イントラスラブ地震:カスカディアスラブの脱水
Leiph A Preston1, Kenneth C Creager, Robert S Crosson
1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA. preston@ess.washington.edu
まとめ
研究者らは,ワシントンにあるフアン・デ・フカ・プレートの3D地震構造をマッピングした. これは,2つの異なる地震の起源を明らかにします:マントルのサーペンチナイト脱水と地殻のベースアルトからエクロジットへの変換.
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
- テクトニクス (地質学) とは
背景:
- フアン・デ・フーカ板は北米の底に沈み込み,複雑な地震活動を発生させる.
- 潜水板の構造を理解することは,地震のメカニズムを解読する鍵です.
研究 の 目的:
- フアン・デ・フカプレートの3次元圧縮波速度構造と反射器幾何学を決定する.
- カスカディア潜流地帯のイントラスラブ地震の起源を調査する.
主な方法:
- 折れと広角反射の地震波の移動時間の同時逆転.
- 3D地震速度のモデリングと地震移転.
主要な成果:
- フアン・デ・フカプレートの地殻マントル境界 (Moho) を特定した.
- モホーに相対する位置に基づいて,2つの異なるグループに分離されたイントラスラブ地震.
- 45kmのモホの深さの上下地震は,沈下した海洋マントルで発生し,下下地震は沈下した地殻で発生します.
結論:
- イントラスラブ上下地震は,サーペンチナイトの脱水と関連しています.
- ダウンディップのイントラスラブ地震は,玄武岩からエコロギットへの変換に起因する.
- カスカディアの潜水地帯での地震発生を理解するための新しい枠組みを提供します.
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