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             CJ  Presence of  Upper Jurassic                      •    •
                  zone of mature  Upper  Jurassic  source  rock  {related to  production
             - or  accumulations)
              �  Positive  areas  (nondeposition  or erosion)
                                                               Figure 3.1. Australasia Upper Jurassic deposition areas,
             ' Rift  with  Upper Jurassic  deposition (orpostdepositional  ritting)
                                                               petroleum systems, and Lower-Middle Jurassic source
             .......  _   Orogenic  "CutOff"  Zone,  behind which any  Upper Jurassic  is  m-ost   facies (eastern Gondwana sector). Circled numbers are
              �  often  met  a  mar phased,  int ruded,o r  destroyed   keyed to Tables 3.1 ahd 3.2. Symbols: X, producing area
                                                               with a Lower-Middle Jurassic source; T, Tethyan facies;
             '  Craton  edge of Upper Jurassic
                                                               subscripts with Tethyan facies: C, carbonate and shales;
                  Upper  Jurassic  volcanics   f]!S� Upper  Jurassic  paleolatitude
             •..                                               E, evaporites; -, <40" paleolatitude; +, >40" paleolatitude .
               . . .
               @)   Petroleum  System      @  Minor  Accumulation   H, Humic facies (clastics); subscripts with Humic facies:
                                                               C, coaly; L, lacustrine, -, <40" paleolatitude; +, >40'
                         �  Major  lakes  & dra in a ge
                                                               paleolatitude.
             of the world where there is a lack of stratigraphic names,   identified  in  this  chapter.  This  occurs  because  the  case
             requiring that the age of the rock units be used for source   studies  usually  include  sufficient  information  to map  a
             and  reservoir;  (2)  petroleum  systems  so  large  and   pod of active source rock, whereas the systems identified
             extensive  that several  stratigraphic names have  been   in  this  chapter  rely  more  on  regional geology.  It  is
             applied to  the same source rock; and  (3) many Upper   apparent that as more attention is given to mapping each
             Jurassic  systems  where  a  great  deal  of  upward   pod  of active  source  rock and  its related  hydrocarbons,
             petroleum  leakage  occurred  so that  many  (multiple)   the  25  petroleum  systems  described  here  will  probably
             reservoirs, rather than  one main reservoir, contain the   increase in number. However, as global as this approach
             bulk of the accumulated petroleum.                may be, it demonstrates  the  usefulness  of identifyg all
               The global scale of this study requires that petroleum   those  petroleum  systems  in  the  world  that  include  one
             systems be lumped for brevity of discussion and because   source rock interval.
             of the lack of detailed information (see uncited references   Estimates  of  the  key  factors  used  to  derive  a
             by petroleum system at end of chapter). This is apparent   petroleum system's recovery efficiency include (1) source
             in that  certain petroleum system case studies included in   rock area  and  thickness,  total  organic  carbon  (TOC),
             this volume that involve Upper Jurassic source rocks do   hydrogen  index  (HI),  density,  and  kerogen  type;  (2)
             not necessarily  correspond  to  the  petroleum  systems   present  discovered  barrels  of  oil  equivalent  recoverable
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