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Koji Masuda Source duration of stress and water-pressure induced seismicity derived from experimental analysis of P wave pulse width in granite Geophysical Research Letters 40

Article first published online: 20 JUL 2013 | DOI: 10.1002/grl.50691

Key Points

  • Source duration of water-induced seismicity is shorter than that in a dry state
  • Increased rupture velocity and a more equidimensional source are responsible
  • Corrections were made for event size and hypocentral distance

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