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Catchment Basin Analysis of Stream Sediment Anomalies                131

           TABLE 5-V

           Values of  M j  (calculated according to equation  (5.5)) for lithologic units (represented by  their
           areas  in sample catchment basins) based on subset A of  log e -transformed uni-element stream
           sediment data (n=38) at sampling sites underlain by Aroroy Diorite (see Fig. 5-7), Aroroy district
           (Philippines).

                                      M j  values of lithologic units (data subset A; n=38)

                               Mandaon Formation   Aroroy Diorite   Sambulawan Formation
                   Cu              4.387              3.711             3.787
                   Zn              3.992              3.452             3.436
                   Ni              2.617              2.065             3.436
                   Co              2.635              2.512             2.833
                   Mn              6.659              6.210             6.107
                   As              0.441             -0.983            -0.669


           the Mandaon and Sambulawan Formations, most of the regression coefficients are higher
           than the corresponding  M j values; whilst for the  Aroroy Diorite, the regression
           coefficients and M j values are more or less similar.
              The estimates of regression coefficients and the M j values for the lithologic units in
           data subset B are given in Tables 5-VI and 5-VII, respectively. Note that the sample
           catchment basins for stream sediment data subset B are underlain by at least one of the
           six lithologic units listed in either Table 5-VI or 5-VII. The regression coefficients of
           lithologic units in data subset B show that the alluvial deposits have the lowest geometric
           means of concentrations  of most elements, followed  by the  Nabongsoran Andesite,
           compared to the other lithologic units. In contrast, the estimated M j values of lithologic
           units in data subset B suggest that the Nabongsoran Andesite and the alluvial deposits
           have more or less similar geometric  mean  uni-element concentrations as the  other



           TABLE 5-VI

           Regression coefficients of lithologic units (represented as areal proportions in sample catchment
           basins) for subset B of log e -transformed uni-element stream sediment data (n=97) at sampling sites
           underlain by  dacitic/andesitic volcano-sedimentary rocks (see Fig. 5-7), Aroroy district
           (Philippines).

                             Regression coefficients of lithologic units (data subset B; n=97)
                       Mandaon    Aroroy   Sambulawan   Lanang   Nabongsoran   Alluvial
                       Formation   Diorite   Formation   Formation   Andesite   deposits
               Cu        4.262     4.176     4.089     4.028      2.203    -4.911
               Zn        4.051     3.699     3.593     4.218      4.218     2.140
               Ni        2.537     2.684     2.619     2.466      1.497    -5.320
               Co        2.905     2.607     3.065     2.798      2.629     0.678
               Mn        6.663     6.407     6.093     6.794      6.785     7.267
               As        1.511    -2.209     -0.303    0.864     -3.604     2.994
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