FIGURE 3.26. Graph showing variation in differential stress necessary to initiate sliding on reverse, strike-slip, and normal faults, as a function of depth. The relationship is given by Equation 8.1, assuming a friction coefficient, μ=0.75, and a fluid pressure parameter, λ=0 (no fluid present) and λ = 0.9 (fluid pressure is 90% of lithostatic pressure).
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