Institut de Physique du Globe de Strasbourg - IPGS - UMR7516

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              First observation of 2S1 and study of the splitting of the football mode               0S2 after the June 2001 Peru earthquake of magnitude 8.4
              Impulsive Source of the 2017, Mw=7.3 Ezgeleh, Iran, Earthquake
              Localized fault slip to the trench in the 2010 Maule, Chile                              = 8.8 earthquake from joint inversion of high-rate GPS, teleseismic body waves, InSAR, campaign GPS, and tsunami observations
              Rupture characteristics of major and great (                                ≥ 7.0) megathrust earthquakes from 1990 to 2015: 1. Source parameter scaling relationships
              Rupture characteristics of major and great (                               ≥ 7.0) megathrust earthquakes from 1990 to 2015: 2. Depth dependence
              Rupture process of the 2010                              7.8 Mentawai tsunami earthquake from joint inversion of near-field hr-GPS and teleseismic body wave recordings constrained by tsunami observations
               Supershear rupture of the 5 January 2013 Craig, Alaska (                              7.5) earthquake
  S‐velocity model and inferred Moho topography beneath the Antarctic Plate from Rayleigh waves
              The 5 September 2012 Nicoya, Costa Rica                              7.6 earthquake rupture process from joint inversion of high-rate GPS, strong-motion, and teleseismic                              wave data and its relationship to adja
              The ZH ratio method for long-period seismic data: inversion for                          S-wave velocity structure
               Validation of linearity assumptions for using tsunami waveforms in joint inversion of kinematic rupture models: Application to the 2010 Mentawai                              7.8 tsunami earthquake
The 1996 Cyprus earthquake: a large, deep event in the Cyprean Arc
The 2006-2007 Kuril Islands great earthquake sequence
The 2007 caldera collapse of Piton de la Fournaise volcano: Source process from very-long-period seismic signals

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