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Rupture complexity of a moderate intraplate earthquake in the Alps: the 1996M5 Epagny–Annecy earthquake

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Figure 1. Focal mechanism of the 1996 July 15 Epagny–Annecy event5Broad-band network operated by the UMR Ge´osciences Azur.
Figure 2. Examples of displacement and velocity waveforms of the at each station that provided unclipped records
Figure 3. Deconvolution results with: (a) the M
Figure 4. Examples of two pulse-width measurements on clipped seismograms.
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