海洋プレートの鋭いリトスフィア-アステノスフィア境界の地震的証拠
Hitoshi Kawakatsu1, Prakash Kumar, Yasuko Takei
1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan. hitosi@eri.u-tokyo.ac.jp
まとめ
プレート構造は,石層圏がアステノスフィア上を移動することを前提としています. リトスフィア-アステノスフィアの境界 (LAB) を理解すると,板の動きを促進する溶融に富んだ層を持つ鋭い,年齢に依存する構造が明らかになります.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- テクトニクス (地質学) とは
- 地震学 地震学とは
背景:
- プレートテクトニクスは,アステノスフィアの上の石層運動を記述する.
- リトスフィア-アステノスフィアの境界線 (LAB) は,地球の動態を理解するために極めて重要です.
- 海洋プレートは,LABを研究するためのよりシンプルなモデルを提供します.
研究 の 目的:
- 海洋プレートの下のLABの特徴を調査する.
- アステノスフィアの物理的状態とプレート構造におけるその役割を理解する.
主な方法:
- 掘削穴のブロードバンドの海底地震計からの地震データの分析.
- シェア波の速度減少の解釈.
主要な成果:
- 太平洋プレートとフィリピン海プレートの下のLABは,鋭く,年齢に依存しています.
- LABでシール波の速度の有意な減少が観察されました.
- 証拠は,部分的に溶けたアステノスフィアと,水平の溶融に富んだ層があることを示唆しています.
結論:
- アステノスフィアは,溶融に富んだ層を含み,LABで大きな粘度コントラストを生み出します.
- この粘度コントラストは,板構造の重要な側面である水平板の動きを容易にします.
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