中洋の山脊:不連続,断片,巨大な裂け目
まとめ
中洋のは,新しい海底の形成に影響を与えるセグメントの階層を特徴としています. セグメント長とマントルのプロセスは,長いセグメントと短いセグメントのバランスを保ち,海底の地質を形作ります.
科学分野:
- 地質学 地質学 地質学
- 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)
背景:
- 中洋のは,硬直と非硬直の不連続によって分割されている.
- セグメンテーションパターンは,新しい海底の形成を決定する.
研究 の 目的:
- 中洋ののセグメンテーションの階層を説明するために.
- セグメントの長さと持続性を制御する要因を理解する.
主な方法:
- 中洋の山脊の地質学的観測.
- セグメンテーションパターンの分析とプレート構造との関係.
主要な成果:
- 大型および長寿命から小型および短命まで,セグメントサイズの階層が存在します.
- セグメントの長さは,クラックの伝播力を影響し,より長いセグメントを好む.
- 部分的な溶解と拡散方向の変化により,新しい短いセグメントが生成されます.
結論:
- リッジセグメンテーションは,セグメントの長さのバランスをとるダイナミックなプロセスです.
- セグメントの長さとマントルのダイナミクスは,海底の形成パターンの鍵です.
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