まとめ
この研究は,ミッド・アトランティック・リッジの西にある840キロメートルの断層地帯を追跡した. 曲線の変化は,地殻板が複数の極の周りを回転していることを示唆している.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- プレート・テクトニクス (プレート・テクトニクス)
- 海洋地質学 海洋地質学
背景:
- 断層地帯は,海洋地殻の重要な特徴である.
- その幾何学を理解することで,プレート構造の過程についての洞察が得られます.
研究 の 目的:
- ミッド・アトランティック・リッジの西にある特定の断層地帯の幾何学と起源を調査する.
- 断裂ゾーンの進化が複数の回転極を伴うかどうかを判断する.
主な方法:
- 断層地帯の範囲を追跡するための地質学的調査.
- 断裂地帯の曲線を分析して,構造回転を推論する.
主要な成果:
- 断裂地帯は,西に向かって840kmの長さで追跡された.
- 曲折半径の顕著な変化は,47度45'W.で特定されました.
結論:
- 曲線の観測された変化は,回転の極のシフトを示しています.
- 断裂ゾーンは,地殻板の回転の少なくとも2つの連続したエピソードのために形成された可能性があります.
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