月面のクリノピロキセン:化学組成,構造状態,質感
まとめ
アポロ11号のクリノピロキセンは,アウジットとピジョンイットの複雑な交差を明らかにした. これらの月のピロキセンは,一次化学的変異と溶解のラメラを示し,単一の一次ピロキセンの相を示唆しています.
科学分野:
- 地質学 地質学 地質学
- ミネラロジーは,鉱物学です.
- 惑星科学は惑星科学である.
背景:
- クリノピロキセンは,火性の過程を理解するための重要な鉱物です.
- アポロ11号のサンプルは,月のマグマの進化についての洞察を提供します.
研究 の 目的:
- アポロ11号の月面サンプルから採取したクリノピロキセンの鉱物学と化学を特徴づけるため.
- 月面環境におけるピロキセンの形成と進化を調査する.
主な方法:
- シングルクリスタルX線 difrractionによるX線です.
- マイクロソーブ分析による分析
- 光学顕微鏡による光学顕微鏡です.
- 電子顕微鏡 (伝送電子顕微鏡を含む)
主要な成果:
- 月面のクリノピロキセンは,主にオーギット・ピジョニット・インターグロウストである.
- 60 Å の薄さの豊富な溶解のラメラが観察されました.
- 主要な化学的不均一性が特定され,Ca,Fe,Ti,Al,Siを含む相互関係があった.
結論:
- 化学的に不均質な亜カルシウムアギトが,おそらく最初のピロキセンの相であった.
- この原始アウジートから溶解したピジョンライトは,複雑な熱的または化学的な歴史を示しています.
関連する概念動画
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