Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection

<div>The vertical component broadband seismograms of a teleseismic event during the 2015 Typhoon Soudelor period. (a) The 220 s-long waveforms bandpass-filtered between 1 and 3 Hz and (b) the 220 s-long waveforms bandpass-filtered from 0.02 to 0.05 Hz. (c) The extended 1000 s-long waveforms bandpass-filtered from 0.02 to 0.05 Hz, which confirm that these seismograms were generated by a teleseismic event.</div>

Geofluids

fig6

Figure 6

Figure 6: Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection 