地球のマントルの真ん中の粘度ジャンプ
Maxwell L Rudolph1, Vedran Lekić2, Carolina Lithgow-Bertelloni3
1Department of Geology, Portland State University, Post Office Box 751, Portland, OR 97207, USA. maxwell.rudolph@pdx.edu.
まとめ
科学者は800~1200kmの深さの 深いマントルの粘度が 大きく増加していることを発見しました この発見は 停滞した地形板や マントルの渦巻のような現象を 説明するのに役立ちます
科学分野:
- 地理学
- 地球科学
- マントルダイナミクス
背景:
- 深いマントルの粘度が地球の熱進化,羽根の動態,物質の混合に影響する.
- マントルの層構造を理解することは,大規模な地質学的プロセスを理解するために不可欠です.
研究 の 目的:
- 地球の深層マントルの粘性層を 推測する事になる
- 粘度変化と観測された深層マントルの構造との関係を調査する.
主な方法:
- 長波長非水静的ジオイドデータの再分析
- 深さによる粘度変化を測定するための新しい方法を使用します.
主要な成果:
- マントルの粘度が800~1200kmの深さで 大きく増加した.
- この粘度上昇は,マントルの移行領域以下で起こります.
- 粘度上昇の深さは,スラブの停滞と羽根の傾斜の地震観測と相関しています.
結論:
- 推測された粘度増加は,観測された深層マントルの現象に統一的な説明を提供します.
- この発見は,マントルの粘度層に関する以前の仮定に異議を唱える.
- 深いマントルの動態における粘度構造の重要性を強調する.
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