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In situ stress regimes with lithology-dependent and depletion effects  171


                          6000
                                                         Measured stress
                          6100                           Possible stress

                                 sandstone
                          6200
                         Depth (ft) 6300  sandstone

                          6400

                          6500    shale
                                 sandstone
                                  shale
                          6600
                                 sandstone
                          6700    shale

                          6800
                             3000  3500  4000  4500  5000  5500  6000
                                       Minimum in-situ stress (psi)
              Figure 5.5 The minimum horizontal stress measured from overcoring of open-hole
              hydraulic fracture tests in the Canyon Sands in West Texas (plotted based on the
              data in Miller et al., 1994).




                           120

                           110
                           100                 RF
                          (MPa)  90      SS

                          σH
                            80              σv
                                       NF
                            70                             mu = 0.2
                                             σ σv = 82.5 MPa  mu = 0.6
                                             Pp = 69.7 MPa
                            60
                             60     70    80    90   100   110   120
                                             σh (MPa)
              Figure 5.6 Stress polygons plotted with the same vertical stress and pore pressure as
              shown in Fig. 5.3, but with two different coefficients of friction of the fault m f ¼ 0.6 and
              m f ¼ 0.2. A smaller m f (mu in the figure) corresponds to a smaller stress polygon.
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