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porous rock has “porosity”. Reservoir rocks must be porous, because
                           hydrocarbons can occur only in pores.
                                  A  reservoir  rock  is  also  permeable  –  that  is,  its  pores  are
                           connected. If hydrocarbons are in the pores of a rock, they must be
                           able to move out of them. Unless hydrocarbons can move from pore to
                           pore,  they  remain  locked  in  place,  unable  to  flow  into  a  well.  A
                           suitable  reservoir  rock  must  therefore  be  porous,  permeable,  and
                           contain enough hydrocarbons to make it economically feasible for the
                           operating company to drill for and produce them.

                           Origin and Accumulation of Oil and Gas
                                  To  understand  how  hydrocarbons  get  into  buried  rocks,
                           visualize  an  ancient  sea  teeming  with  vast  numbers  of  living
                           organisms. Some are fishes and other large swimming beasts; others,
                           however,  are  so  small  that  you  cannot  see  them  without  a  strong
                           magnifying glass or a microscope. Although they are small, they are
                           very abundant. Millions and millions of them live and die daily. It is
                           these tiny and plentiful organisms that  many  scientists  believe gave
                           rise to oil and gas.
                                  When  these  tiny  organisms  died  millions  of  years  ago, their
                           remains  settled  to  the  bottom.  Though  very  small,  as  thousands  of
                           years  went  by,  enormous  quantities  of  this  organic  sediment
                           accumulated  in  thick  deposits  on the  seafloor.  The  organic  material
                           mixed with the mud and sand on the bottom. Ultimately, many layers
                           of sediments built up until they became hundreds or thousands of feet
                           (metres)  thick.  The  tremendous  weight  of  the  overlying  sediments
                           created  a  great  pressure  and  heat  on  the  deep  layers.  The  heat  and
                           pressure changed the deep  layers  into rock. At the  same time,  heat,
                           pressure,  and  other  forces  changed  the  dead  organic  material  in  the
                           layers into hydrocarbons: crude oil and natural gas.
                                  Meanwhile, geological action created cracks, or faults, in the
                           earth’s  crust.  Earth  movement  folded  layers  of  rock  upward  and
                           downward.  Molten  rock  thrusted  upward,  altering  the  shape  of  the


















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