Fig. 10
From: Half-graben inversion tectonics revealed by gravity modeling in the Mikawa Bay Region, Central Japan
Profiles of the Bouguer anomaly and the topography of the basement surface with 600 m of displacement along the Kou Fault at 2.26 km with a dip of 45° E. a Reverse fault structure of the Kou Fault using the optimal basement model. b Normal fault structure of the Kou Fault using the optimal basement model. Lines and circles are same as shown in Fig. 8. The origin of the x-axis is set at the tip of the Utsumi Fault in both a and b