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124    Morse



              A
                         Simple
                         Dune                  PREVAILING
                                             WINDS
                                        /                     8
                         Interdune
                         Simple
                         Dune
                         Interdune
              r          Simple
             1 - 40m     Dune
              j_






                                                                                           0- 1 50m




                                                                                          1 00- 7 00m

                          " D  OWNWIND"  DEPOSITIONAL
                               ENVIRONMENTS
                                                                                          0- 1 00m



           Figure 6.2. (A) Simple dune packages of fine to medium sand are composed of translatent strata (t) formed by migrating wind
          ripples with grain flow or avalanche strata (a) and/or grain fall strata (f). Interdune sands are formed largely by translatent
           strata (t). (B) Eolian depositional block diagram of a migrating erg system with (1) an idealized vertical facies sequence of
          fore-erg, central-erg, and back-erg facies divisions based on types and scale of eolian strata and the nature of intra- and
           extradunal facies (after Porter, 1986).

           braided  rivers,  then  meandering  rivers.  The  fluvial   giant  and  supergiant  fluvial  reservoir  fields  (Table  6.1).
           system  commonly  ends  at a  lake  or  at the sea  where  it   These  sands are  thicker  than  meandering  river  deposits
           may form a delta.                                and  typically occur in structural traps because  they lack
             Fluvial reservoirs  consist  of clean  (lack silt and clay),   the  lateral  seals  required  for  stratigraphic  traps.
           poorly  sorted,  boulder  to  fine-grained  sand  porous   Depending on the curvature or size of the meander loops
           bodies.  Thick,  stacked braided stream deposits  form   and  the  thickness  of the  point  bar  sands,  meandering
           widespread  reservoirs  that  are  more  common  in the   river deposits form  "shoe-string sands"  that in an updip

           Table 6.2.  Eolian Reservoirs

                                                                           Pay           Depositional
           Field              Location          Agea        Formation   Thickness (m)    Environment
           Gronigen          Netherlands       L Perm      Rotliegendes               Eolian with fluvial
                              and Germany                                              intradunal strata
           Viking            United            L Perm      Leman Ss        244        Eolian with sabkha and
                              Kingdom                                                   alluvial interbeds
           Urucu             Brazil                        C ltaituba                 Eolian
           Rangely           U.S.A. (Colorado)   L Perm    Weber Ss                   Eolian with fluvial
                                                                                        interbeds
           Mary Ann          U.S.A. (Alabama)   J          Norphlet Ss     240        Eolian
           Elk Basin         U.S.A. (Wyoming)   Penn       Tensleep Ss                Transverse and oblique
                                                                                        dunes
           Painter Reservoir   U.S.A. (Wyoming)   L J      Nugget Ss       260        Eolian
           aL, lower, Penn, Pennsylvanian; Perm, Permian; J, Jurassic.
           bA, antidine: 81. Med block; St. stratigraphic; WrA. wrench antidine; Th, thrust anticline.
           cv, vertical; Lt, lateral.
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