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主要なホットスポットの下にある地球のマントルの底部に根付いた広い羽根
Scott W French1, Barbara Romanowicz1,2,3
1Department of Earth and Planetary Science, Berkeley Seismological Laboratory, University of California at Berkeley, California 94720, USA.
Nature
|September 4, 2015
まとめ
ホットスポット火山の潜在的源である 深いマントルの羽根は 薄い熱尾ではなく 広い準垂直管として明らかにされています これらの構造は 深い超低速帯に繋がり マントルの熱化学的起源が 長く存在することを示唆しています
科学分野:
- 地理学
- 地震学
- マントルダイナミクス
背景:
- ホットスポット火山の起源は議論されており,熱の羽根が提案されていますが,検出は困難です.
- 地力学モデルによると 純粋に熱の渦巻は 薄くて 地震に耐えられない
研究 の 目的:
- 先進的な地震技術を使用してホットスポットの下の深いマントルの構造をイメージします.
- マントルの羽根の物理的特徴と起源を調査する
主な方法:
- 精密な波場計算と完全な地震波形分析を組み合わせた全マントルの地震画像技術を使用しました.
- この方法を使って 突出のホットスポットの下にある 広い準垂直管を明らかにした
主要な成果:
- 核-マントルの境界から ~1,000 kmの深さまで広がる広い (薄くない) 導管を特定した.
- ハワイ,アイスランド,サモアなど, 接続を確立しました.
- 導管は熱噴出モデルよりも広く,熱化学的起源と鈍い深層マントルの循環を示唆しています.
結論:
- マントルの羽根は幅広く,長生きで,純粋に熱的ではなく,熱化学的かもしれません.
- 超低速圏とマントルの間を 直接接続した
- 発見は,マントルの粘度層と熱化学的コンベクション研究に制約を与える.
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