Extended Data Fig. 7: Tectonically accommodated strain along the Chile Ridge.
From: Mid-ocean ridge unfaulting revealed by magmatic intrusions
Cumulative fault heave versus distance from the axis along individual transects from each segment of the Chile Ridge, based on the fault scarp compilation of ref. 24. Red and yellow dots correspond to the western and eastern sides of the axis, respectively, with best-fitting piecewise linear functions shown as black lines. This excludes poor fits highlighted in grey in Supplementary Table 3.
