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            oillwater contacts on the two flanks of  some oil fields differ by as muchas
            150 m.
              The effective drainage areas of  wells in carbonate reservoirs with fracture
            porosity are large, and productivity of wells is usually large. These are impor-
            tant factors in the economics  of oil production because the oil can be produced
            with  relatively  few  wells.  High productivity  is one of the characteristics of
            carbonate reservoirs, including reef reservoirs. Intisar field, Libya, for example,
            tested  one  well  at 74,867  bbl/day  (11,900 m3/day) clean 37'  API oil (sp.
            gr., 0.84) from 223 m (731 ft) of fossil reef (World Oil, January 1968).
              As regards irreducible  water saturations,  less is known of carbonate reser-
            voirs than of sandstone reservoirs, and some carbonate reservoirs are thought
            to be oil-wet. It seems certain, however, that oil and gas will come into close
            contact with solid carbonate surfaces in the reservoir. In reservoirs with frac-
            ture  porosity,  the  irreducible  water  saturation  is  probably  very low in the
            fractures, but may be high in the rock itself.
              Of  particular importance in carbonate provinces is the evidence for differ-
            ential entrapment of  oil and gas.  GUSSOW'S (1954) hypothesis of differential
            entrapment is very simple, and it grew from the observation that in a sequence
            of reefs in a single trend in the Western Canada basin, the deepest reefs con-
            tain gas only; the shallowest, water only; there will be one deep reef with a
            gas/oil contact, and one shallow one with an oil/water contact, but the others
            will be full to spill point. Gussow explained this characteristic distribution as
            follows:
              Starting with saturated oil (that is, oil that contains the maximum amount
            of dissolved gas) migrating updip (Fig. 9-18), gas comes out of solution as it
            moves to lower pressures and temperatures. At the first trap encountered on
            its migration path, both oil and gas accumulate; but as the trap fills, a gas cap
            forms by gravity segregation, so when the trap is full, only oil spills out and
            continues its migration.  However, gas can still enter the first trap, displacing
            oil  until  the trap is filled with gas only, and filled to the spill point. When
            this stage is reached, both oil and gas bypass the first trap, and the process is
















            Fig.  9-18, Differential entrapment of  oil and gas in traps that are hydraulically connected
            (Gussow's principle).
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