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Updated: Apr 30, 2026

Blast Quantification Using Hopkinson Pressure Bars
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余震の密度が距離とともに減少することは,動的ストレスによって引き起こされたことを示している

K R Felzer1, E E Brodsky

  • 1US Geological Survey, 525 S. Wilson, Pasadena, California 91106, USA. kfelzer@gps.caltech.edu

Nature
|June 9, 2006
PubMed
まとめ

地震波によるダイナミックなストレスは,静的なストレスの変化だけでなく,ほとんどの地震を引き起こす可能性があります. この研究は,余震の崩壊を長距離で分析し,波の振幅が誘発の鍵であることを示唆しています. 地震の余震を理解することは極めて重要です.

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