Extended Data Fig. 8: Results from geodynamic simulations.
From: Extensional tectonics and two-stage crustal accretion at oceanic transform faults
a, b, Obliquity of the transform shear zone 10 km below top of the model, as a function of its length for different spreading rates (a) and of age offset for different transform lengths (b). c–e, Depth to plate boundary versus obliquity for different transform lengths, for slip rates of 1 cm yr−1 (c), 3 cm yr−1 (d) and 6 cm yr−1 (e).
