflections was R=0.086. Synchysite-(Y) possesses a characteristic (001) layer structure, with layers of (Ca) and (YF) separated by layers of carbonate groups. The layers stack in a manner analogous to C2/c muscovite, where (Ca) layers in synchysite-(Y) are equivalent to (K) layers in muscovite, (CO3) layers in synchysite-(Y),to layers of tetrahedra in muscovite, and (YF) layers in synchysite-(Y),to layers of octahedra in muscovite. As in m uscovite,offsets of adjacent (CO3) layers are similar to those in 2M2,which results in the layer-stacking polytype structure.

    Reference
    Related
    Cited by
Get Citation

王立本, 周康靖,1995,Synchysite-(Y)(新奇钙钇矿)的晶体结构[J].岩石矿物学杂志,14(4):336~344. Wang Liben,1995,The Crystal Structure of Synchysite-(Y), YCa(CO3)F[J]. Acta Petrologica et Mineralogica,14(4):336~344.

Copy
Share
Article Metrics
  • Abstract:
  • PDF:
  • HTML:
  • Cited by:
History
  • Received:
  • Revised:
  • Adopted:
  • Online:
  • Published:
Article QR Code