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Roberto Benavente and Phil R. Cummins Simple and reliable finite fault solutions for large earthquakes using the W-phase: The Maule (Mw = 8.8) and Tohoku (Mw = 9.0) earthquakes Geophysical Research Letters 40

Version of Record online: 22 JUL 2013 | DOI: 10.1002/grl.50648

Key Points

  • We use W-phase waveforms to infer the slip distribution of large earthquakes
  • Our results for two megathrusts are a good first-order source characterization
  • Rapid finite slip inversions might be carried out relying in W-phase waveforms

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