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Earth, Planets and Space
Fig. 6 | Earth, Planets and Space

Fig. 6

From: Numerical simulations to explain the coseismic electromagnetic signals: a case study for a M5.4 aftershock of the 2016 Kumamoto earthquake

Fig. 6

Comparison between a localized EM fields and b evanescent EM waves. These wave-fields are calculated for the four receivers with the same lateral offset xr = − 80,890 m and yr = 8680 m, but different depths zr = 0, 500, 1000 and 1500 m in the water-saturated half-space porous model. The signals in the gray boxes are amplified to have a better visibility

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