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ハワイの羽根による石層の若返り
Xueqing Li1, Rainer Kind, Xiaohui Yuan
1GeoForschungsZentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany.
Nature
|February 27, 2004
まとめ
ハワイ諸島 ハワイ諸島とは
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- プレート・テクトニクス (プレート・テクトニクス)
背景:
- ハワイの火山活動は,固定されたマントルの羽根の上での海洋石層の移動と関連しています.
- 既存の地震画像には,羽根-石灰圏相互作用モデルを区別するための解像度が欠けている.
研究 の 目的:
- 地震受信機能を使用して,ハワイ諸島の下の石層厚度をマッピングする.
- 羽根-石灰圏の相互作用とその影響が島鎖形成に及ぼす影響を調査する.
主な方法:
- S波受信機機能技術の応用.
- ハワイ諸島の3つの恒常的なブロードバンドステーションからの地震データ分析.
主要な成果:
- リトスフィアの厚さはビッグアイランドの下100~110kmで,未修正の古い海洋プレートと一致する.
- リトスフィアは,300kmの幅でカワイ島の下から50~60kmまで徐々に薄くなります.
- 証拠は,若返りモデルが薄くなるゾーン内で活性化していることを示唆しています.
結論:
- マントルの羽根は,ハワイの島連鎖に沿った石層を活発に薄くします.
- より広範な地形的な膨張は,単に石層の薄めではなく,ダイナミックな力によって支えられている可能性が高い.
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