太平洋プレートにおける二重火山ホットスポットの同時出現と原因
T D Jones1, D R Davies1, I H Campbell1
1Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory, Australia.
Nature
|May 4, 2017
まとめ
ハワイのダブルトラックの火山は,マントルの羽根によって引き起こされ,太平洋プレート運動の変化によって説明されます. このモデルは,プレートの傾きとプレートの動きが 異なる地化学的な溶岩型を作り出し,プレート構造の洞察を提供していることを示しています.
科学分野:
- 地理学
- 地化学
- プレート構造
背景:
- マントルの羽根は プレート構造とは無関係な火山活動を引き起こします
- ハワイの天皇連鎖は,明確な地化学を備えた,説明できない二重の火山軌跡 (ロアとケア) を表しています.
研究 の 目的:
- ハワイの2つの火山の軌跡の起源を説明するために
- 二重の火山軌跡の出現と太平洋プレートの動きを 結びつけるためだ
主な方法:
- ハワイのダブルトラックの火山の3部モデルを開発した.
- マントルの流れ,羽根の傾き,プレート運動のダイナミクスを分析した.
- 融解源地域に関連した地化学的差異を調査した.
主要な成果:
- パシフィックプレート運動の変化は ハワイの羽根を傾け 溶融の源を分離します
- プレートの動きが変化すると 異なる溶融物質が露呈し 太平洋を横断する 二重線路が形成されます
- 低圧溶融地域における二次性ピロクセニットはロア軌道の地化学を説明する.
結論:
- ハワイのダブルトラックの火山は 暫定的な現象です
- ダブルトラックの形成は,プレート運動の変化を測定するための方法を提供します.
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