Page 247 - The Geological Interpretation of Well Logs
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-  FACIES,  SEQUENCES  AND  DEPOSITIONAL  ENVIRONMENTS  FROM  LOGS  -
                                                              LITH.

                         3"   GAMMA    RAY  API            |            SONIC  Réit     7
                 Oo,   ,   ,  “caliper   100    1590

              0      SS
                    \Y  1  al.                           g
            10m  4       “     y-  aR                  xe
                                                       WO
                                            dip  2°    ox
                   N                      _            Er
            20m  -                                       3
                     bit
                   size  v                                                                   gep
                   IWS                           7
                                                                                            c15  ma

            30m  4   SN             UNCONFORMITY         a
                                        PEAK             5

                                      Oo OeeeelG       a
                                                         cc  oO

            som
      Figure  14.19  Anomatous  gamma  ray  peak  at  an  unconformity.  The  peak  corresponds  to  gap  of  [5  Ma:  its  stratigraphic  importance
      is  evident.  The  radioactivity  is  probably  due  to  uranium  concentrated  in  phosphatic  nodules.











                                                                AUNAL
              .                    SHALLOW         DENSITY      ENV.       f
           el]e|@]   .   GAMMA  RAY   |resisTivITY                 =|   Mason  |  envs.   BREAKS   co
           e/#)S]   =z  E                   Sonte             3  Reig  g   crcLes   SEQUENCES   MMENTS
           5|z13)   5
         °             2        x00}                          B22           i   -

            |
           w)   ic                                                                     '

           5/2                                                         FU          deepening   bagin  sinking?
           a3]   2

              oS

             >
                                                                                 UNCONFORMITY:  | _ slight  structuration
                                                                                    MAJOR    Limit
        26  7                                                 =
                                                                               |   progressive
                                                                       more        deepening   sea  level  tise?
                                                                       marine
                                                               LL
             <=
             =                                                   LL                FLOODING:   =|
             3
                                                                    _              EXTENT?   SEQUENCE  LIMIT?
             «                                                                    tluvial  channel
             s                                                          FU          in  core
           yg]
       6)  3   =                                                   co            erosion:  channel,
           <x                                                                     delta  top  Isuna
                                                                                    in  core

           &
           -                                                     }——4
                                                                 =      u           major
                                                                      \  e          della
       764                                                                        progradalion
                                                                     LC   oe   ee              MAJOR
                                                                                             PROGRADATION
          5
          at

          &
                  =z                               a  4  =              |   i  aur                            l    FLOODING:
          8                                         3  s                 cv
                                                     =
             «
             8
                                                     >
                                                   a
             5
      400m  +  ist                                                                          eustatig  sea  level
                                                    a
                                                    ‘>
                                                   2
                       .
                                                                                                ise
                                                       5
                                                                                    MAJOA
                                                                                             SEQUENCE  LIMIT
                                                       a



      Figure  14.20  A  completed  electrosequence  analysis.  Lithology,  electrofacies  and  sample  data  are  brought  together  to  give  a  verti-
      cal  sequence  of  depositional  environments  and  an  indication  of  the  depositional  sequences  and  major  breaks.
      *Environments:  |,  deeper  marine;  2,  shallow  marine;  3,  prodelta;  4,  delta  front;  5,  delta  top;  6,  channel;  7,  beach-littoral;  8,
      continental;  CU  =  coarsening  up,  FU  =  fining  up.

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