Page 100 - The Geological Interpretation of Well Logs
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-  THE  GEOLOGICAL  INTERPRETATION  OF  WELL  LOGS  -


                                                   a<#—;
               xr                                  excess’  &       ———$—$<$<—$   >   ~
                   L                                       l

                                                                     Thorium  pom
               5           GAMMA  RAY  API     240      ThiU  ratio   106]20  '   ojo   K%   5/10  Uranium  ppm
                                                           3
                                                    pitinet   7          1   )   1   1   )   4   L   1   b   )   1
                                                             10

                                                             mS
          cdE
                        ay,  rus,  2
                     OQ   Q
        10m
        20m

        30m
                td  =  condensed  sequence  (marine  band}
        Figure  7.31  Condensed  shale  sequences  showing  very  low  thorium/uranium,  Th/U  ratios  due  to  ‘excess’  uranium  content.  Most
        shales  have  a  THU  ratio  of  3-6,  the  ‘norm’.  In  condensed  sections,  where  organic  matter  is  concentrated,  uranium  values  are
        abnormally  high  and  cause  Th/U  ratios  of  less  than  3.  The  low  ratio  can  be  diagnostic.

        analysis  (Chapter  15).  Condensed  sequences  in  marine   Fracture  localization
        areas  arise  when  the  detrital  influx  into  an  environment  is   The  mobility  of  uranium  and  its  presence  in  formation
        low.  This  causes  a  relative  increase  in  the  in-situ  material   waters  is  considered  to  be  the  cause  of  high  uranium
        over  the  externally  derived  detritus.  In-place  material   radioactivity  in  fractures  and  faults  (Fertl,  1979;  Fertl  and
        typically  consists  of  the  shells  of  pelagic  macro-  and   Rieke,  1980).  Using  the  spectral  gamma  ray  log,  zones  of
        micro-fauna  and  locally  derived  organic  material,  alt  of   high  uranium  radiation  can  be  detected,  and  other  logs
        which  simply  fails  to  the  depositional  surface  to  form  4   may  be  used  to  confirm  that  fractures  are  present.
        slowly  accumulating  (organic  rich)  sediment.  Provided
        that  there  is  a  low  rate  of  dissolution,  (i.e.  that  the  envi-   Comment
        ronment  is  oxygen  depleted  or  deficient  =  anoxic)  the   Because  a  precise,  quantitative,  petrophysical  use  for  the
        amount  of  organic  maiter  in  the  condensed  sequence  will   gamma  ray  spectral  log  has  not  been  found,  it  is  frequently
        be  high,  and  in  a  marine  environment,  will  have  2  high   not  included  in  a  logging  suite.  This  is  short-sighted.  As
        adsorbed  uranium  content.  On  the  gamma  ray  spectral   methods  are  developed,  such  as  those  outlined  above  (but
        log,  this  high  uranium  content  will  show  up  as  a  low   which  only  represent  a  start),  spectral  logs  in  old  wells  will
        Th/U  ratio.  That  is,  using  the  methodology  proposed   be  sought  in  vain.  There  is  no  doubt  that  geologically,  a
        above,  condensed  sequences  will  show  ‘excess’  uranium   knowledge  of  the  distribution  of  the  three  naturally
        (Figure  7.31).  Using  this  ratio  based  method  is  more   radioactive  elements  leads  to  a  much  more  refined  interpre-
        accurate  and  selective  than  simply  using  high  overall   tation  of  depositional  environments,  mineral  content  and
        gamma  ray  (i.e.  gamma  sptke)  or  even  high  uranium  val-   fluid  locatisation.  The  use  of  these  logs  in  sequence  stratig-
        ues  (Chapter  15).                               raphy  and  all  that  it  implies  is  particularly  significant.




























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