Fig. 11
From: Audio-frequency magnetotelluric imaging of the Hijima fault, Yamasaki fault system, southwest Japan
Comparison of MT responses between the optimum model and the models with assumed depths of the lower boundary of zone C2. Solid gray lines indicate the responses of the optimum model. The responses of the representative models are shown by broken lines (1.6 km), thin dotted lines (1.4 km), and dash-dotted lines (1.2 km). Circles with error bars indicate observed responses.