Page 14 - The Petroleum System From Source to Trap
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6     Magoon and Dow

          Sedimentary Basin Investigations                  tectonic  process,  such  as  rifting,  as a  basin.  On inter­
                                                            preting a seismic profile, a geophysicist refers to a thick
            Over  the last several  decades,  investigations of sedi­  package  (measured  in  two-way  time) of sedimentary
          mentary basins have emphasized plate tectonics or struc­  rocks as a  basin.  Geologists  frequently  use  the  term
          tural evolution.  Basin classification  schemes  evolved   geographically, that  is,  to name  and locate a  province,
          from  descriptive geology  (Weeks,  1952;  Knebel  and   such as the Williston basin,  which  is separate from  the
          Rodriguez-Eraso,  1956)  to  genetic  interpretations   genetic use of basin to  mean any  sedimentary basin. In
          (Halbouty et al.,  1970a,b;  Klemme,  197la,b,  1975,  1986;   some cases, the water column is implied as the basin, in
          Bally,  1975;  Huff,  1978,  1980;  Bally and Snelson,  1980;   others the sedimentary rock contents are the basin, and
          Bois et al., 1982; Kingston et al., 1983a) with the advent of   in yet others, the  container  is the  basin. None of these
          plate  tectonics theory. With  increased understanding  of   meanings is incorrect, and specialists from different disci­
          organic geochemistry, work on the occurrence of oil and   plines  are  usually  aware  that basin  has more  than one
          gas  also  has  gone  from  the  descriptive  (Weeks, 1952;   meaning.
          Knebel and Rodriguez-Eraso,  1956)  to  the deterministic   For this volume, the sedimentary basin  is a  depression
          (Tissot, 1969; Tissot and Pelet,  1971; Zieglar and Spotts,   filled with sedimentary rocks. The depression, formed by
          1978; Welte and Yukler, 1981;  Demaison, 1984; Ungerer   any  tectonic  process,  is lined by basement rock,  which
          et al., 1984; Tissot et al., 1987).               can be igneous, metamorphic, and/ or sedimentary rock.
            Each  new approach  to  the  analysis  of  petroliferous   The basin  includes the rock matter, organic matter,  and
          sedimentary basins becomes more focused on  the   water deposited in this depression. In certain cases, such
          genesis of petroleum. Bally (1975) pointed out that sedi­  as with coal and some carbonate deposits,  the sedimen­
          mentary basin type  does little to  improve  our ability  to   tary material is formed in situ. Basin used by itself refers
          forecast the volume of petroleum  from  a particular type   to the sedimentary basin.
          of basin. However, as more petroleum geochemistry is   The term  basin  used with a  proper noun refers  to  a
          incorporated into the analysis of a sedimentary basin, the   petroleum province,  such  as  the Williston basin.
          success ratio goes up (Demaison,  1984) and  the forecast   Sometimes basin is capitalized, such as in the Green
          of petroleum occurrence becomes more certain (Tissot et   River Basin, when  it  is a proper geographic name that
          al., 1987).                                       usually  refers to  the  present-day  river drainage. A
            When sedimentary basins  with  uncomp i cated   petroleum province  is  sometimes referred  to  as  a
                                                 l
          geologic histories are studied, a basin analysis approach   petroleum  basin,  which  is  different  from a  petroleum
          that  promotes  organic g e ochemistry  works  well.   system.
          However,  when similar studies are  carried out  in fold   A sedimentary basin analysis investigates, in a myriad
          and thrust belts (such as in Wyoming, U.S.A.), in areas of   of  ways, the  formation  and contents of this  depression.
          complex geology  (such  as  the Basin and Range  of   Structural and stratigraphic studies are the most conven­
          Nevada and Utah, U.S.A), or in areas of uncommon heat   tional way to  study  a  sedimentary basin.  More  recent
          source (such as in the mid-Pacific Ridge) (K venvolden et   techniques  include seismic stratigraphy  and sequence
          al., 1988), basin analysis techniques are more difficult to   stratigraphy. Sequence stratigraphy, for example, can be
          apply because the original sedimentary basin is severely   used to  understand the  distribution of sandstone and
          deformed or incomplete.  In fact, for maps that show oil   shale  in a  particular area as a package of  related sedi­
          and gas fields and basin outlines together, the petroleum   mentary rock. For the petroleum  geologist,  in certain
          accumulations occur  within the basin outline as often as   areas the reservoir properties of  this sandstone  can be
          they occur on  the  adjacent  highs or  arches that are   mapped as well as the organic facies of the shale. Sedi­
          outside the basin outline (Vissides  and Quirin,  1964;   mentary  basin  analysis  includes  all  aspects  of basin
          Wilkerson and Reed,  1982). Oil and gas  fields usually   formation and the basin fill up to the  time petroleum is
          (but not  always)  occur in  sedimentary  rocks,  but  not   generated, at  which  time a  petroleum system investiga­
          necessarily within the boundary of basins. Therefore,  to   tion  is  required.  Because  petroleum is  mobile,  fragile,
          understand  the occurrence  of these accumulations,  at   and responds to  different physiochemical parameters
          least two items need clarification. First, a working defini­  than does basin fill, this second type of investigation, the
          tion  is needed for the  sedimentary basin  and  what is   petroleum system, is needed.
          being investigated, and second, a different type of inves­
          tigation  is  needed  that is separate from basin analysis   Petroleum System Investigations
          and deals only with oil and gas.
            First,  the  term basin  has different implications  to   Each  investigative procedure has an appropriate
          different  specialties.  A  paleontologist uses  the  term in   starting  point. For the  prospect  analysis, the starting
          reference to where in the water column fossils live, such   point is the trap, for the play, a series of traps, and for a
          as benthic or planktonic. A petroleum geochemist visual­  basin analysis, a tectonic setting and sedimentary rocks.
          izes the most anoxic part of  a paleoocean or continental   Similarly,  the  investigative  procedure for  the petroleum
          basin  where  organic  matter accumulates and  refers  to   system  starts  with  discovered hydrocarbon accumula­
          that as the basin.  Carbonate  and siliciclastic stratigra­  tions, regardless of size. Because of this, shows or traces
          phers refer to  the  sedimentary fill  that was deposited   of  oil  and  gas  take on  new importance.  Petroleum
          sometime in the  past as the basin. Structural geologists   geochemical analysis of  oil and gas traces can provide
          refer  to  the  container  that  is created in  response  to  a   critical  information  as to the  nature  of the responsible
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