Page 182 - The Geological Interpretation of Well Logs
P. 182

-  THE  GEOLOGICAL  INTERPRETATION  OF  WELL  LOGS  -
               STANDARD  RESISTIVITY  Qm?/m   SHDT

                                             resistivity
                                              —e
            1          19        100      1900
        177m

                                                                             meas uring
                                                                             electrodes
                                                                  bem

                                                                        e
        1800m

                                                                      PS


                                                                                       “SHOT  DIPMETER
                                                                                           PAD

                                                            ek        J -upt pap
        1825m
                                                                       at  eee   ata   Pe  ae   fe  tie  eye.

                                                          Figure  12.5  Dipmeter  pads.  The  single  electrode  HDT  (High
                                                          Resolution  Dipmeter)  pre-1985  and  the  two  electrode  SHDT
                       MSFL          LLO                  (Stratigraphic  High  Resolution  Dipmeter)  with  2  shorter  pad
                                                          for  better  formation  contact.  (re-drawn  from  Schlumberger,
       Figure  12.4  Standard  resistivity  logs  compared  to  SHDT  dip-
                                                          1986).
       meter  resistivity  curves.  The  SHDT  curves  are  sampled  every
       0.25cm  (0.1")  and  are  very  detailed  while  the  standard  logs
       are  sampled  every  15cm  (6").  However,  the  SHDT  curves  give
                                                          Field  log  presentation
       only  relative  resistivity  values,  as  base  resistivity  (EMEX)
                                                          Two  types  of  dipmeter  log  are  produced.  The  first  is  a
       vanes  depending  on  formation  resistivity.  In  this  way,  detail
                                                          field  log,  a  plot  of  the  raw  data  acquisition  curves;  the
       is  measured  in  both  the  absolute  low  and  high  resistivity
                                                          second  presents  the  processed  data  —  the  actual  dips
       intervals  (hydrocarbon  bearing  in  this  example).  SHDT  =
       Stratigraphic  High  Resolution  Dipmeter  of  Schlumberger.   derived  by  the  computer.  The  field  logs  will  be  described
                                                          in  this  paragraph,  the  logs  showing  dips  are  described  in
       Orientation  and  other  measurements              section  12.4.
       To  calculate  the  resistivity  curve  displacement  across  the   A  typical  dipmeter  field  log  will  show  not  only  the  raw
       borehole,  clearly,  the  borehole  size  must  be  known.  To   microresistivity  curves,  but  also  most  of  the  orientation
       this  end,  the  two  pairs  of  arms  measure  two  independent   and  caliper  data.  The  example  chosen  is  from  a  Western
       calipers,  giving  two  orthogonal  hole  size  measurements.   Alas,  4-arm  (pad)  Diplog  (Figure  12.6).  In  track  1  are  the
        This  allows  a  dip  to  be  calculated  from  the  displacement.   deviation  of  the  borehole  from  the  vertical  (DEV)  and
        However,  for  this  plane  to  represent  the  true  dip,  in  other   azimuth  (DAZ),  the  azimuth  (AZ)  of  the  reference  pad
        words  not  just  any  plane  but  referenced  to  north,  other   (pad  1)  and  a  gamma  ray  curve  from  a  sonde  attached  to
        orientations  must  be  measured  by  the  tool.  These  are:  the   the  dipmeter  tool.  The  gamma  ray  allows  the  dipmeter
        orientation  of  the  too]  in  relation  to  north  (pad  J  acts  as   to  be  matched  to  the  standard  log  rums  (note  the  great
        the  tool  reference  =  pad  |  azimuth):  the  deviation  of  the   difference  in  detail  between  the  gamma  ray  and  the
        axis  of  the  tool  from  the  vertical  (=  the  deviation  of  the   dipmeter  curves),  In  tracks  2  and  3  are  the  raw  acquisition
        borehole):  the  direction  of  this  deviation  relative  to  north   curves,  the  tension  and  the  two  calipers.  The  tension
        (=  azimuth  of  hole  deviation,  sometimes  called  drift).  The   curve  is  useful  in  identifying  zones  of  tool  sticking
        latter  orientation  is  calculated,  not  measured,  from  the   although  these  are  usually  evident  on  the  caliper  and  the
        ‘relative  bearing’,  which  is  the  clockwise  angle  between   raw  curves  themselves.  The  format  of  the  raw  dipmeter
        pad  |  azimuth  and  the  high  side  of  the  tool  (this  is  the   data  varies  between  companies  although  the  basic  infor-
        same  as  the  hole  deviation  azimuth  orientation),  Pad  1]   mation  included  is  similar.  The  logs  are  plotted  at  a  1:200
        azimuth  minus  yselative  bearing  azimuth  (+360°)  =  hole   scale.
        deviation  azimuth.  Speed  variations  may  also  be  mea-
        sured.  This  can  be  done  directly  by  using  accelerometers
                                                          12.3  Dipmeter  processing
        or  by  using  a  speed  electrode.  The  latter  is  a  duplicate
        electrode  on  one  or  two  of  the  pads,  several  centimetres   Generalities
        vertically  above  the  main  electrode,  which  should  dupli-   To  derive  a  dip  direction  and  azimuth  from  the  raw,  tool
        cate  the  main  measurement.  When  there  are  large  speed   produced  resistivity  curves,  needs  computer  processing.
        differences  the  speed  electrode  and  main  electrode  read-   The  requirement  is  to  correlate  the  curves  around  the
        ings  will  differ  and  corrections  can  be  made.   172   borehole  so  as  to  identify  the  various  displacements,
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