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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Polytypism and microstructures of the mixed-layer member B_2S, CaCe_3(CO_3)_4F_3 in the bastnaesite-(Ce)-synchysite-(Ce) series
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Polytypism and microstructures of the mixed-layer member B_2S, CaCe_3(CO_3)_4F_3 in the bastnaesite-(Ce)-synchysite-(Ce) series

机译:镁橄榄石-(Ce)-杂合体-(Ce)系列B_2S,CaCe_3(CO_3)_4F_3混合层成员的多型性和微观结构

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摘要

The crystal structures and polytypism of bastnaesite-(Ce) (CeCO_3F, B layer) and synchysite-(Ce) (CeCO_3F·CaCO_3, S layer) mineral series are very complicated in Sichuan Province, Southwest China. Four new polytypes: 6R, 2H_2, 4H and 12H of the mixed-layer member CaCe_3(CO_3)_4F_3 (B_2S) of this series were discovered by X-ray diffraction analyses and high resolution transmission electron microscopy, structural symmetry, cell and subcell parameters, possible space group, and structural stacking mode (dededgfgl…). They reveal that the mixed-layer member B_2S is formed by the ordered stacking of two structural unit layers of bastnaesite-(Ce) (B layer) and one unit layer of synchysite-(Ce) (S layer) along the c direction. The forming of the new polytypes may depend on distributions and the periodical variation of orientation of the [CO_3] groups between the unit layers of B_2S. We have observed the {0001} microtwin of the 6R polytype and the syntactic intergrowths among the different polytypes formed by stacking faults in B_2S.
机译:在中国西南地区的四川省,贝氏体-(Ce)(CeCO_3F,B层)和杂合物-(Ce(CeCO_3F·CaCO_3,S层)矿物系列的晶体结构和多型性非常复杂。通过X射线衍射分析和高分辨率透射电子显微镜,结构对称性,细胞和亚细胞参数发现了该系列混合层成员CaCe_3(CO_3)_4F_3(B_2S)的四个新多型:6R,2H_2、4H和12H ,可能的空间组和结构堆叠模式(dededgfgl ...)。他们揭示出,混合层构件B_2S是通过沿c方向有序地堆叠两块贝氏体-(Ce)的结构单元层(B层)和一层合硼铁矿-(Ce)的结构单元层(S层)而形成的。新多型体的形成可以取决于B_2S的单元层之间的[CO_3]基团的分布和取向的周期性变化。我们已经观察到6R多型的{0001}小孪生子和B_2S中的堆积断层形成的不同多型之间的句法共生。

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