A. Miyake, Y. Igami, yuhchyuan Chang, N. Shimobayashi, K. Tsuda
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引用次数: 0
摘要
Grosssular(Ca3Al2Si3O12)-红柱石(Ca3Fe3+2Si3O1 2)石榴石固溶体(空间群,Ia-3d),称为granite系列,经常表现出光学双折射和虹彩。通过透射电子显微镜(TEM)(例如,Shimobayashi等人,2005),来自日本奈良县Tenkawa的虹彩石榴石具有精细的层状结构(厚度约为100-300nm),Al/Fe3+比率差异较小。我们之前的研究(Chang et al.,20162017)报道了额外的反射,110、200、411等等,在富Al细晶片层的选区电子衍射(SAD)图中检测到破坏Ia-3d对称性的现象,该富Al细片层的晶体家族为三斜晶系,晶格类型为I晶格,表明在会聚光束电子衍射(CBED)图中空间群为I-1或I1。Chang等人(2017)还报道了片层核心和富铝和富铁片层边界周围的CBED模式不同。在这项研究中,我们通过扫描TEM检查CBED
PM-08CBED analysis of iridescent garnets from Tenkawa, Nara Prefecture, Japan
Grossular (Ca 3 Al 2 Si 3 O 12 ) - andradite (Ca 3 Fe 3+2 Si 3 O 12 ) garnet solid solutions (space group, Ia-3d), termed grandite series, often exhibit optical birefringence and iridescence. Iridescent garnet from Tenkawa, Nara Prefecture, Japan, has the fine lamellar texture (ca. 100-300 nm in thickness) with small differences in Al/Fe 3+ ratio by transmission electron microscope (TEM) (e.g., Shimobayashi et al., 2005). Our previous studies (Chang et al., 2016, 2017) reported that extra reflections, 110, 200, 411 and so on, to break the symmetry of Ia-3d were detected in selected area electron diffraction (SAD) patterns from Al-rich fine lamellae and the crystal family of this Al-rich fine lamella is triclinic and lattice type is I-lattice and suggest the space group is I-1 or I1 in the convergent-beam electron diffraction (CBED) pattenrs. Chang et al. (2017) also reported that CBED patterns in the core of lamella and around the boundary between Al-rich and Fe-rich lamellae were different. In this study, we examine CBED by scanning TEM
期刊介绍:
Microscopy, previously Journal of Electron Microscopy, promotes research combined with any type of microscopy techniques, applied in life and material sciences. Microscopy is the official journal of the Japanese Society of Microscopy.