Page 228 - Geochemical Anomaly and Mineral Prospectivity Mapping in GIS
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230                                                             Chapter 7

             TABLE 7-VIII

             Examples of values of EBFs assigned  to  evidential classes in individual evidential maps
             portraying the recognition criteria for epithermal Au prospectivity, Aroroy district (Philippines).
             Values of Bel and Unc are first estimated together and then Dis is derived as 1–Bel–Unc (see text
             for further explanation). Ranges of values in bold include the threshold value of spatial data of
             optimum positive spatial associations with epithermal Au deposits in the case study area.

                                                                        2
                        Proximity to NNW 1                   Proximity  to FI
             Range (km)   Bel     Unc      Dis   Range (km)  Bel     Unc       Dis
             0.00 – 0.08   0.30   0.44     0.26   0.00 – 0.39  0.30   0.44    0.26
             0.08 – 0.15   0.35   0.43     0.22   0.39 – 0.58  0.40   0.42    0.18
             0.15 – 0.23   0.40   0.42     0.18   0.58 – 0.80  0.45   0.41    0.14
             0.23 – 0.32   0.45   0.41     0.14   0.80 – 1.09  0.50  0.40     0.10
             0.32 – 0.41   0.50   0.40     0.10  1.09 –  1.40  0.40  0.42     0.18
             0.41 – 0.52   0.40   0.42     0.18   1.40 – 1.80  0.20   0.46    0.34
             0.52 – 0.71   0.30   0.44     0.26   1.80 – 2.32  0.10   0.47    0.43
             0.71 – 1.06   0.20   0.46     0.34   2.32 – 2.92  0.05   0.48    0.47
             1.06 – 1.73   0.10   0.48     0.42   2.92 – 3.62  0.03   0.49    0.48
             1.73 – 3.55   0.05   0.50     0.45   3.62 – 5.92  0.01   0.50    0.49
                                                                       4
                        Proximity to NW 3                     ANOMALY
             Range (km)   Bel     Unc      Dis     Range     Bel     Unc       Dis
             0.00 – 0.18   0.30   0.44     0.26   No data   0.00     1.00     0.00
             0.18 – 0.36   0.35   0.43     0.22   0.00 – 0.06  0.05   0.50    0.45
             0.36 – 0.54   0.40   0.42     0.18   0.06 – 0.10  0.10   0.48    0.42
             0.54 – 0.75   0.45   0.41     0.14   0.10 – 0.16  0.15   0.46    0.39
             0.75 – 1.01   0.50   0.40     0.10  0.16 –  0.25  0.25  0.44     0.31
             1.01 – 1.29   0.40   0.42     0.18   0.25 – 0.29  0.35   0.43    0.22
             1.29 – 1.65   0.30   0.47     0.23   0.29 – 0.37  0.50  0.40     0.10
             1.65 – 2.24   0.20   0.48     0.32   0.37 – 0.49  0.45   0.41    0.14
             2.24 – 3.02   0.10   0.49     0.41   0.49 – 0.78  0.40   0.42    0.18
             3.02 –  5.32  0.05   0.50     0.45
             1 NNW-trending faults/fractures.  Intersections of NNW- and NW-trending faults/fractures.  NW-
                                     2
                                                                                3
                                4
             trending faults/fractures.  Integrated PC2 and  PC3 scores obtained from the  catchment basin
             analysis of stream sediment geochemical data (see Chapter 3).
                The formulae for combining EBFs of two spatial evidence maps (X 1, X 2) according to
             an AND operation are defined as (An et al., 1994a):

                      Bel  Bel
             Bel X 1 X  2 =  X 1 β  X 2  ,                                      (7.14)

                      Dis  Dis
             Dis X 1 X 2 =  X 1 β  X 2  , and                                   (7.15)
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