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Fig. 1 | Geomechanics and Geophysics for Geo-Energy and Geo-Resources

Fig. 1

From: Quantitative 3-D investigation of faulting in deep mining using Mohr–Coulomb criterion and slip weakening law

Fig. 1

Schematic illustration of the 3-D model and the fault friction properties. a Geometry of the 3-D model simulating mining-induced faulting. b 3-D image illustrating the Mohr–Coulomb failure criterion for the friction cone on the fault plane. The shear stress state on the fault plane is represented by two orthogonal shear stresses, τ1 and τ2. The relationship between the normal stress σn and the shear stress τ indicates that particles adhering within the red circle slide undergo sliding once they intersect with this circle. c Slip-weakening diagram where the average shear stress is assumed to increase from an initial to peak stress with no slip and then linearly decrease to a dynamic resistance level over Dc

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