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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
地中海地域のプレート構造
1Department of Geodesy and Geophysics, University of Cambridge, Madingley Rise, Cambridge.
Nature
|April 18, 1970
まとめ
地中海東部の2つの小さな,急速に移動するプレート構造は,プレート構造の原理が大陸プレート境界や瞬時の動きに適用されることを示しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- テクトニクス (地質学) とは
- 地震学 地震学とは
背景:
- 東地中海は複雑な地震性を示しています.
- プレート運動を理解することは,地質学の研究にとって極めて重要です.
研究 の 目的:
- 地中海の地震性と断層平面の解決策を分析する.
- 小規模で,急速に移動するプレート構造の存在と影響を調査する.
主な方法:
- 地震データ分析による地震データ分析
- 断層平面の解決策の決定
- プレートモーションモデリング
主要な成果:
- 東地中海で2つの小さな,急速に移動する構造板を特定しました.
- これらのプレートは,収縮する海洋盆地の特徴かもしれません.
- プレートテクトニクスの大陸の境界を越えた瞬間の動きへの適用性を確認しました.
結論:
- 小さく,速く動くプレートの存在は,プレート構造学にとって重要な発見です.
- プレートテクトニクスの概念は,大陸プレート境界の動きに対して検証されています.
- 海洋盆地における同様のプレート構成に関するさらなる研究が必要である.
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