プレート下部の部分的な融解の地震的証拠
Eric Debayle1, Thomas Bodin2, Stéphanie Durand2
1Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, Villeurbanne, France. Eric.Debayle@ens-lyon.fr.
Nature
|October 22, 2020
まとめ
部分的な融解は上層マントルの地震低速度地帯 (LVZ) に存在し,アステノスフィアに供給されます. 0.30%未満の融解は プレート移動と結晶の並び方を 促進します
科学分野:
- 地理学
- マントルダイナミクス
- 地震学
背景:
- 頂上マントルの地震低速帯 (LVZ) はプレート構造に不可欠ですが,その起源は議論されています.
- 現存する理論では,部分的な溶解,固体機構,または低地震速度の原因として揮発性成分が提案されています.
研究 の 目的:
- シーア・アテンチュエーションと速度モデルを用いて,低速度ゾーン (LVZ) の起源を調査する.
- LVZ内の部分溶融の存在と分布を決定する.
主な方法:
- グローバル3次元シーア減弱モデルの解釈
- グローバル3次元地震速度モデルの解釈
主要な成果:
- 海洋 LVZ の内部の部分的な溶解の証拠は,中海の山脊,ホットスポット,バック・アーチ地域の下の 150 - 200 km までです.
- 溶融の0.30%未満が海洋のLVZに閉じ込められ,溶融は大陸の下ではほとんど存在しない.
- 溶融の濃度はプレート速度で増加し,特に3〜5cm/年です.
結論:
- 部分的な融解は,海洋上のマントルLVZの重要な構成要素です.
- 溶けるとアステノスフィアの粘度が低下し,板の動きや大規模なマントルの結晶の整列が容易になる.
- 発見は,マントルからの構造板の分離における 融解の役割を裏付ける.
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