Page 79 - Origin and Prediction of Abnormal Formation Pressures
P. 79

ORIGIN OF ABNORMAL FORMATION PRESSURES                                 61


                          ~   15

                         QC
                                ,Xx\o   \
                                 xxx\   \
                                \~,  ,x~l!x,
                                   x  x~xx  \
                                          -
                         [   s          xx~O   9  x   x
                         o
                                                             x-""'~_
                                           XX~X
                                                                 _
                         if)   I        x..x -~  x x  -'~.._ X   x   x
                         w   3
                         Z
                         -r
                         ~   0       !     I     i     I     t      I
                                    0.5    1.0   1.5   2.0   2.5   3.0
                                       DISTANCE  FROM  FAULT,  KM
                            I00


                         j   80                     B
                         (..9            e 13
                         ~2
                         ~  .60
                         _.1             2o ,,
                            4O
                                           17'
                         W
                         I-.                         14
                         ~   20                          0 22
                                                  012   O 9
                                     i     I     !     I     !      I
                              0.9   0.9'5   1.0   i.05   I.i   1.15   1.2
                                        _FORmAl" tON  PRESSURE
                                        HYDROSTATIC  PRE SSURE
            Fig. 2-23. Correlations between the thickness  of gas-filled rocks and distance from the fault (A), and between
            the  pressure  abnormality  and  water  salinity  (B)  for  pre-Jurassic  formations  of  the  North  Rakushechnoye
            field,  Mangyshlyak  Peninsula,  west  coast  of  the  Caspian  Sea,  Kazakhstan.  (Modified  after  Larichev  and
            Timurziev,  1987;  in Gurevich  and Chilingarian,  1997,  fig.  8, p.  328.)



            (Fig.  2-24).  Thus,  fluids  were  collected  at  the  roots  of  the  fault  and  transferred  (in-
            jected) upward through the fault into formations within the fractured zone.  The pressure
            distribution,  therefore,  is  controlled  by  these  injection  scenarios.  To  predict  a  pressure
            abnormality  of  this  type,  approaches  that  are  different  from  the  current  ones  should
            be  used.  A  combination  of  various  geophysical  methods  with  geologic  studies  can  be
            recommended for a case like this.
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