地震の際の故障潤滑
1Dipartimento di Geoscienze, Università di Padova, Padova 35131, Italy. giulio.ditoro@unipd.it
Nature
|March 25, 2011
まとめ
岩石の摩擦は,地震の滑り際に著しく減少し,この現象は断層潤滑と呼ばれています. 物理化学的プロセスによって引き起こされるこの潤滑は,様々な種類の岩石で発生し,地震のメカニズムを理解するために不可欠です.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震の力学 地震の力学
- ロック物理学 ロック物理学
背景:
- 断層摩擦は地震力学において極めて重要であり,ストレス低下とエネルギー放出に影響を与えます.
- 断層摩擦の判定のための地震学的方法は,挑戦的で,実験的アプローチが必要である.
研究 の 目的:
- 地震滑り率における岩石摩擦に関する実験データをレビューする.
- 地震時の断層潤滑のメカニズムと範囲を解明する.
主な方法:
- およそ300の出版・未出版の実験を分析した.
- 地震滑り率 (0.1-2.6 m/s) をシミュレートするために回転切断装置を使用しました.
主要な成果:
- 地震の滑り率で岩石の摩擦が著しく減少した (最大1桁) ことが観察されました.
- 断層潤滑の原動力として特定された物理化学的プロセス (例えば,凝縮,脱水,融解)
- 実験結果は,自然欠陥産物と地震学的推定値と一致しています.
結論:
- 断層は,岩の組成や弱体化メカニズムに関係なく,地震中に潤滑を経験する可能性が高い.
- 実験的発見は,7~15 kmの深さでの地震核形成を理解するために重要である.
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