ハワイの下のマントルに余分な鉄があるという地化学的証拠
Munir Humayun1, Liping Qin, Marc D Norman
1Department of the Geophysical Sciences, 5734 South Ellis Avenue, Chicago, IL 60637, USA. humayun@magnet.fsu.edu
まとめ
地球 地球 地球 地球 地球 地球
科学分野:
- 地化学,地物理学,ペトロロジー
背景:
- 地球の核とマントルの間の化学相互作用は,マントルの構成に影響を与えます.
- ハワイの溶岩のオスミウム同位体比は,コアからマントルへの物質の流れを示唆しています.
研究 の 目的:
- ハワイの下のマントルの鉄含有量を調べるために.
- 鉄の濃縮を密度異常とオスミウム同位体シグネチャーと相関させるため.
主な方法:
- ハワイの溶岩における鉄とマンガン (Fe/Mn) の比率の正確な測定.
- オスミウムの同位体比の分析.
- 地震トモグラフィーデータとの比較.
主要な成果:
- ハワイの溶岩は,マントルの鉄モール分数の1~2%の増加を示しています.
- この鉄濃縮は ~0.5%の密度異常に対応しています.
- マンガンが豊富な堆積物は,Os同位体信号の源として除外されています.
結論:
- 証拠は,液体外核とマントルの間の化学相互作用を裏付けている.
- ハワイの下のマントルは,コア材料の添加と一致する鉄で濃縮されています.
- この研究は,地球深層の組成の異質性に関する私たちの理解を洗練します.
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