Synchysite-(Y)(新奇钙钇矿)的晶体结构
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The Crystal Structure of Synchysite-(Y), YCa(CO3)F
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    摘要:

    新奇钙忆矿(synehysite-(Y)], YCa(C03)F,经单晶X射线魏森堡法研究表明属单斜晶系,空 间群为C2/c,由四圆衍射仪精化求得的晶胞参数为:a=12.039(3)A, b=6.950(1)A,c=18.43(6)A. β=102.45(2)°。在四圆衍射仪上采用MoKa辐射收集的三维衍射数据,已经劳伦兹偏振因子校正,未做吸收校正。总共1019个衍射点的强度数据,应用全矩阵最小二乘法对结构进行了精化,经各向异性温度因子校正后,R因子为0.086. 新奇钙忆矿具有(001)层状结构特征,Ca层和(YF)层由碳酸根层隔开.层的堆垛方式与C2/c白 云母类似,其中Ca层与白云母中的K层相对应,C03层和(YF)层则分别对应于白云母中的四面体层和八面体层.由于Ca层上下两边的CO3层的相对错动,形成了类似于2M2白云母的堆垛多型结构。

    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.

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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.

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