Modeling of the coseismic electromagnetic fields observed during the 2004 M w 6.0 Parkfield earthquake

The coseismic electromagnetic signals observed during the 2004 M w 6 Parkfield earthquake are simulated using electrokinetic theory. By using a finite fault source model obtained via kinematic inversion, we calculate the electric and magnetic responses to the earthquake rupture. The result shows that the synthetic electric signals agree with the observed data for both amplitude and wave shape, especially for early portions of the records (first 9 s) after the earthquake, supporting the electrokinetic effect as the reasonable mechanism for the generation of the coseismic electric fields. More work is needed to explain the magnetic fields and the later portions of the electric fields. Analysis shows that the coseismic electromagnetic (EM) signals are sensitive to both the material properties at the location of the EM sensors and the electrochemical heterogeneity in the vicinity of the EM sensors and can be used to characterize the underground electrochemical properties. Coseismic EM signals were observed during the 2004 Parkfield earthquake The coseismic EM signals were modeled based on electrokinetic theory The synthetic electric fields explain the observed data