まとめ
月岩15415.9の結晶化年齢は409億年であり,月の地殻は早期に形成されたことを示唆しています. これは,早期の小分結晶化による融けた月面の理論を支持する.
科学分野:
- 月面地質学 月面地質学
- 宇宙化学 (コスモケミストリー)
- 惑星科学は惑星科学である.
背景:
- 月の原始的な地殻の形成は,太陽系の初期の歴史における重要な出来事である.
- 月の地殻の形成を理解することは,惑星の進化の洞察を提供します.
研究 の 目的:
- アポロ15号アノルソサイトサンプル (15415,9) の結晶化年齢を決定する.
- 月の原始的な地殻形成のタイミングを評価するために.
- 早期の融けた月面と,その後の小分結晶化に関する仮説を検証する.
主な方法:
- アポロ15号のアノソサイト岩 (15415.9) の放射測年代測定法による年代測定.
主要な成果:
- サンプル15415.9の結晶年齢は (4.09 ± 0.19) × 10 ^ 9年と決定されました.
- この年齢は,原始的な月の地殻は,おそらく月の歴史の最初の3億から4億年の間に形成されたことを示しています.
結論:
- この発見は,初期の月面が溶融だったという仮説を裏付けている.
- この結果は,大規模な分量結晶が,月の初期の地質進化において重要な役割を果たしたことを示唆している.
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