Page 105 - Fundamentals of Gas Shale Reservoirs
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APPLICATIONS   85
            vertical  stratigraphy common  and  interpretable,  but over   overlain by an upper HST interval which exhibits a lower
            long distances sequences and parasequences can be expected   gamma ray response. In terms of geomechanical properties,
            to downlap and terminate onto an organic‐rich condensed   Slatt and Abousleiman (2011) refer to these as “Brittle–
            section (Figs. 4.5 and 4.11 are examples).           Ductile couplets.”
              Another important application is the ability to relate   Although it may seem that drilling into a CS/mfs
            stratigraphic  features  to  geomechanical,  geochemical,  and     (ductile strata) might provide the opportunity to release
            other features of shale strata, and through sequence strati­  more hydrocarbons than in more Brittle HST strata, these
            graphic correlations, to be able to map those properties. An   intervals tend to not fracture as well, and drilling can be
            example is shown in Figure 4.17 where P‐wave impedance,   more hazardous in the organic‐rich zones (Figs. 4.18 and
            TOC, fracture gradient, and isopach thickness of two   4.19). By contrast, drilling into the Brittle zone of a Brittle–
            Woodford Shale intervals (labeled GRP‐4 and GRP‐5) were   Ductile couplet has the opportunity to produce longer vertical
            mapped on the basis of logs from several wells (Amorocho‐  fractures that will release more hydrocarbons (sweet spot).
            Sanchez, 2012). Taken together, these two intervals com­  In addition, proppant will tend to keep fractures open in
            prise a high‐frequency sequence consisting of a lower,   the Brittle zone, but not as readily in the ductile zone
            organic rich, high gamma ray CS/mfs interval (GRP‐4)   (Terracina et al., 2010).





                                                                                      Fracture  Fracture
                           GR     RT90      PE      TOC    Impedance  RHOB   Porosity  gradient  toughness
                          Bad_hole  RT90 (derived)1  PE  TOC  P_Impedance  PHOB  Porosity  FG    Kic
                        0.00  10.00  2.0 ohm.m 200.0 2.00  4.00 0.00  20.00  xxxxxx  1.95 g/cm3 2.95 0.00 ft3/f13 0.60 0.40 psi/ft 0.90 0.00 MPa 1.80
                           GR              Color  ll  Color  ll  Color  ll  Color  ll  Color  ll  Color  ll  Color  ll  Rock
                       0  gAPI  800
                         Color  ll                                                                     type
                  20 ft

                  GRP-10
                                                                                                        Upper woodford
                  GRP-9



                  GRP-8



                  GRP-7
                  GRP-6

                  GRP-5

                  GRP-4                                                                                 Middle woodford


                  GRP-3


                  GRP-2
                                                                                                       Lower  woodford
                  GRP-1





                                 Rock type I            Rock type II          Rock type III
            FIGurE 4.18  Properties of a Brittle–Ductile couplet, potential drilling target, Woodford Shale. After Amorocho‐Sanchez (2012).
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