Page 58 - The Petroleum System From Source to Trap
P. 58

Magoon, L. B, and  W. G. Dow,  eds.,  1994, The petroleum
                                                                   system-from source to trap:  AAPG Memoir 60.




                                                                                       Chapter  3



                       Petroleum  Systems of the World

                       Involving Upper Jurassic  Source  Rocks


                       H. Douglas Klemme
                       Bo11dvi/lc, Vcrmo11l, U.S.A.

                                                                                           Abstract

                   Fourteen "mega" petroleum systems with Upper Jurassic source rocks contain one-fourth of the
                 world's discovered petroleum. These petroleum systems, their locations in space and time, and their
                 petroleum  plumbing  ingredients  are  reviewed,  descrbed, and  tabulated.  Each system's  recovery
                 efficiency is estimated. Plumbing ingredients are related to the relative magnitude of the petroleum
                 system's estimated  recovery  efficency.  While the presence  of a  source  rock is  a  requirement  of all
                 petroleum  systems-with  source  rock  abundance  and  character  of  considerable influence  on
                 recovery  efficiency--other  plumbing  ingredients are capable of  even  more influence  on  the
                 magnitude of the systrne's recovery efficiency. These other plumbing factors include the quality and
                 quantity (extent) of reservoir and cap rock, trap evolution and size, and the dynamics and timing of
                 these factors along  with source  rock maturation and  migration. The character,  quality, and  quantity
                 of these petroleum  systems' plumbing are  related  to  their plate tectonic  location,  palelatitudinal
                 realms, and the structural (tectonostratigraphic) evolution of the basin or province.


           INTRODUCTION                                      updip zero edge from either nondeposition or truncation
           Fourteen petroleum  systems  with  Upper Jurassic   of  Upper  Jurassic  sedimentary  rocks along  the  craton
        source  rocks contain  one-fourth  of the  world's  discov­  margins,  (2)  positive areas  of  either  nondeposition  or
        ered petroleum. Eleven other  systems  with  Lower  and   truncation  within  the  Upper Jurassic depositional  trend,
        Middle Jurassic source  rocks presently have a minor but   and  (3) an  orogenic  cut-off  zone  behind  which  any
        significant  amount  of  discovered  petroleum.  These   Upper  Jurassic  sedimentary rocks have usually been
        petroleum  systems are  g.eologically  reviewed,  their   destroyed  by  orogenic  metamorphism,  intrusion,  or
        location in space and time is described and mapped on a   truncation associated with Phanerozoic terrane accretion.
        continental  scale,  their  relative  petroleum  system   The  latter  is  often  considered  a  zone  of  petroleum
        recovery  efficiencies  are  estimated, and the  effect  their   economic  basement,  although  notable  exceptions  occur
        essential  elements  and  processes  have  on  their   where  the Jurassic  source  rock  is  preserved  in  these
        "petroleum plumbing"  is  outlined.  In addition,  their   zones (see Cook Inlet and Vienna basin).
        petroleum dynamics are discussed.                      Tables  3.1 and  3.2 attempt  to  organize the petroleum
           The  information  used  to  identify  and  map  these   plumbing  ingredients,  including  source  rock,  reservoir
        Jurassic petroleum systems come from many references,   rock, cap (seal rock), trap type, and dynamic characteris­
        the  more  important  ones  being  Bedoes  (1973),  Beydoun   tics,  together  with an  estimate  of  the  recovery efficiency
        and  Dunnington  (1975),  Jones  (1975),  Weeks  (1975),   for  the  petroleum  systems  that  involve  Upper Jurassic
        Nehring (1978, 1981), Kanstler et al. (1984), Carmolt and   source  rocks.  An  events  chart  for  each  of  the  14
        St. John (1986), Masters et al.  (1987,  1991), Ziegler (1988),   petroleum  systems  outlines  the  timing  of  essential
        Creaney  and  Allan  (1990),  Hubbard  et al.  (1990),  and   elements and processes  in relation  to the timing  of  the
        Zappaterra (1990).                                   system's plumbing dynamics (Figure  3.6).  The timing of
           In  mapping  the  world's  petroleum  systems  that   the initial development  of  a given trap  was found  to be
        involve  Upper Jurassic  source  rocks,  continental  maps   variable  dependent  on  the  type  of  trap  being  formed.
        (not  including  Antarctica)  with  currently accepted   Different trap types and different ages and lithologies of
        Upper Jurassic paleolatitudes were used as a base. Three   reservoir rocks are the departure point for the division of
        "cut-off"  margins or limits to those Upper Jurassic sedi­  petroleum systems into plays and prospects.
        mentary  rocks  that  include  source  rocks  generally   Difficulty  in  naming  Upper Jurassic  petroleum
        considered available for potential petroleum systems are   systems by using major source rocks and reservoir rocks
        outlined  (Figures  3.1-3.5).  These  cut-offs include  (1)  the   was  encountered  in  the following  situations:  (1)  regions

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