アフリカのホットスポット火山活動:クラトン下の上層マントルの小規模なコンベクション
1Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47907-1397, USA. sking@purdue.edu
まとめ
上層マントルの小規模なコンベクションは,アフリカと南米の下のプラーク内火山活動と地震異常を説明します. エッジ駆動コンベクションは,これらの地質的特徴を理解するために,マントルの羽根の代替案を提供します.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- ジオダイナミクスは地力学です.
- マントラコンベクション マントラコンベクション
背景:
- アフリカと南米の内部火山活動と地震異常は地質学的なパズルを提示しています.
- マントルの羽根が主要な仮説であったが,代替説明が求められている.
研究 の 目的:
- 上層マントルの小規模なコンベクションの役割を調査する.
- クラトーン層と海洋層の石層の下にあるプラーク内火山の起源と地震の特徴を説明する.
主な方法:
- マントルのコンベクションの数値モデリング.
- 厚いクラトンプレートと薄い海洋プレートとの間の石層の移行の分析.
主要な成果:
- 小規模なコンベクションは,厚いクレートン層と薄い海洋層の石層の境界で発生する.
- モデルは,プラーク内火山の位置と地化学的シグネチャを成功裏に複製しています.
- 高い地震切断波速度 (寒いダウンウェリング) は,モデルの予測と一致しています.
結論:
- 小規模で,エッジ駆動のコンベクションは,マントルの羽根に適した代替手段を提供し,板内火山現象を説明します.
- このコンベクションモデルは,アフリカと南米の石層の下にあるマントルの下流と一致しています.
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