Fig. 4: Evolution of the model α = 7∘, Δ = 52 km. | Nature Communications

Fig. 4: Evolution of the model α = 7∘, Δ = 52 km.

From: Lithospheric models supported by the Caribbean and Levant examples help rethink transpression at plate boundaries

Fig. 4: Evolution of the model α = 7∘, Δ = 52 km.

The left column shows the stress regime of the active deformation. The central column shows serial cross-sections with the stress regime superimposed. The right column shows the long-term slip-rate on the faults. Fault surfaces are reconstructed following ref. 108. Slip-rate estimation method is detailed in “Slip-rate estimation”.

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