Fig. 10From: High-density surveys conducted to reveal active deformations of the upper forearc slope along the Ryukyu Trench, western Pacific, JapanStacked seismic profiles across the southern Yoron Basin (see Fig. 2 for the track location). Traceable normal faults are located in the Yoron Basin. The faults strike east-west and dip to the north. The faults have deformed the uppermost sediments, thereby indicating that they are activeBack to article page