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Updated: May 4, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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中洋の山脊における断層の形態

W Roger Buck1, Luc L Lavier, Alexei N B Poliakov

  • 1Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA. buck@ldeo.columbia.edu

Nature
|April 9, 2005
PubMed
まとめ

海洋地殻の断層は,最も一般的な構造的特徴であり,プレート拡散センターで形成されます. 2つの異なるメカニズム,プレート不屈とプレート伸縮の2つの異なるメカニズムは,マグマティックダイクの侵入によって,それらの多様なサイズと方向性を説明します.

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