Page 81 - The Petroleum System From Source to Trap
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Magoon, L. B, and  W.  G.  Dnw, eds.,  1 '1'1-!, The petroleum
                                                                    system-from source to trap:  AAPG :'l.lemoir 60.




                                                                                       Chapter  4



                        Genetic  Classification  of Petroleum

                        Systems Using Three Factors:

                        Charge,  Migration,  and  Entrapment


                       Gerard Demaison                        Bradley J. Huizinga
                       Capitola, Cahfomia, U.S.A.             ARCO Intcmatimwl Oil and Gas Co.
                                                              Plano,  Texas, U.S.A.


                                                                                            Abstract
                    Our genetic  classification  of petroleum systems  is founded  on a  simple working  nomenclature
                  that consists  of combining qualiers  from each  of the  following  three  categories:  (1) charge  factor
                  (supercharged,  normally  charged,  or undercharged),  (2)  migration  drainage  style  (vertically
                  drained or laterally drained), and (3) entrapment style (high impedance or low impedance).
                    The  charge  factor  is estimated  using the initial  richness  of  the  source  rock and the volume  of
                  mature source rock. The source potential index (SPI), which combines source rock richness and net
                  source rock thickness into a single parameter, is a convenient shortcut for comparing the petroleum
                  potential  of diverse  source  rocks  containg  dissimilar  kerogen  types  and  for  rapidly  estimating
                  regional  charging  capacity.  In  extensively  explored  petroleum  provinces  that  contain  a  single
                  petroleum  system,  a  positive  correlation exists between  the  magnitude  of  the  SPI and  province­
                  wide petroleum reseres.
                    Migration  drainage style is detennined  from  the structural  and stratigraphic  framework  of the
                  basin fill. Vertical migration drainage, which occurs mainly through faults and fractures that breach
                  a seal,  is characteristic of petroleum systems  in  rift basins,  deltaic sequences,  salt  dome provinces,
                  wrench  basins,  and  fold  and  thrust belts.  In  contrast,  lateral  migration  drainage  is  dominant
                  wherever stratigraphically continuous seal-reservoir  "doublets"  or carrier beds extend over a large
                  area in a tectonically stable  province  (e.g., foreland or intracratonic platform basins). Recogtion of
                  the  dominant migration  style  helps  to  predict  the  location  of zones  of petroleum  occurrence  in
                  relation to the pOd of mature source rock.
                    Entrapment  style,  which  is also dependent  on  the  structural  framework  and  the  presence  and
                 effectiveness of seals, describes the degree of resistance  (impedance)  working against dispersion  of
                  the  petroleum charge.  Application of these  working  concepts should help to  reduce  geologic  risk
                  significantly, particularly in new ventures exploration.


         INTRODUCTION                                         (Klemme,  1975,  1980,  1983; Bois et  al., 1982; Carrnalt and
                                                             St. John, 1 9 86). Also, field size distributions in petroleum
           During the past 40  years,  several  tectonic  classifica­  basins generally show some relationship to basin classifi­
         tions  of sedimentary  basins  have  been  developed  by   cation  and  basin  size  (Klemme,  1 9 83).  Furthermore,
         petroleum  geologists  to  provide  a  common  framework   recognition  of tectonic style  helps to  predict regional
         of  reference  for  the  earth's  sedimentary  basins  (e.g.,   retention efficiency  (e.g., in the evaluation of thrust belts;
         Weeks,  1952;  Perrodon,  1972;  Klemme,  1975,  1980,  1983;   Vann,  1 9 89)  or  abnormally  high  heat  flow  regimes
         Bally  and  Snelson,  1980;  Kingston  et  al.,  1983;  Helwig,   affecting  source  rock maturation  and  oil  preservation
         1985). These classifications have been developed with the   (e.g.,  in  proto-oceanic  rifts  such as  the  Red  Sea or  Afar
         purpose  of  finding  relationships  between  tectonic  style   triangle).
         and  petroleum occurrence.  The  most  useful  outcome  of   Nevertheless,  any  degree  of  petroleum  richness,
         these  studies  has been  to  demonstrate  the  statistical   ranging from  near  barren  to  highly prolific, can be
         predominance  of giant  fields  and  major  petroleum   observed  among  specific  examples  of each  basin  type.
         reserves  in cratonic sags and foredeep basins, in contrast   Bally  and Snelson (1980,  p.  71)  recognized  this  point  by
         to  lesser  reserves  in  pull-apart  and  thrust-belt  settings   concluding  that  "the classification of basins does  little to

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