湿ったペリドート固体と海洋マントルの潜在温度に関する実験的制約
Emily Sarafian1,2, Glenn A Gaetani2, Erik H Hauri3
1Massachusetts Institute of Technology-Woods Hole Oceanographic Institution Joint Program in Oceanography/Applied Ocean Science and Engineering, Cambridge, MA 02139, USA. etursack@whoi.edu.
まとめ
海上マントルの溶けた水 (H2O) はペリドート固体の温度を著しく上昇させる. この発見は,海洋の広がりの中心の下のマントルの上昇のための潜在的な温度推定値の向上調整を必要とします.
科学分野:
- 地化学
- 地理学
- 鉱物物理学
背景:
- 大洋の地殻は,マグマから形成され,マントルの圧縮解消により,広がりの中心の下から形成される.
- 表面上無水質のマントル鉱物中の溶けた水 (H2O) は,溶解点 (固体) に著しい,しかし実験的に定量化されていない影響を及ぼします.
研究 の 目的:
- 溶けた水素がペリドート固体に与える影響を実験的に決定する.
- マントルの融解状態に対するH2Oの影響を定量化する.
主な方法:
- 制御されたH2O濃度下でのペリドート固体の実験的決定.
- マントルのペリドートに 高温と圧力の実験を行いました
主要な成果:
- H2O不飽和のペリドライト・ソリッドは,実験的に,以前に推定されたよりも高いことが示されています.
- 溶けたH2Oの存在は,ペリドータイトが溶ける温度を大幅に上昇させます.
結論:
- 海洋マントルの融解の既存のモデルは 必要な潜在温度を過小評価しているかもしれません
- 東太平洋上昇の下での地質学的観測は,海洋上のマントルの潜在的な気温推定値の~60°Cの向上調整を示唆しています.
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