Fig. 2: Pre-stack depth migrated section of seismic dip-lines.
From: Megathrust reflectivity reveals the updip limit of the 2014 Iquique earthquake rupture
Yellow arrows indicate a coherent plate boundary reflection. The vertical red dashed line denotes the location of the deformation front. The red arrows specify the intersections with the strike lines. Temperatures are shown as colored dots according to the color bar. The approximate depth range of smectite clay dehydration is based on refs. 2,7,29,32,33. a seismic line MC04. b seismic line MC06. c seismic line MC25. d seismic line MC17.
