Page 168 - The Geological Interpretation of Well Logs
P. 168

-  THE  GEOLOGICAL  INTERPRETATION  OF  WELL  LOGS  -

        Table  11.1  Logging-too]  response  values.  All  vatues  are  shown  so  that  they  cover  the  ranges  found  in  the  various  sources,  i.e.
        none  of  the  sources  has  values  outside  those  listed.  Prom  Serra  (1972,  1979),  Dresser  Atlas  (1983),  Gearhart  (1983),
        Schlumberger  (1985,  1989a).

              Material         Resistivity    Gamma  ray    Auna          Density  log   Neutron  porosity
                               (ohm  m?/m)    API           (usif)        (g/cm?)  (ma)   units

        c  %   Sandstones      up  to  1000   18-160        53-100        2.59-2.84      0-45
        E  ‘a   Limestones     80-6  X  107   18-100        47.6-53      2.66-2.74      0-30
         53  °0   Dolomites     1-7  X  106   12-100        38.545        2.8-2.99       0-30
        Y=    Shales           0.5-1000      24-1000        60-170        2.65-2.7       25-75

        *  2   Quartz           }o-10     >                 $1.2-56      2.64-2.66       -2
        Ee  &   Calcite         107-39?       0             45.5-49       2.71           -)
        =  2   Dolomite         1-7  X  103   0             38.5-45      2.85-2.88       1

          4   Illite                         250-300                      2.52-3.0       30
        z  &   Chlorite                       180-250                     2.6—3.22       §2
        uO  <   Kaolinite                     80-130                      2.4-2.69       37
              Smectite                         150-200                    2.0-3.0        44

        g     Glauconite                      75-90                       2.2-2.8        38
        3     Muscovite         10"'-16"       140-270      49            2.76-3.1       20
              Biotite           10'-10'5      90-275        50.8-5 1      2.65-3,1       21

        2.    Microline                       220-280       45            2.53-2.57      3
        a     Omnhoclase                      220-280       69            2.52-2.63      —3

        ”     Anthracite        103-5         0             90-120        1.32-180       38
        s     Bituminous  coal   10-10°       0-18           100-140      1.15-1.7       60
        e     Lignite          4X  lo?       6-24            140-180      05-15          52

              Gas  (av.)        a             0                           000886
        a     Methane          ct             0             626           00076
        S     Oil  (40°  API)   10-10"        0.12-0.40     238           85-97          60
        4     Water  (80°F)
        2      pure             a             0              189-207      1.00           100
               salt
               (33,000  ppm)    0.035  (var)   0             180           L.19          60

        2s
        3  g   Pyrite           j0-'-10~%                   39.2-39       4.8~-5.17      -3
        =  3   Siderite         10*-1000      0             47            3.0-3.89       12

        a     Halite            <10"-10"      0             66.7-67       2.03-2.08      3
        2     Anhydrite         10-10"       0-12           50            2.89-3.05      -2
        a      Gypsum           1000          0             52-53         2.33-2.4       60
        a     Syivite           10-10"        500           74            1.86-1.99      -3
               Polyhalite                     200           57.5-58       2.79           25

        =      Basalt           8  X  102105   12-24        45-57.5°      2.7-3.2
          3    Granite          108           24-96         46.8-53.5     2.52-2.8
        5     Gneiss            10-10!        24-48         48.8-51.6     2.6-3.04

              (1}  No  hole  conditions  specified:  wil!  therefore  vary,   (4)  Calibrated
              (2)  Values  for  the  matrix  material,  compressional  wave.   (5)  Pressure  1  kbar.
              (3)  For  the  CNL  tool  of  Schlumberger               (6)  All  values  variable.
              Fsp  =  Feldspars   ma  =  matrix
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