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leum exploration has revealed 432 reefs of  which  139 are gas-filled, 221 are
            oil-filled, and  72  are  barren.  The  cap  rock  is evaporite. Figure 9-19 shows
            that the reef  belt  consists of  a downdip gas zone, an intermediate oil zone,
            and  an  updip water  zone.  Figures  9-20 and  9-21 show the cross-sections.
            The Lockport Formation  is the common porous and permeable  base to the
            reefs, and Gill (1979, p. 618) considered that the Cain Formation, overlying
            the  Lockport  between  the reefs  and  downdip,  is the source rock. The oil
            gravity increases up-dip from 65'  to 43'  API (s.g., 0.72-0.81).
              We  shall consider these and other reefs in more detail in Chapter 12.
              The  same processes could, of  course, operate in a sequence of  sandstone
           traps; but those in carbonates are clear.



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