Re-Osは,地球の上層マントルの長寿の異質性と均衡プロセスに関する同位体証拠である
Anders Meibom1, Norman H Sleep, C Page Chamberlain
1Geological and Environmental Sciences, 320 Lomita Mall, Stanford University, California 94305, USA. meibom@pangea.stanford.edu
Nature
|October 18, 2002
まとめ
地球の上層マントルは,数十億年にわたる溶融の抽出と地殻のリサイクルにより,非常に異質的です. レーニウム-オスミウム (Re-Os) 同位体データは,
科学分野:
- 地質化学 地質化学
- イソトープ地球化学 イソトープ地球化学
- ペトロロジー・ペトロロジーとは
背景:
- 地球の上層マントルの構成は,数十億年の地質学的過程を反映しています.
- レーニウム・オスミウム (Re-Os) 同位体系は,溶融抽出と地殻リサイクルに敏感である.
研究 の 目的:
- 上層マントルの地化学的異質性を調査する.
- Re-Osイソトープを使用して,溶融の微量抽出と地殻物質のリサイクル.
主な方法:
- 700以上のオスミウムに富んだプラチナ系元素合金によるオスミウムイソトープ組成を分析した.
- マントルの進化を評価するためにRe-Osイソトープ体系論を利用した.
主要な成果:
- オスミウムイソトープのデータは,上層マントルの極端な異質性を示す広範なガウス分布を示しています.
- 枯渇し,豊かになったマントルの領域は,何十億年も不均衡に留まることがある.
結論:
- 中洋の山脊のような高度の部分融解は,効率的なRe-Os均衡のために必要である.
- ガウスのオスミウムイソトープ分布は,離散的な溶融枯渇事件ではなく",プラムプディング"マントルの混合プロセスを示唆しています.
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