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Updated: Apr 30, 2026

Blast Quantification Using Hopkinson Pressure Bars
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余震密度与距离的衰减表明由动态应力触发的触发

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
概括

来自地震波的动态应力可能会触发大多数地震,而不仅仅是静态应力变化. 这项研究分析了余震对距离的衰变,表明波幅是触发震荡的关键. 了解地震余震是非常重要的.

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