地震の余震が動的ストレスによって引き起こされる
1Center for Earthquake Research and Information, The University of Memphis, Tennessee 38152, USA.
Nature
|December 16, 2000
まとめ
暫定的な地震波,またはダイナミックストレスは,断層の性質を変えることで,近くの地震を引き起こす可能性があります. これは,地震誘発パターンの直接的な影響が少ない静的ストレス変化と対照的です.
科学分野:
- 地球科学 地球科学 地球科学
- 地震学 地震学とは
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 地震の誘発は,しばしば断層の移動による静的ストレス変化に起因する.
- 以前の研究は,静的ストレスの変化と,近隣の断層活動への影響に焦点を当てていた.
研究 の 目的:
- 地震の余震パターンの静的および動的ストレス変化の影響を比較する.
- 地震を誘発する地震波の伝播の役割を調査する.
主な方法:
- 7.3マグニチュード (Mw) のランダーズ地震の瞬間後の余震パターンの分析.
- 観測された余震分布と計算された静的および動的ストレス変化の比較.
主要な成果:
- 破裂伝播の影響を受けたダイナミックなストレスパターンは,余震分布に似た非対称性を示した.
- 静的ストレスの変化は,余震パターンと同じ非対称性を表さなかった.
- 動的ストレスが,近い場所と遠い場所の両方で地震を引き起こす可能性があるという証拠があります.
結論:
- 動的ストレスだけでなく,静的なストレスも,地震を誘発する上で重要な役割を果たします.
- この調査結果は,地震の予測と危険性評価において,地震波の影響を考慮することの重要性を強調しています.
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