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

<div>Two examples of landslide relocation results during the 2012 Typhoon Saola (a) and the 2015 Typhoon Soudelor (b). The maps show the optimal locations determined by the back projection method. The 1~3 Hz RMS envelopes of broadband and short-period recordings used in the back projection are displayed on the right of each map.</div>

Geofluids

fig7

Figure 7

Figure 7: Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection 