Fig. 8
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 values of resistivity in zone C1. Solid gray lines indicate the responses of the optimum model. The responses of the representative models are shown by thick broken lines (20 Ω m), dotted lines (80 Ω m), dash-dotted lines (100 Ω m), and thin broken lines (140 Ω m). Circles with error bars indicate observed responses.