ソフト堆積物における断層外損傷が地表付近の断層破壊挙動を制御する
Nicola De Paola1, Rachael J Bullock2, Robert E Holdsworth2
1Department of Earth Sciences, Durham University, Durham, UK. nicola.de-paola@durham.ac.uk.
Nature communications
|December 13, 2025
まとめ
断層外エネルギー散逸は、浅部地震断層の破壊を著しく遅くするか、停止させる。この研究により、地表付近の損傷が全破壊エネルギーの最大85%を占め、破壊速度の遅さを説明することが明らかになった。
科学分野:
- 地球物理学
- 地震科学
- 断層力学
背景:
- 地表破壊断層は、地震による重大な危険をもたらします。
- 断層周辺の地表付近の破壊挙動とエネルギー散逸は、ほとんど理解されていません。
- 断層破壊先端周辺の断層外エネルギー散逸に関するデータは限られています。
結論:
- 断層外の損傷は、地表付近の地震断層破壊ダイナミクスを制御する上で重要な要素です。
- 地震ハザードの評価には、断層外エネルギー散逸の理解が不可欠です。
- この発見は、浅部地震イベントで観察される現象の説明に貢献します。
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