Page 152 - Reservoir Geomechanics
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a.
                             Stress or pressure
                     0    20    40    60    80  MPa
                    0
                        2000 4000  6000  8000  10000  12000  psi

                                       Normal faulting
                  1000
                      4000           overpressure at depth
                                    S v  ≥ S Hmax  ≥ S hmin
                 Depth (meters)  2000  6000  S hmin

                      8000
                                  S Hmax
                  3000         P p
                      10000              S v
                      12000 (feet)
                  4000



               b.            Stress or pressure
                     0    20    40    60   80   MPa
                    0
                        2000 4000  6000  8000 10000  12000  psi
                                      Strike-slip faulting
                  1000               overpressure at depth
                       4000
                                    S Hmax  ≥ S v  ≥ S hmin
                 Depth (meters)  2000  6000  S hmin


                       8000
                                        S Hmax
                  3000         P p
                       10000
                       12000 (feet)          S v
                  4000



               c.            Stress or pressure
                     0    20    40    60   80   MPa
                   0
                        2000 4000  6000  8000  10000 12000  psi
                                       Reverse faulting
                                     overpressure at depth
                                     S Hmax  ≥ S hmin  ≥ S v
                  1000
                      4000
                 Depth (meters)  2000  6000  S hmin

                      8000
                               P p  S v  S Hmax
                  3000
                      10000
                      12000 (feet)
                  4000



              Figure 4.29. Same as Figure 4.28 when overpressure develops at depth as shown. Note that in all
              three stress states, when pore pressure is nearly lithostatic, all three principal stresses are also close
              to S v .
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