Page 275 - The Geological Interpretation of Well Logs
P. 275

-  CONCLUDING  REMARKS  -


        at  present  than  quantitative.  This  will  necessarily  change.   As  tools  become  more  sophisticated,  they  become  more
        The  biological,  astronomical  and  remote  sensing  sciences   dependent  on  such  software  for  signa]  processing.
        have  long  possessed  imaging  and  have  developed  an   Indeed,  this  has  been  demonstrated  with  the  dipmeter
        array  of  image  analysis  techniques.  These  work  on  the   (Chapter  12},  where  the  raw  data  (the  microresistivity
        images  themselves.  They  enhance,  modify  and  extract   curves)  are  uninterpretable  until]  processed  into  dip  tad-
        certain  altributes.  In  image  log  analysis  this  is  just  begin-   poles.  The  dipmeter  also  shows  that  it  is  necessary  to  be
        ning.  For  example,  extracting  dip  from  images  is  familiar.   familiar  with  at  least  some  aspects  of  the  signal  process-
        But  techniques  for  extracting  attributes  indicative  of  thin   ing  in.order  to  make  a  proper  interpretation  of  the
        beds,  of  fractures  and  even  grain  size  and  permeability,   software  produced  results.  The  use  to  which  the  results
        are  being  tentatively  tried  (Sullivan  and  Schepel,  1995).   will  be  put  should  influence  the  processing,  whether  this
        There  is  no  reason  why  more  geological  attributes  should   be  for  geological  or  petrophysical  purposes.  The  current
        not  be  extracted:  facies,  structures,  sequences,  and  these   problem  for  both  geologist  and  log  analyst  alike  is  to  keep
        will  be  quantitative  attributes:  the  software  will  be  new.   up  with  developments.
                                                             The  second  category  is  software  which  aids  interpreta-
                                                           tion.  While  the  influence  of  geological  purpose  on  signal
         16.5  A  rainforest  of  software
                                                           processing  software  is  small,  the  influence  can  be  domi-
        No  one  wants  the  rainforests  to  be  cut  down:  but  it  is   nant  in  interpretation  software  (should  be  dominant).  This
        happening.  No  one  wants  to  throw  away  software:  but   point  was  made,  again,  with  dipmeter  interpretation:
        they  should.  Software  comes  in  many  guises:  indispens-   dipmeter  manipulation  sofiware  should  be  designed  with
        able,  useful,  infuriating,  fancy,  pretty,  pretty  useless  and   geological  ends  in  mind  (Chapter  12),  The  problem  at
        unnecessarily  expensive.  5%  for  the  first:  40%?  for  the   present  is  that  much  geological  software  is  written  by
        second:  certainly  80%  for  the  last.  Let's  look  at  software.   software  writers  and  undirected  by  geological  needs.
        There  are  essentially  two  categories,  the  first  is  signal   There  are  many  ‘feature  rich’  packages  in  which  the
        processing  software,  the  second  is  interpretation  software.   routines  dreamed  up  by  the  software  writers  are  very
          An  example of the  first  category  is  the  software  used  to   impressive,  but  in  practical  terms,  useless.  Many  simple

        produce  the  output  from  the  NMR  tool  discussed  above.   routines  which  would  be  useful  have  not  been  written.
        Interpretable  information  is  only  produced  from  the   An  exception,  and  notable  for  that,  is  time  series
        processed  raw  tool]  responses:  there  is  a  software  interface   analysis  of  log  traces.  This  type  of  analysis  treats  a  log  as
        between  the  raw  data  and  the  interpretable  information.   Gamma-Ray
                                                           a  geological  record,  containing  therefore,  a  time  element

                                                                                     Foraminifera
                                                                                                   Age
                 Kirchrode  1/91
                                                                                               100%  My
                                                                                        60%
                                                                                                   ae
                                                                                           +
                     1
                       pirate  ]                           (10cm  sample}
                                                                                    ss

                                                                                      r
                    a
                                                                                       A
                    ES ieee   eet   es                                           benthos   wy  }
             cycles   yr)   a   ee                                                      we   <="
             12m   100,000    cee                                                    i
                                                                                      .
             strong    a      =                                                       S           is
                                                                                                    2
                                                                                  c               |.
             |                                                                        5             <
             16m-35m   cycles                                                      —   4          |  >
                                                                                                    a
                                                                                    fs
                                                                                    ——————
               ‘chaotic’                                                            —_       *     |  99.0
                                                                            ~
                                                                                       <
                                                                            ~al
                                 4
                                                                         ia
                                        5.2
                                             Thickness  of |  P  -phosphorite  coneretio  ns
           |
                    4835  24  18
                                  12
                                            Periods  in  m|  Gl  --glauconite

        Figure  16.5  Wavelet-spectrogram  representation  of  a  gamma  ray  log  processed  using  a  wavetei-transform  method  to  bring  out
        cyclicity.  The  section  from  35m-163m  shows  well  developed  12m  thick  cycles  associated  with  a  100,000  year  eccentricity  period.
        Upper  Albian  marls,  North  Germany.  Sedimentation  rate  from  biostratigraphy,  about  10cm/1000yrs  (gamma  ray  data  from
        J.  Thurow,  biostratigraphy  from  BCCP  Group.  1994).
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