Page 89 - The Geological Interpretation of Well Logs
P. 89

-  THE  GAMMA  RAY  AND  SPECTRAL  GAMMA  RAY  LOGS  -


                                                                     2.  RADIOACTIVE  ELEMENTS
                                                         80
                 1.  NON-RADIOACTIVE  ELEMENTS
                                                                                            clays
                                                      100

          detrital  grains                    {






                                                       0
                                                       x
                                                       §  9

                                                       =  40
                                                                                       radioactive  detrital
                                                       8
                                                                                     /
                                                                                           grains
                                                       E  °
                                                       Qa
                                                       3


                                                                     feldspar
                                                                                                =
       0.031   0.0863   0.125     0.25    050       1.0  mM


            SILT    Vv.  FINE   FINE   ME      CSE
                           .     .                        0.031   0.063    0.125    0.25     0.50     1.0  mm
                        median  grain  size   ==
                                                              SILT    Vv.  FINE   FINE    ME      CSE
                                                                           median  grain  size  —~
         Figure  7.16  Radioactive  elements  in  detrital  rocks.  Typical  sandstone  compositian  shown  against  grain  size  for  the  Reindeer
         Formation,  Mackenzie  Deita,  Beaufort  Sea.  Radioactive  elements  vary  with  grain  size.  It  is  a  deltaic  sand  of  Lower  Tertiary  age.
         (Redrawn  from  Nentwich  and  Yole,  1982).
                        Table  7.15  Potassium  content  of  some  common  detrital  materials  (from  Serva,  1979;
                        Edmundson  ef?  ai.,  1979;  Dresser  Atlas,  1983;  Schlumberger,  1985).

                                                %  potassium   Average      Gamma  ray  value
                                Mineral  species   by  weight   %           (API)

                           4    Glauconite*      3.2  -5.8     4.5           75'  -  90'
                          $     Muscovite       7.9-9.8        9.8          140'  -  270
                                Botite           6.2  -  10.1   8.7          90°  -  275


                                Microline        10.9-  16      16          220  —  280'
                           ww
                          xs    Orthoclase       11.8-14        14          220  —  280'
                          cm

                         *Detrital  or  authigenic
                         ‘For  8in  hole,  1.2g/cm?  mud,  3%in  Nal  scintillator

         7.8  Qualitative  use  of  the                     Radioactivity  of sandstones  and
         simple  gamma  ray  log                            other  arenaceous  rocks
                                                            Quartz,  the  principal  component  of  the  coarse-grained
         Lithology
                                                            detrital  rocks,  shows  no  radioactivity.  Sandstones  conse-
         As  a  first  indicator  of  lithology,  the  gamma  ray  log  is
                                                            quently  usually  show  low  gamma  ray  values  (Figure  7.1).
         extremely  useful  as  it  suggests  where  shale  may  be
                                                            However,  associated  detrital  minerals  are  radioactive.  The
         expected  (Figure  7.1).  Moreover,  as  shown  above,  the
                                                            most  common  of  these  are  feldspars,  micas,  heavy
         higher  the  gamma  ray  vajue,  the  higher  the  percentage  of
                                                            minerals  and  lithic  fragments  (Figure  7.16).  The  first  two
         shale  (Figure  7.15).  But  the  log  is  only  a  first  indicator.
                                                            groups  contain  potassium  (Table  7.15),  the  third  thorium
         The  radioactivity  of  some  typical  lithologies  other  than
                                                            (Table  7.12)  and  the  last  contains  shale.  These  all  cause
         shale  is  now  considered.  This  shows  that  any  lithology
                                                            sandstones  with  high  to  moderate  gamma  ray  values.
         indicated  by  the  simple  gamma  ray  log  must  be  con-
         firmed  by  other  logs.
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