アノートソサイトの熱い,深く沈んだ隕石による変化の際に,短命の酸素拡散
1Department of Geological Sciences, University of Tennessee, Knoxville, TN 37996-1410, USA. Chemical and Analytical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831-6365, USA.
まとめ
メタイグニオスの岩石のプラジオクラゼは,極度の酸素-18の枯渇を示し,高温で流星流体との相互作用を示しています. これは,アノースサイト内の急速な液体交換と拡散を示唆しています.
科学分野:
- 地質化学 地質化学
- 同位体地質学とは,同位体地質学である.
- メタモルフ Petrology メタモルフペトロロジー
背景:
- メタイニオスの岩のプラジオクラスは,流体岩相互作用の記録を保存することができます.
- 酸素同位体組成は,地質学的過程についての洞察を提供します.
研究 の 目的:
- ボールズ・ブッテ・アノルトサイトからのプラジオクラゼの酸素同位体組成を調べる.
- アノースサイト内の流体相互作用の性質とタイミングを決定する.
主な方法:
- プラジオクラゼの酸素同位体分析.
- プラジオクラゼ結晶の微細構造分析.
- 同位体交換の地球化学モデリング.
主要な成果:
- プラジオクラゼは,酸素-18値が非常に枯渇している (-16/mlまで).
- 隕石流体との高温 (500°C以上) の同位体交換の証拠.
- 反応により高まった透性により,流体の流入が容易になりました.
- 鋭い同位体グラデーションは,短命 (~10 ^ 4年) の拡散交換と高い水:岩比を示しています.
結論:
- 流星流体により,高温でアノルトサイトが大幅に変化した.
- 急速な液体交換と,その後の拡散の停止が起こった.
- ボールズ・ブッテ・アノルソサイトは,古代の隕石・熱水系へのユニークな窓を提供します.
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