Page 106 - Petroleum Geology
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             sentially because of a restraint on further migration that is due to stratigraphic
             causes. Of the many possibilities, the two most important are organic reefs
             enclosed  above  by  mudstones,  and  unconformities  where  the  subcrop  of
             the  permeable  formations  is  sealed  by  mudstone  on  the  unconformity.
             Some  very  large  fields are palaeogeomorphic traps, where transgression has
             led  to  porous  and  permeable  beds  against  a  contemporary  topographic
             feature that was covered by  mudstone as the transgression proceeded. Wed-
             ging,  lensing, and  convergence  of  rock  units  also  cause stratigraphic traps.
               In practice it is not always possible to assign an accumulation exclusively
             to a single class of  trap.  Many anticlinal traps are faulted, and are classed as
             structural  traps. Most unconformity  traps are also faulted, some also folded.
             Organic reefs  and  palaeogeomorphic  traps  are usually not folded, but may
             be faulted, and they are usually purely stratigraphic traps.



             GEOPHYSICS

              It  is  not my purpose here to review the role of  geophysics in petroleum
            geology,  but  rather  to pick out some salient points  to illustrate the impor-
            tance of the topic in petroleum geology.
               Geophysics is  the  study  of  the  physical properties  of  the Earth and the
            study of the Earth through  its physical properties.  It is concerned with the
            distribution  of matter in and around the earth, particularly that within the
            Earth to depths to 10 km or so. It is concerned with the force of gravity and
            its variation from place to place; the strength and direction of the magnetic
            field and their variations from place to place; the occurrence of earthquakes
            and the transmission  of  their energy, and the propagation of artificially gen-
            erated elastic (seismic) waves through the earth.
              As  applied  to  economic  geology,  geophysics  consists  of  measuring the
            physical properties of  the rocks beneath  an area (gravity, magnetism, radio-
            activity) and  measuring  the  response  of  the  rocks  to artificially  generated
            energy fields (seismic, electric or electro-magnetic). The scale of such investi-
            gations varies from the global to the very local (such as the measurement of
            the velocity of  sound in the wall of a borehole). The application of geophys-
            ical  techniques  to the  search  for petroleum  has not only been of  immense
            importance to the petroleum industry, it has also provided an important stim-
            ulus  to  the  broader  development  of  the  science  of  geophysics.  It  is  the
            practical  application,  largely,  that  has  kept  geophysics  closely  related  to
            geology.
              Although  many  of  tne  early regional exploratory surveys were based on
            magnetic and gravity methods, and gravity surveys were used  to detect salt
            domes and  other structures, their importance in  petroleum  exploration  has
            declined.  The  enormous  improvements  in  seismic technology  since  1960,
            largely due to improvements in computer technology, in turn, often stimulated
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