Fig. 7From: Fault source model for the 2016 Kumamoto earthquake sequence based on ALOS-2/PALSAR-2 pixel-offset data: evidence for dynamic slip partitioningSlip 1-sigma uncertainties for each segment calculated by 200-times iteration of inversion with random noise. a Right-lateral slip on F1. b Normal slip on F1. c Right-lateral slip on F2. d Normal slip on F3. All figures are shown by same color scale in meters and are projected on same UTM coordinate frame (Zone 52)Back to article page