関連する実験動画
Updated: Jul 12, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
月面からの粗い粒子物質の鉱物学と地質学は,静寂基地の静寂基地にあります
まとめ
アポロ11号の粗い細工には,衝撃で生成されたガラスとマフィの火山岩が含まれています. これらの岩の断片は,アポロ11号のより大きなサンプルと異なる多様な質感を示しています.
科学分野:
- 月面地質学 月面地質学
- ペトロロジー・ペトロロジーとは
- ショックメタモルフィズム
背景:
- アポロ11号ミッションは,粗い罰金を含む月面サンプルを返還しました.
- 月面のレゴリット組成を理解することは,月面科学にとって極めて重要です.
研究 の 目的:
- アポロ11号の穀物の組成と起源を特徴づける 粗い細い (10085,11).
- 粗細な岩石のペトログラフィを,より大きなアポロ11号の結晶岩石サンプルと比較してみましょう.
主な方法:
- 5グラムの粗細な繊維から1227個の粒子を採取したペトログラフィック分析.
- 岩石の断片とガラスのモダル分析と質感検査.
主要な成果:
- 粗細な細部は,マフィのホロクリスタリン岩の断片,マイクロブレッチア,衝撃で生成されたガラスが支配しています.
- 結晶の断片は,多種多様な質感を持つガブロイド岩石を表しています.
- 豊富なガラスは主にショックイベントの結果であり,テクトイトガラスは観察されなかった.
結論:
- 粗い細い部分は,月面の岩石の多様性のより広い範囲に洞察を与えます.
- 衝撃の変形は,これらの月の細部の組成と質感に大きな影響を与えました.
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