Fig. 3: Percentage of finite strain accumulation in a lithospheric shear zone.
From: Grain-size-evolution controls on lithospheric weakening during continental rifting
Strain due to diffusion creep (blue) or dislocation creep (white) after 20 Myr of divergence. Red, contour of η = 1021.5 Pa s indicating thickness of the elastic lithosphere. a, COH = 50 H/106 Si. b, COH = 175 H/106 Si. c, COH = 600 H/106 Si. d, COH = 2,500 H/106 Si.
