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Updated: Jul 13, 2026

07:55
Flexural Rigidity Measurements of Biopolymers Using Gliding Assays
Published on: November 9, 2012
スリップパーティションは,深さで斜滑りの弾性プラスチックの伝播によるスリップパーティションです
David Bowman1, Geoffrey King, Paul Tapponnier
1Department of Geological Sciences, California State University, Fullerton, 800 State College Boulevard, Fullerton, CA 92834-6850, USA. dbowman@fullerton.edu
まとめ
tektonic 境界線に沿ってスライド分割は,斜滑りの上向きの伝播によって説明され,明確な断層ゾーンを作成します. このモデルは,主要な故障システムで観察される故障の種類を正確に予測します.
科学分野:
- 構造地質学 構造地質学
- テキトノフィジックスの物理学です.
- 地震の力学 地震の力学
背景:
- tektonic 境界の斜面運動はしばしば,滑り感覚が異なる断層に分割されます.
- スリップパーティションの起源を理解することは,構造地質学,地質物理学,地震力学において極めて重要です.
研究 の 目的:
- tektonic 境界に沿ってスライド分割の現象を説明するために.
- 断層形成におけるエラストプラスチックの伝播の役割を調査する.
主な方法:
- より深い断層または切断地帯から斜滑りによる上向きの弾性プラスチックの伝播をモデリングする.
- 拡散する断層の先にある結果の張力場を分析する.
主要な成果:
- 断層の先にある張力場は,正規,逆転,ストライクスリップ断層の異なるゾーンに分割されます.
- このモデルは,故障タイプの観察された分布をうまく予測します.
結論:
- スリップ・パーティションは,斜滑りの弾性プラスチックの伝播によって説明できます.
- このモデルは,テクトニックの境界における断層の振る舞いを理解するための実行可能なメカニズムを提供し,フィールド観測によって検証されています.
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