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Analysis of Sequences of Data
















                                                   X
             Figure 4-13.  Sequence of data points to be analyzed  by the method of runs up and down.

             entire segment cdef can be considered as a single downward run. The interval ij
             can be considered either as part of the run down ghi or the run up ijk, as the total
             number of runs remains the same in either case. In this example, we are assuming
             that the successive points have integer values. If  the observations are expressions
             of magnitude, they ordinarily will contain fractional parts, and ties (two successive
             points with identical values) are unlikely.
                 By  considering only differences in magnitude between successive points, we
             have reduced the data sequence to a string having only two states (or three, if ties
             occur). We  can rewrite the sequence in Figure 4-13  in the following form:

                                         + + + -0-  + - -o+

                 Regarding the first zero as ‘I-”  gives a total of five runs, three of “+” and two of
             ‘I-”  (it makes no difference in the number of runs if we call the second zero “+” or
             “-”).  We  can now apply test procedures outlined for the case of  sequences of  two
             dissimilar items (Eqs. 4.8-4.10). We must have a large sample to utilize the normal
             approximation method presented here, but in most geologic problems, adequate
             numbers of  samples will be available.


                         Table 4-7.  Numbers of radiolarian tests per square centimeter
                                     in thin sections  of siliceous shale.
             (Bottom
             ofsection)  1  2  3  2  3  5     7  9  9  11  10  12  7  4  3  2  3
                         2  2  1   0   2  3  2  0  3  3  491010  8  912
                        10  12  14  22  17  19  14  4  2  1  0  0  8  14  16  27   (Topof
                                                                                 section)



                 In the study of  a silicified shale unit  in the Rocky Mountains, it was noted
             that the rock contained unusual numbers of well-preserved radiolarian tests. Their
             presence in the silicified shale suggested a causal relationship, so a sequence of
             samples was  collected at approximately equal intervals in  an exposure through
             the unit.  Thin sections were made of  the samples and the number of  radiolarian
             tests in a  10 x  10-mm area of  the slides was counted.  Data for 50 samples are
             given in Table 4-7  and shown graphically in Figure 4-14.  Does the abundance of

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