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Twin Orthorhombic Structure of Haüyne from Sakrofano (Italy)

机译:Sakrofano(意大利)的Haüyne的双正交结构

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摘要

The structure of hauyne from Sakrofano (Italy) is solved using the superstructure reflections, which double the unit cell parameters in three directions. The cubic symmetry of the diffraction pattern of hauyne results from the twinning of the equidimensional orthorhombic components by the [111] threefold axis. The structure is refined in the orthorhombic space group Pba2 with the unit cell parameters a = b = 12.872(7) A and c = 9.102(3) A in the anisotropic approximation to R = 0.043 for 1737 reflections. Compared to high-potassium hauyne from Arissia (Italy), the mineral studied contains potassium in smaller amounts and the distribution of K, Na, and Ca atoms over four body diagonals of the cell is ordered, which apparently causes the lowering of symmetry from cubic to orthorhombic.
机译:来自Sakrofano(意大利)的hauyne的结构是使用上层结构反射来求解的,该结构将单位晶胞参数在三个方向上加倍。 hauyne的衍射图样的立方对称性是由[111]三重轴对等维正交晶体成分的孪生产生的。在正交各向异性空间组Pba2中,通过单位近似参数a = b = 12.872(7)A和c = 9.102(3)A来精细化结构,各向异性近似为1737次反射,R = 0.043。与来自Arissia(意大利)的高钾hauyne相比,所研究的矿物含有少量的钾,并且该单元的四个对角线上的K,Na和Ca原子的分布是有序的,这显然导致立方晶的对称性降低到斜方。

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