Page 148 - Statistics and Data Analysis in Geology
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In previous chapters we have considered the analysis of data consisting of only
              a single variable measured on each specimen or observational unit.  In Chapters 4
              and 5 we also considered the influence of the temporal or geographic coordinates of
              the sample points. We will now examine techniques for the analysis of multivariate
              data, in which each observational unit is characterized by several variables. Multi-
             variate methods allow us to consider changes in several properties simultaneously.
              Examples of  data appropriate for multivariate analysis abound in geology.  They
              include chemical analyses, where the variables may be percentage compositions
              or parts per million of  trace elements; measures on streams, such as discharge,
              suspended  sediment load, depth, dissolved solids, pH, and oxygen content; and
              paleontologic variables, perhaps a large number of  measurements made on speci-
              mens of  an organism. Dozens of  other examples quickly spring to mind. Some are
              simple extensions of  problems we have considered previously; others are entirely
              new classes of problems.
                  Multivariate methods are extremely powerful, for they allow the researcher to
              manipulate more variables than can otherwise be assimilated.  They are compli-
              cated, however, both in their theoretical structure and in their operational method-
              ology.  For some of  the procedures, statistical theory and tests have been worked
              out  only for  the most  restrictive  set of  assumptions.  The nature and behavior
              of the tests under more relaxed, general assumptions (such as those necessary for
              most real-world problems) are inadequately known. In fact, some of the procedures
              we will consider have no theoretical statistical basis at all, and tests of  significance
              have yet to be devised. Nevertheless, these methods seem to hold the most promise
              for fruitful returns in geological investigations.  Most of  the problems in geology
              involve complex and interacting forces which are impossible to isolate and study
              individually. Often a meaningful decision as to the relative worth of one of a num-
              ber of  possible variables cannot be made.  The best course of  action frequently is
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