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On the Reactivation of the Pre Existing Normal Fault

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Figure

Figure 1. Coulomb fracture criterion and frictional sliding criterion for the same rock
Figure 3. A reactive pre-existing fault with minimum dip angle and a newly formed
Figure 4. Coefficient of pore fluid pressure vs. minimum dip angle for pre-existing fault for various depthes
Figure 5. Coulomb shear fractures and reactive pre-existing faults with increasing αangles of pre-existing faults in less confining pressure and higher confining pressure

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