Fig. 6: Spatiotemporal evolution of slip along the EAF during the earthquake cycle. | Communications Earth & Environment

Fig. 6: Spatiotemporal evolution of slip along the EAF during the earthquake cycle.

From: Slip complementarity and deficit of the East Anatolian Fault revealed by geodetic observations

Fig. 6: Spatiotemporal evolution of slip along the EAF during the earthquake cycle.The alternative text for this image may have been generated using AI.

(a1-a4) Spatiotemporal evolution of fault slip on the four branches. Black contours show interseismic slip; green and purple contours denote cumulative afterslip from E-1 and E-2, respectively. Cyan dashed lines outline accumulated slip. The blue star is the epicenter of E-1. Green stars are epicenters of E-2. (b1–b4) Integral of slip along strike for each point at the same depth for the four branches, with associated error bars. (c1–c4) Integral of slip along depth for each point at the same strike for the four branches, with associated error bars. Uncertainties are estimated for each period by the bootstrap method (see Methods and Supplementary Figs. S3, S8, S15).

Back to article page