Extended Data Fig. 4: Simplified model relating driving shear traction τD, normal traction σn, μ, and slip s along the tiger stripe faults. | Nature Geoscience

Extended Data Fig. 4: Simplified model relating driving shear traction τD, normal traction σn, μ, and slip s along the tiger stripe faults.

From: Jet activity on Enceladus linked to tidally driven strike-slip motion along tiger stripes

Extended Data Fig. 4

Upper row: Frictionless fault subject to driving tractions. In this case, the fault cannot support shear traction (resolved shear traction τR = 0) and driving traction τD is resolved along interfaces (s ≠ 0) regardless of the applied σn. Slip results in a concentration of elastic strain at the fixed ends of the fault. The subsequent unloading of the driving shear traction results in a return to zero slip. Center row: frictional fault with time-variable driving shear traction and constant normal traction. In this case, s ≠ 0 when τD > σnμ (that is, τc = τD − σnμ > 0). Constant values of σn result in symmetric slip profiles following the onset of sliding. Bottom row: frictional fault with time-variable driving shear and normal tractions. In this case, variable σn results in an increased magnitude of τD required to initiate sliding and an associated decrease in the amplitude of s during the first occurrence of τc > 0. The resulting slip profile is double-peaked and asymmetric.

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