Page 167 - The Petroleum System From Source to Trap
P. 167

Magoon, L. B, and W. G.  Dow, eds.,  1 994, The petroleum
                                                                      system-from source to trap:  AAPG Memoir 60.




                                                                                            Chapter  8


                    � H drocarbon  Seal  Rocks
                             y


                          Madan  W. Downey
                          President, ARCO lntemational Oil [-r Gas
                          Plano, Texas, U.S.A.


                                                                                           ABSTRACf
                       The geographic extent of a petroleum system  is defined  by the observed occurrences of geneti­
                    cally  related  hydrocabons  that  emanated  from  a  given  pod of mature  source rock.  These  related
                    hydrocn occurrences and associted migration routes,  in turn, are confined  and limited by the
                    presece of sealg surfaces. Where confing  seal are lacking, hydrocns escape to the surface.
                    Therefore, the seal rock is an essential element of the petrleum system.
                       In  the  petroleum  system,  there  are  two  important  classes  of seals:  regional seals  that  roof
                    migrating  hydrocarbons  and  local seal  that  confine  accumulations.  Major  roofing  seal  act to
                    confine migrating hydrocns to particular stratigraphic units. Any lithology can serve as a seal
                    for a hydrocn accumulation. The only requirement is that minium displacement pressure of
                    the lithologic unit comprising  the sealg  surface be greater than the  buoyancy  pressure of the
                    hydrocarbon  column  in  the  accumulation.  In  practice,  however, the overwhelming  majority  of
                    effective seal rocks are evaporites, fine-grained clastics, and organic-rich rocks. These lithologies are
                    commonly  evaluated  as seal because they  have  high  entry pressures,  are laterally  continuous,
                    maintain uniformity of lithology over large area, and are relatively ductile.
                       Regional evaluation of the exploration potential of an area should start with (1) determition of
                    stratigraphic  position  and  area distribution of thermaly mature  sour rocks,  (2)  identification  of
                    the regional seal for migrating hydrocns, (3) an analysis of trapping conditions focus on the
                    areas under the regional seal and updip from the thermally mature source rocks, and (4) an exami­
                    nation of the distribution of hydrocn shows and production.


                                                                1988).  Most quantitative seal data  derive  from  studies of
           INTRODUCfiON
                                                                seals roofing local accumulations, but such  field  data are
              The  geographic  extent  of  a  petroleum  system  is   related  only  inferentially  to  the general  properties  of  the
           defined  by  the  observed  occurrences  of genetically   regional  seals  that  must  roof  and  guide  the  migrating
            related  hydrocarbons that emanated from a given pod  of   hydrocarbons in the petroleum system.
            mature  source  rock.  These  related  hydrocarbon  occur­  In  a  petroleum  system  investigation,  seal  analysis
            rences  and  associated  migration  routes,  in  turn,  are   should  start  with a  determination  of  the  time  and  place
           confined and limited by  the presence of sealing surfaces.   where  hydrocarbons  are  generated  and  expelled.  Many
           A seal rock can be defined as one that has pore throats too   stratigraphic  horizons  display  properties  of a  seal,  but
           small  and  poorly  connected  to  allow  the  passage  of   only  those  few  that are  above  the  mature source  rock(s),
           hydrocarbons.  The  geographic  extent  of  seal  rocks   are  regionally  extensive,  and  have  a  seal-transmission
           defines  the  effective  limits  of the  petroleum  system.   (reservoir  rock)  couplet  are  important  to  a  particular
           Where  confining  seals  are  lacking,  hydrocarbons  escape   petroleum  system.  Making  maps,  cross sections,  and
           to  the  surface.  Therefore,  the  seal  rock  is  an  essential   measurements  of  all  possible  sealing  rocks  in  a
           element of the petroleum system.                     petroleum  province  would  be  an  inefficient  and  time­
              Many stratigraphic  horizons have properties of a seal;   consuming way to understand the distribution of hydro­
           it  is  important  to  identify  those  that  define  the  hydro­  carbons in a petroleum system.
           carbon migration and accumulation system at the critical   Understanding  seals  that  are  part  of a  petroleum
            moment.  All other  seals  are  irrelevant  to  the  petroleum   system  involves  focusing  on  just  those  impermeable
           system.                                              surfaces  that  control  migration  and  accumulation  of
              Two  important  classes  of seals  occur  in  a  petroleum   genetically related hydrocarbon pools. Maps of the distri­
           system:  regional  seals  that  roof migrating  hydrocarbons   bution, character, and structural attitude of regional seals
            and  local  seals  that  confine  accumulations  (Ulmishek,   are  important  in  understanding  the  petroleum  system.

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