Coupling of Multiple Rayleigh Waves and Water Level Signals during 2011 Great Tohoku Earthquake Observed in Georgia, Caucasus
T Chelidze, I Shengelia, N Zhukova, T Matcharashvili… - 2014 - 109.205.44.60
2014•109.205.44.60
The dynamic triggering due to the great Tohoku M 9 earthquake Japan (2011) was observed
in local seismicity all around the globe. We presume that Tohoku EQ could also trigger local
seismic events in Georgia (Caucasus), which is separated from Japan by 7800 km. It was
discovered during integrated analysis of seismic and water level records in wells that
besides S, L and R waves, multiple surface Rayleigh waves also induce water level
oscillations
in local seismicity all around the globe. We presume that Tohoku EQ could also trigger local
seismic events in Georgia (Caucasus), which is separated from Japan by 7800 km. It was
discovered during integrated analysis of seismic and water level records in wells that
besides S, L and R waves, multiple surface Rayleigh waves also induce water level
oscillations
The dynamic triggering due to the great Tohoku M 9 earthquake Japan (2011) was observed in local seismicity all around the globe. We presume that Tohoku EQ could also trigger local seismic events in Georgia (Caucasus), which is separated from Japan by 7800 km. It was discovered during integrated analysis of seismic and water level records in wells that besides S, L and R waves, multiple surface Rayleigh waves also induce water level oscillations
109.205.44.60
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