Page 284 - Modern Spatiotemporal Geostatistics
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        A CALL NOT TO ARMS, BUT TO RESEARCH


          "What  an interior strength  a  man  can summon if  he devotes  himself
              entirely  to knowledge and creation, rather  than to a vain search



                for  honors and  celebrity!  What  a  lesson!" B . Russell for G. Frege
        Unification     and    Distinction

        A  careful  study  of  the  developments  in  geostatistics  reveals  that  the  latter
        continuously  undergoes two  major  processes of  growth  and advancement:
          1.  A  unification  process with  respect to  its  methods.
         2.  A  distinction  process with  respect to  its  mathematical  structure  and the
            way  it  relates to  experience.
        These  two  processes  may seem  to  follow  opposite  paths,  but  in  essence  they
        complement  each  other,  and are equally important for  the  growth of the  field.
            As  the  methods  of  modern  spatiotemporal  geostatistics  lay  claim  to
        broader  domains  of  space/time  data  analysis, they  also  become  increasingly
        unified.  For  example,  as  we  saw  in  Chapter  12,  generalized  random  fields
        unite  previously  separate  classes  of  fractal  and  wavelet  random  fields;  also,
        BME  mapping incorporates the interpolation  methods  of traditional geostatis-
        tics  and  spatial  statistics  as special  cases.  At  the  basis of  the  unified  frame-
        work  lies a physical geometry  in which  space and time constitute an  integrated
        whole.  The  choice of  an appropriate geometry  depends on the  local  properties
        of  space/time  and on the  physical constraints  imposed  by the  phenomenon of
        interest  (Chapter  2).  Within the unified framework, useful classifications of the
        geostatistical techniques  are possible, which depend on the  physical  knowledge
        sources  processed, the  information  functions  assumed, the  conditionalization
        rules  used, etc.  (Chapters  3-8).
            Considered  as a  theory  of  physical  model-based estimation,  geostatisti-
        cal  mapping  has two  distinct  parts:  a formal  part  and  an  interpretive  part.

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