Page 29 - The Petroleum System From Source to Trap
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1.  The Petroleum System   21


              This example shows the use and limitations of oil-oil   the  present  day, the source rock would  presently  be  at
            and  oil-source  rock  correlations.  First,  if  two  oils  are   maximum burial depth; see Magoon,  Chapter 22;  Cole
            identical,  they  may  not  necessarily  be  in  the  same   and  Drozd,  Chapter  33,  this  volume.)  Various  articles
            petroleum system even though the oil-source rock corre­  and computer programs exist to model petroleum gener­
            lations  indicate  that  they  are  from the same  source  rock.   ation and migration; most  use the burial  history curve or
            Second, if two oils are different, they can still be from the   geohistory  chart  (Waples,  Chapter  17, this  volume).  The
            same  source  rock.  For  example,  if  the  organic  facies   essential elements of the system should be shown on  the
            changes within a pod of active source rock,  the  oils may   burial history chart.
            be from the same petroleum system.  Finally, to identify a   Next,  a  map  and  cross  section  are  drawn  for  the
            petroleum  system  uniquely,  the extent  of  hydrocarbon   critical  moment  (Figures  1 . 3  and  1.4), and all accumula­
            shows  must  be  mapped  relative  to  the  pod  of  active   tions  are  itemized  (Table  1 . 3).  The  critical  moment  is
            source rock. This example also shows why the distribu­  important  because  the  geometry  of  the  migration  paths
            tion  as  well  as  the  quality,  quantity,  and  thermal   and traps are reconstructed for about the time the oil and
            maturity of source rock should be mapped worldwide at   gas  accumulated.  If  the  critical  moment  is  prior  to
            the time of deposition (Klemme, Chapter 3, this volume).   present-day,  then  the  location of present-day traps  on  a
                                                              play  or prospect  map  (not shown)  can be  compared  to
            Fictitious Example #2                             the location of traps at the critical moment to determin if
                                                              oil  and  gas  have remigrated.  If  the traps  have  shifted
              The  previous  example  identified  and  mapped  the   from the critical moment to  the  present  day,  the  shifted
            geographic  and  stratigraphic  extent  of seven  petroleum   trap  or  prospect  would  have  to  be  charged  with  remi­
            systems.  The  next  example  investigates  and  describes   grated  oil  or  gas.  These  maps  can  also  be  compared  to
            one petroleum system (see Peters  and Cassa, Chapter 5,   determine if physical or  microbial  alteration  (or destruc­
            this volume).                                     tion)  occurred  during  the  preservation  time.  A  table  of
              To  demonstrate  how  the four figures  and  one  table   accumulations  for  this  petroleum  system  indicates  its
            work  together  to  characterize  a  petroleum  system,  we   size and is the basis for further calculations and compar­
            illustrate  a  petroleum  system  study  with  a  specific   isons carried out in the case studies.
            example.  Figures  1.2-1.5 and Table  1.3 depict a fictitious   Last,  a petroleum system events  chart is  constructed
            petroleum  system,  the  scrcalled  Deer-Boar(.)  petroleum   to summarie the essential elements, processes, preserva­
            system.  The  oil  accumulations  and  shows  prove  the   tion  time,  and  critical  moment  (Figure  1 . 5).  In  our  ficti­
            existence of at least one system, but if there is  more  than   tious  example,  the  description  is  as  follows.  The  Deer
            one  group  of oils, there  could  be  two  or more  systems   Shale, a Devonian (390-380 Ma)  source rock is buried by
            present.  To  identify  and  name  each  system,  oil  and   Devonian-Perrni  (380-250 Ma)  rocks  to  its  maximum
            source rock samples were collected and analyzed for  the   depth  in  the  Late  Permian  (250 Ma).  The  process  of
            following  reasons:  (1) to  establish  oil families,  (2)  to   generation-migration-accumulation  of  hydrocarbons
            determine  which  family originated  from  which  source   occur during  the Permian  (260-240  Ma),  and  the critical
            rock,  (3)  to  map the quantity and type of organic matter   moment  is  250  Ma.  These  hydrocarbons  accumulated
            in the source rock, and (4) to map the thermal maturity of   under the George Shale  (300-286  Ma)  and  in  the  Boar
            the  source rock.  On  a map, we  have shown the present­  Sandstone, reservoirs of Pennsylvanian age (315-300 Ma)
            day  location  of each oil  accumulation  attributed  to  each   that   formed   into   traps   during   the   Late
            group  (Table  1 . 3)  and  have  indicated  the  pod  of  active   Pennsylvanian-Early Permian (290-270 Ma). The preser­
            source  rock.  Much  of  this  information  is  included  in   vation time is 240 m.y. (Figures  . 3 and 1.4).
                                                                                       1
            Figures 1.3 and 1.4.                                The events  chart  can be  viewed  as  a team organiza­
               In our fictitious  example,  sufficient  information  was   tional tool.  For  example,  geologic  time  is  studied by the
            collected to identify and map the thermal maturity of the   paleontologist  and  stratigrapher,  the  reservoir by  the
            Deer Shale as the most likely source for the oil accumula­  petrophysicist  and  stratigrapher,  and  trap formation by
            tions in the Boar Sandstone (Peters and Cassa, Chapter 5,   the structural geologist and geophysicist.
            Figure 5.12, this volume).  However, because of a lack of   These  four  figures  and  table  are  simplified  to  make
            thermally  mature  samples  of  the  Deer  Formation,  an   important  points  about  a single  petroleum system  Each
            oil-source rock  correlation was  inconclusive  (see  Lewan,   figure could be drawn to include additional information
            Chapter  11, this  volume,  for  solution).  Therefore,  our   unique  to  a  particular  petroleum  system.  Once  a
            level of certainty is hypothetical because we are unable to   petroleum  system  is named, mapped, and  described,  it
            demonstrate  geochemically  that  the  oil  originated  from   can be analyzed in many ways. For example, this volume
            the  Deer  Shale.  However,  geographic  and  stratigraphic   contains  case  studies  that  describe  petroleum  migration
            evidence  is  sufficient  to  assign a  name  and  level  of   from the pod of active source rock to a trap.
            certainty-the Deer-Boar(.) petroleum system.
               At the  location  of  the  most  thermally  mature  source
            rock, a burial  history chart has  to be  made to  determine   SUMMARY
            the  critical  moment  (Figure  1 . 2). The critical  moment,  in
            this case,  is when the source  rock is at  maximum burial   Sedimentary  basins,  petroleum  systems,  plays,  and
            depth  and  is  near  the  time  when  most  hydrocarbons   prospects can be  viewed  as separate levels of petroleum
            migrated into primary traps. (If the critical moment were   investigations,  all  of  which  are  needed  to  better under-
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