Page 272 - The Geological Interpretation of Well Logs
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-  THE  GEOLOGICAL  INTERPRETATION  OF  WELL  LOGS  -


                          GR  total                                          OUTCROP
                            cps        Th  ppm     K%   40   U  ppm   14   SEDIMENTOLOGY
                                                              6
                        30      40   6   12   200
                                                                                    HIGHSTAND   SYSTEMS   TRACT
                     10  5



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                                                                                    TRANSGRESSIVE   SYSTEMS   TRACT








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                          OUTCROP  SPECTRAL  GAMMA  RAY

                          Q  goniatites    ®  crinoids

        Figure  16.1  Outcrop  spectral  gamma  ray  profile  of  key  sequence  stratigraphic  surfaces  including  an  important  maximum  flooding
        surface  (MFS).  Carboniferous  (Namurian),  Western  Ireland,  SB  =  sequence  boundary.  IFS  =  initial  flooding  surface.  FS  =  flooding
        surface  (data  from  §  .Davies,  modified  from  Davies  and  Elliott,  1996).



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                    0.5     2.5     4.6    (2.5)   [4.5]                                         6
                                   {0.5]                                        GR  (AP!)  —
                         83  C  %o  PDB  Benthics                            Central  North  Sea
                                                          massive  shale  (bioturbatad}
                                                    ES    laminated  shale  anoxic}
        Figure  16.2  The  Palaeocene-Eocene  boundary:  carbon  isotope  values  in  deep  ocean  cores  of  the  North  Pacific  (Skatsky  Rise),  South
         Adlaatic  (Walvis  Ridge)  and  Weddell  Sea  (Maude  Rise)  compared  to  gamma  ray  logs  from  a  well  in  the  Central  North  Sea  basin.
        See  text  for  discussion  (modified  from  Corfield  and  Norris,  1996  for  isotopes  and  O’Connor  and  Walker,  1993  for  well  Jogs).
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