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Natural Gas Reservoirs
                  Natural gas, being less dense than either oil or water, tends
           to float above water and oil in the subsurface.
                  Sometimes,  the  natural  gas  is  dissolved  in  the  oil,  but  it
           very often forms a separate layer of its own which floats above the
           oil layer. In such a case, we get a layer of natural gas floating upon
           a layer of oil which is in turn underlain by a layer of water.

                  Geologic Structures Become Hydrocarbon Traps
                  Common sense suggests that these sedimentary layers will
           tend to be laid down more or less horizontally over large areas. We
           also kno w, however, that we need traps to provide areas in which
           oil and gas can collect. This  means that the  layers of rock must
           somehow  become  buckled  and  bent  to  provide  the  geologic
           structures that may become traps. Fortunately for oil prospectors,
           forces within the earth itself create these geologic structures. These
           powerful forces that tend to stretch, squeeze, bend and break the
           rock  layers  are  the  same  forces  that  cause  earthquakes.  The
           geologic structures that are created (ie. bends and breaks or faults
           in  the  rock  layers)  can  become  hydrocarbon  traps  where  certain
           conditions are present:
                  1)  There  must  be  hydrocarbon  source  rock  in  the  area.
           Source rock is the fine grained rock in which the organic material
           originally present has been converted into hydrocarbons.
                  2)  There  must  be  a  porous  and  permeable  rock  layer  to
           provide a reservoir in which the hydrocarbons can accumulate.
                  3) There  must  be an  impermeable  sealing rock  overlying
           the reservoir rock to trap the hydrocarbons.
                  Figure 6 shows some examples of geologic structures that
           commonly  form  hydrocarbon  traps.  Note  that  there  are  both
           structural  traps  and  stratigraphic  traps.  Stratigraphic  traps  are
           traps that are formed by changes in the characteristics of the rock
           formation such as a loss of permeability or porosity or a break in
           continuity of a layer. Structural traps on the other hand are caused
           by  the  bending  or  breaking  of  the  sedimentary  layer.  The  most
           common and simplest type of structural trap is the anticline which




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