まとめ
高圧のシリカポリモルフであるコエサイトは,タイのムオン・ノング型のテクタイトで発見された. これらのテクタイトは最小限の変化を示しており,高温による急速な冷却を示しています.
科学分野:
- 地質化学 地質化学
- ミネラロジーは,鉱物学です.
- マテリアルサイエンス 材料科学
背景:
- テクタイトは,隕石の衝突で放出された地上の破片から形成された天然のガラスです.
- ムョンノング型のテクティットは,独特の質感や構成のバリエーションで知られています.
研究 の 目的:
- ムオン・ノン型テクティスのインクルージョン内の鉱物相を特定するために.
- これらのテクタイトの熱史と親物質を理解するために.
主な方法:
- 鉱物の識別のためのX線微分法 (XRD).
- 電子マイクロプローブによる元素組成の化学分析.
主要な成果:
- 高圧のシリカポリモルフであるコエサイトは,インクルージョンで特定されました.
- インクルージョンには,レハテリエライトに囲まれた細かいコエサイトと粗いクォーツの混合物が含まれています.
- コエサイトの存在は,高圧下での形成を示唆しています.
結論:
- テクタイトは,高温から急速に消えた.
- 観測された鉱物組成は,元の原材料の最小限の改変を示しています.
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