日本地球惑星科学連合2018年大会

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[JJ] 口頭発表

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG60] 岩石・鉱物・資源

2018年5月23日(水) 09:00 〜 10:30 A04 (東京ベイ幕張ホール)

コンビーナ:門馬 綱一(独立行政法人国立科学博物館)、野崎 達生(海洋研究開発機構海底資源研究開発センター)、齊藤 哲(愛媛大学大学院理工学研究科、共同)、土谷 信高(岩手大学教育学部地学教室)、座長:門馬 綱一土谷 信高

09:30 〜 09:45

[SCG60-03] 奈良県天川村産イリディセントガーネットの収束電子回折分析

*三宅 亮1伊神 洋平1張 育銓1下林 典正1津田 健治2早坂 祐一郎3 (1.京都大学・理学研究科・地球惑星科学専攻、2.東北大学・学際科学フロンティア研究所、3.東北大学・先端電子顕微鏡センター)

キーワード:イリディセントガーネット、収束電子回折法

Grossular (Ca3Al2Si3O12) - andradite (Ca3Fe3+2Si3O12) 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/Fe3+ 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 (STEM) to investigate the symmetry to investigate the symmetry of iridescent garnet, especially from the core of Fe-rich lamella to the core of Al-rich lamella, in more detail. And furthermore, chemical map by STEM-EDS were obtained from the same area as STEM-CBED analysis.
A thin section (100μm thickness) cut parallel to the (001) face through the center of the crystal was prepared from an euhedral single crystal of iridescent garnet with well-developed rhombic dodecahedral {110} facets. TEM specimens with various crystal planes, (001), (110), and (111) were prepared from the thin section by using a focused ion beam technique (ThermoFischerScientific: Quanta 200 3DS, Helios G3 CX) and then TEM (JEOL, JEM-2100F; ThermoFischerScientific, Titan3 60-300 Double Corrector) observation was carried out to investigate the symmetry and analysis of chemical composition.
CBED patterns in the core of Fe-rich lamella have the clear high order Laue zone (HOLZ) lines in (111), (110) and (001) TEM samples and mirror, 2, 3, 4-fold axes can be identified. These results show that the symmetry of Fe-rich lamella core has Ia-3d. In the core of Al-rich lamella, on the other hand, although HOLZ lines were observed in CBED patterns, no symmetryical elements, such mirror, 2-fold axis and so on, were identified. Thus the symmetry of Al-rich lamella is I(P)-1 or I(P)1. Around the boundary between Fe-rich and Al-rich lamellae, Al/Fe chemical components gradually change. Clear CBED patterns and HOLZ lines were not observed and no symmpetrical elements were identified exactly in all samples. In all TEM samples, however, the analysis of very weak and no-clear HOLZ line shows that mirror plane may exit normal to lamella boundary.

Reference
Shimobayashi et al. (2005) Abstracts of Annual Meeting of the Mineralogical Society of Japan ,p80.
Chang et al. (2016) Japan Geoscience Union MEETING 2016, SCG56-P04
Chang et al. (2017) JpGU-AGY joing meeting 2017, SCG73-01