3つの粗粒子の月面サンプルから採取したピロクセンの構成区画とその重要性
まとめ
月面のピロキセンは,色の変化に関連した重要な組成の変動を示します. これらのカルシウムに富んだ鉱物は,陸上のピロキセンとは異なり,フェロシルライトの濃縮に向けたユニークな差別化傾向を示しています.
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.
- 月科学 月科学 月科学
背景:
- 月面のサンプルは,カルシウムに富んだピロクセンを含んでいる.
- これらのピロキセンは複雑な組成区画を示します.
研究 の 目的:
- 月面のピロキセンの組成の変動を分析する.
- これらの鉱物の成長と分化傾向を理解するために.
主な方法:
- 月面サンプル (10047,10058,10062) の分析について.
- ピロキセンの結晶構造と組成物の試験.
- 構成データと光学特性の相関.
主要な成果:
- ピロキセンで観察された顕著なセクターおよび放射線組成の変動.
- 変異は,色や光学特性の変化と相関する.
- 証拠によると,Alは四面体で,Tiは四面体である.
- フェロリゾライトの濃縮に向けたユニークな差別化傾向が特定されました.
結論:
- 月面のピロキセンは,類似の組成の融解から生じる.
- 差異化傾向は,陸上のピロクセンと異なる.
- 鉄に富んだ部分では,トリクリニック型ピロキセノイド構造を呈することがあります.
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