Page 176 - Geochemical Anomaly and Mineral Prospectivity Mapping in GIS
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Analysis of Geologic Controls on Mineral Occurrence                  177

           TABLE 6-III

           Results of distance correlation calculations to quantify spatial association between occurrences of
           epithermal Au deposits and NNW-trending faults/fractures, Aroroy district (Philippines). Table
           entries in bold pertain to optimal spatial association

               AP     Y max (m)   r d  jx d  jy     t-value*   Proximal- r d  jx d  jy  Distal- r d  jx d  jy
                            r
                        j
               C          200      0.9981     53.123      0.9962         0.9771
               N          200      0.9994     98.819      0.9994         0.9963
               NE         100      0.9984     58.081      0.9978         0.9864
               E          200      0.9914     25.193      0.9857         0.9249
               SE         200      0.9996    112.630      0.9992         0.9949
               S          200      0.9999    308.139      0.9999         0.9989
               SW         200      0.9989     69.957      0.9985         0.9905
               W          200      0.9988     68.604      0.9983         0.9960
               NW         100      0.9999    233.427      0.9998         0.9988
           *Calculated values of  r d  jx d  jy   are significantly different from zero; the critical  t-value at

           α=0.001 and ν=13-2=11 degrees of freedom is 4.025 (Davis, 2002).


              Table 6-V and Fig. 6-14C indicate that there is positive spatial association between
           the epithermal Au deposits occurrences and intersections of NNW and NW-trending
           faults/fractures in the study area and the positive spatial association is optimal within 0.9
           km of intersections of NNW- and NW-trending faults/fractures. Inspection of individual
           distances between the epithermal Au deposits and intersections of NNW- and  NW-


           TABLE 6-IV

           Results of distance correlation calculations to quantify spatial association between occurrences of
           epithermal Au  deposits and NW-trending faults/fractures, Aroroy district (Philippines). Table
           entries in bold pertain to optimal spatial association.

               AP     Y max (m)  r d  jx d  jy     t-value*   Proximal- r d  jx d  jy  Distal- r d  jx d  jy
                       j
                            r
               C         800       0.9739    14.219       0.9526         0.8497
               N         600       0.9893    22.519       0.9811         0.9230
               NE        600       0.9872    20.513       0.9787         0.8917
               E         800       0.9752    14.624       0.9501         0.8932
               SE        600       0.9969    41.905       0.9945         0.9815
               S         700       0.9956    35.309       0.9925         0.9565
               SW        600       0.9854    19.215       0.9727         0.8961
               W         700       0.9878    20.841       0.9765         0.9372
               NW        600       0.9975    46.962       0.9954         0.9598
           *Calculated values of  r d  jx d  jy   are significantly different from zero; the critical  t-value at
           α=0.001 and ν=13-2=11 degrees of freedom is 4.025 (Davis, 2002).
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