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5.  Applied Source Rock Geochemistry   103


                    '  OXYGEN   HYDROGEN   ORGANIC   WELL   i  HYDROCARBON  SOURCE   RE  HYDROCARBON
                     INDEX   INDEX    CARBON      DATA   i    POTENTIAL   I  F LECTANCE  i   INDICATIONS
                                                                           AND  TMAX  i
                DEnH                     I                               1    I
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                             S,  ;HCS   ALREADY  IN  ROCK   S,  ;HCS   FROM  KEROGEN  PYROLYSIS.   S3 ;CQ2  FROM  KEROGEN  PYROLYSIS.
             Figure 5.4. Geochemical log for well I, showing immature and mature source rocks in the Upper and Lower Cretaceous
             (see Tables 5.1-5.3). Mud gas data were unavailable for this well.
             II.  High  productivity  indices  (at  100-600  m  and   equivalent 0.5% for this unit). Because it is very thick, the
             1820-2600  m)  are an artifact  of low S1 and  S 2  values  in   Upper Cretaceous source rock still shows a high SPI of 15
             rocks containing highly oxidized organic matter.   t HC/m 2 . Variations in TOC and HI in the Upper Creta­
               Well  III  is  located  about  80  km  northwest  of  well  I   ceous  source  rock  in  this  well  are more  obvious  than  in
             (Figure 5.6). Sidewall cores are indicated by dotted bars,   wells I and II and can be explained by local sea level fluc­
             while ditch cuttings are indicated by  solid bars.  Only the   tuations.  Geochemical  parameters  on the logs in  Figures
             Upper  Cretaceous  potential  source  rock  was penetrated   5.4-5.6 allow  individual  units  to  be  correlated  among
             in this well.  This unit is less oil prone than in  wells I and   these  three  wells,  similar  to  conventional  correlations
             II, but  it  is  approaching  the  onset  of oil  generation  (R,   using wireline logs and paleontology.
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