Page 244 - Origin and Prediction of Abnormal Formation Pressures
P. 244

216     V.I. ZILBERMAN, V.A. SEREBRYAKOV, M.V. GORFUNKEL, G.V. CHILINGAR AND J.O. ROBERTSON JR.
                                      Geologic cross-section


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                        "  ~  "  k  L  L  L  L  L  '   I.   P2   L   L.,.   ,.,.   .




                         L   L   1   [   L   o,-   p_3    --   L   ~   C   L   L   L   L   L
                        C   L   L   LI   L   LI   v~   ~    L  I  C   L   L   L   C   L
                         L   L   L   iC.   L  /   ~  t  .    it   L   ~.   L   c   ~.   L
                           L  ~   L
                           i.   L                              9   L   L   C   L   L   .
                            I   '                        I   l
                                         Isopach map (J1)



                                                                        120
                                                100




                                  ',   '                               ' 200

                         L


                        L  LLC f


                                                     -700  ~
                          Legend:
                      [~:1  Stratigraphic boundaries
                      ~   Indicator sequence
                      [7]  Isopachs of indicator sequence   ~   Gas accumulation with AHFP
                          Faults                  ~   Massive gas accumulation
                          Salt plugs              ~   Zone of possible AHFP
            Fig. 9-4.  Direct delineation  of AHRP  zones  in  the  near-plug area.  (After Zilberman  and  Chernyakov,  1981.)


            The  weakness  lies  in  the  delineation  of  the  salt  plug,  which  is  the  boundary  between
            the  accumulation  and  the  AHFP  zone.  As  mentioned  above,  the  seismic  survey  is
            not  capable  to  accurately  delineate  the  salt  plugs.  Errors  in  locating  the  boundaries
            result in poor  well  locations.  As  an  example,  in Western  Krestischensk  gas condensate
            accumulation,  five appraisal  wells  and  one  development well have  been  drilled without
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