Fig. 4From: Numerical simulations to explain the coseismic electromagnetic signals: a case study for a M5.4 aftershock of the 2016 Kumamoto earthquakeSeismic and EM signals simulated for the water-saturated half-space porous model. Multiple components of a seismic and EM wave-fields and b localized and evanescent EM waves are calculated for a receiver nearby the ground surface, which is located at (− 80,890, 8680, 0.1) mBack to article page