まとめ
深海の地震調査は,海洋地殻の下には,これまで隠されていた7.3km/sの速度層があることを示しています. この発見は,マーシャル諸島とハワイ諸島の間に行われたもので,世界的に広く知られるかもしれない.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 海洋学 海洋学とは
- 地震学 地震学とは
背景:
- 海洋の地殻と上層マントルの地震構造は,プレート構造を理解するための鍵です.
- 以前の屈折の研究では,海洋の地殻内の異なる層を特定しました.
研究 の 目的:
- 深海底の地震速度の構造を調査するために.
- 海洋の地殻とマントルの間の潜在的な地震層を特定し,特徴づけること.
主な方法:
- マーシャル諸島とハワイ諸島の間に深海屈折測定が行われました.
- 連続空気砲の地震屈折データを活用して,微妙な速度層を明らかにした.
主要な成果:
- 7.3 km/sの速度を持つ明確な地震層が特定されました.
- この層は,海洋の地殻 (6.8 km/s) とマントルの間に位置しています.
- この層は以前,二次地震の到着としてマスクされていました.
結論:
- 以前は認識されていなかった地震層が,海底の海殻の下,深海に存在しています.
- この層は,広範囲に広がる深海の盆地で共通する特徴かもしれません.
- この層の構成と範囲を決定するためにさらなる研究が必要である.
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