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Rapid determination of the magnitude and tsunami potential of large earthquakes, and implications for source physics.M wpd and high-frequency, apparent rupture duration T.Tsunamigenic earthquakes T s.P-wave dominant period calculation T d.Tsunamigenic earthquakes the T d ∙T discriminant.Importance of identifying length and depth of faulting Anthony Lomax ALomax Scientific, Mouans-Sartoux, France Alberto Michelini Istituto Nazionale di Geofisica e Vulcanologia Roma, Italy M wpd and high-frequency, apparent rupture duration T M wpd processing steps min September , M.Sumatra T Lomax Michelini A ,n velocity seismogram oitaru n D o it er a.Hz, HF seismogram r ut u p D T u R F T estimate HF envelope Hedu ground-displacement ti M wp lp M wpd M estimate integral of m OT - min displacement over duration T A Duration-amplitude magnitude M wpd CMT Raw M compared to M for wpd w recent, large earthquakes.interplateM.CMT M w Duration-am
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