Fig. 4
From: Geoelectrical evidence of fluid controlling slow and regular earthquakes along a plate interface
(a) Resistivity section along the plate interface. (b) Resistivity section along a surface 10.5 km below the plate interface. Note that this surface corresponds to the region where KPR range was estimated based on low-velocity anomaly29. (c) Vertical section along line B–B’. (d) Interpretation of the section shown in (c). Red diamonds are OBEM observation sites. Other symbols are same as Fig. 2.
