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The  greatest  improvements  in  petroleum  exploration  in  the  last  several  decades  have
                  involved new seismic acquisition techniques and computer processing of digital seismic data.

                                                           Acquisition
                         The seismic method uses impulses of sound energy that are put into the earth. The energy
                  travels down through the subsurface rocks, is reflected off subsurface rock layers, and returns to
                  the surface to be recorded. Seismic exploration uses subsurface echoes to image the shape of
                  subsurface sedimentary rocks and locates petroleum traps. A source and a detector are used. The
                  source emits an impulse of sound energy either at or near the surface of the ground or at the
                  surface of the ocean. The sound energy is reflected off subsurface rock layers. The maximum
                  reflection energy occurs when the angle of incidence between the seismic source and reflector is
                  equal to the angle of reflection between the reflector and seismic detector. Only about 2 to 4% of
                  each sound impulse is reflected off each layer, and the remaining sound impulse goes further into
                  the rock, to be  reflected off deeper and deeper  layers. The reflected sound energy  from  each
                  layer returns to the surface, where the detector records it.
                         The detector on the surface records both the signal, wanted direct (primary) reflections
                  from the subsurface rock layers, and noise, unwanted energy. Noise can be caused by surface
                  traffic, wind, surface and air waves, and subsurface reflections that are not direct reflections from
                  subsurface  rock  layers.  A  high  signal/noise  ratio  is  desired.  A  noise  survey,  a  small  seismic
                  survey,  can  be  run  first  to  determine  the  nature  of  noise  in  that  area  and  plan  the  optimum
                  seismic program to reduce noise.
                         The location of the seismic source is called the shot point. On land, the common seismic
                  sources are explosives and vibroseis. Dynamite was the first seismic source used and is still the
                  most  common  explosive  source  used  today.  Explosives  are  used  today  where  the  surface  is
                  covered  with  loose  sediments,  swamps,  or  marshes.  When  using  explosives,  a  small,  truck-
                  mounted drilling rig often accompanies the seismic crew to drill a shot hole, usually 18 to 30 m
                  deep, to a point below the soil. The explosives are planted in solid rock on the bottom of the
                  hole.  Primacord, a  length of explosive  cord, can be planted  in  a trench about 0.3 m deep or
                  suspended in air as a seismic source.
                         At sea, a common seismic source is an air gun.  Other seismic sources used at sea include
                  water gun, sleeve gun, and sparker.
                         A seismic contractor  is a company that owns and operates the seismic  equipment and
                  runs the seismic survey. The seismic contractor can run the seismic survey under contract with
                  an  exploration  company.  A  spec  survey  can  also  be  run  by  a  seismic  contractor.  A  limited
                  number of exploration companies then pay for and view the nonexclusive seismic records. In
                  another method, several exploration companies share the cost and results of a seismic survey run
                  by a seismic contractor in a group shoot.
                         Before seismic exploration is run on private land a permit person must obtain permission
                  from the surface rights owners of the land. A fee per shot hole or seismic line mile is paid, and
                  damage  fees  are  negotiated.  A  survey  crew  then  cuts  a  path  through  the  trees  and  brush  (if
                  necessary), accurately locates and flags the shot points and detector locations, and records them
                  in  the  survey  log  book.  Members  of  the  seismic  crew  called  jug  hustlers  lay  the  cable  and
                  arrange and plant the geophones. At sea, permitting is not necessary. The ship’s crew does the
                  navigation while the  seismic crew runs the  seismic equipment. Surveying on  land and  at sea
                  today is done by global positioning using navigational satellites.
                         Seismic  exploration  is  most  expensive  on  land,  especially  in  rugged  terrain.  It  is  less
                  expensive and of better quality at sea.

                         Task 3. Answer the following questions, using the vocabulary from Task 1.
                       1.  What is geophysics?
                       2.  What kind of surface methods do geophysicists usually use to explore the subsurface?
                       3.  Which of the methods is the most useful and advanced?
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