薄い地殻は,マリオン・ライズを支えるマントルの枯渇の証拠である
Huaiyang Zhou1, Henry J B Dick
1State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China. zhouhy@tongji.edu.cn
Nature
|February 8, 2013
まとめ
マリオン・ライズは,他の海上のライズとは異なり,薄いか欠落した地殻が特徴で,それを示す.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 海洋地質学 海洋地質学
- プレート・テクトニクス (プレート・テクトニクス)
背景:
- 海洋の上昇は,軸深さの変動によって特徴付けられ,しばしばマントルのホットスポットと関連付けられています.
- アイスランド・ライズに匹敵するマリオン・ライズは,その長さのほとんどに沿ってユニークな軸裂け目を呈しています.
- 南西インド・リッジは,体系的なサンプリングにより,地殻の建築を研究するためのユニークな機会を提供します.
研究 の 目的:
- 南西インディアン・リッジ沿いのマリオン・ライズの地殻構造を調査する.
- マリオン・ライスの形成と特徴に起因する地質学的プロセスを理解する.
主な方法:
- 南西インド山脊の全長に沿って,地質学的サンプルを体系的に採取する.
- 地殻の露出と組成の分析.
- 脊柱システムの地球物理学的解釈.
主要な成果:
- マリオン・ライズで,アイスランド・ライズと対照的にペリドータイトの大幅な露出.
- マリオン・ライズ (Marion Rise) の裂け目を越えて,一般的に薄いか欠けている地殻の証拠がある.
- マリオン上昇は主にイソスタティック反応であり,厚くなった地殻や大きな熱異常によるものではありません.
結論:
- マリオン・ライズの構造は,底辺の枯渇したマントルの同静的調整を示唆しています.
- この枯渇したマントルは,カルーとマダガスカルの洪水ベースルトイベントの間に置かれたマントルから起源がある可能性が高い.
- この研究は,海洋上昇の形成とマントルプロセスとの関係に関する新しい洞察を提供します.
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