まとめ
東太平洋上昇層の地殻は,表面の近くでP波の衰弱が高く,軸に近づくにつれて減少しています. より深い高衰弱は,軸性地殻内の部分的な溶融の小さな部分を示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- 海洋地質学 海洋地質学
背景:
- 中洋の山脊の軸の地殻は,マグマの過程を理解するために重要である.
- 地震波の衰弱は,温度や融解量などの地殻の特性についての洞察を提供します.
研究 の 目的:
- 東太平洋上昇軸の地殻の二次元P波減衰構造を決定する.
- 観測された衰弱変数の原因を調査する.
主な方法:
- アクティブソースの地震トモグラフィー実験.
- 波形スペクトルの逆転により,P波の衰弱構造を導き出す.
主要な成果:
- 高P波減衰は,軸の地殻の表面全体で観察されます.
- 衰弱は上昇軸から1〜3km以内で著しく低下し,ベースアルト層の厚み化と水熱変化に起因する.
- 2kmの深さから地殻の底まで上昇軸の下では高い衰弱が持続し,小さな部分的な溶融分子が示されています.
結論:
- 浅瀬の衰弱の変動は,地表地質学的プロセスと関連しています.
- 深い衰弱は,東太平洋上昇軸の下の地殻内の少量の部分溶融の存在を示唆しています.
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