Page 232 - Geochemical Anomaly and Mineral Prospectivity Mapping in GIS
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234                                                             Chapter 7























             Fig. 7-20. Maps of integrated EBFs [(A) Unc, (B) Pls and (C) Dis] accompanying the map of
             integrated  Bel (Fig. 7-19A) for the proposition of epithermal  Au prospectivity, Aroroy district
             (Philippines). The inference network in Fig. 7-4 was used in combining input evidential maps with
             EBFs given in Table 7-VIII. Triangles are locations of known epithermal Au  deposits; whilst
             polygon outlined in grey is area of stream sediment sample catchment basins (see Fig. 4-11).


             of locations without stream  sediment geochemical evidence, have lowest degrees  of
             uncertainty in the proposition  under examination. The other final maps  of integrated
             EBFs –  Unc,  Dis and  Pls (Fig.  7-20) – also provide  geo-information regarding the
             predictions portrayed in the final map of integrated Bel (Fig. 7-19A). The final map of
             integrated Unc (Fig. 7-20A) depicts locations where the input pieces of spatial evidence
             are insufficient to provide support for the proposition of mineral prospectivity. In the
             case study area, examples of such locations are obviously those without stream sediment
             geochemical evidence.  The final map of integrated  Pls (Fig. 7-20B)  depicts  not only
             prospective areas but also locations where additional pieces of spatial evidence are
             required to provide support for the proposition of mineral prospectivity. In the case study
             area, examples of such locations are in the east-central parts of the area where there are
             multi-element stream sediment anomalies (see Fig. 5-12) but faults/fractures are scarce
             (see Fig. 5-13A). The final map of integrated Dis (Fig. 7-20C) complements the pieces
             of spatial geo-information provided by the corresponding final maps of integrated Bel,
             Unc and  Pls in terms of depicting  prospective and non-prospective areas as well as
             locations where the input pieces of spatial evidence are insufficient to provide support
             for the proposition of mineral prospectivity.
                 The ability of explicit representation of evidential uncertainty, even in the case of
             missing evidence, is an advantage  of evidential belief modeling compared to the
             modeling techniques explained earlier. As in fuzzy logic modeling, the availability of
             different operators and the ability to modify inference networks for combining pieces of
             evidence is an advantage of evidential belief modeling compared to binary and multi-
             class index overlay modeling. Perhaps the  only  disadvantage  of evidential belief
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