Page 190 - Geochemical Anomaly and Mineral Prospectivity Mapping in GIS
P. 190

192                                                             Chapter 7









































             Fig. 7-1. Schematic GIS-based procedures for creating binary or multi-class evidential maps from
             input spatial data of continuous or discrete fields. Evidential class scores are assigned and stored in
             attribute tables associated with evidential maps.


             sometimes called aggregation functions, in order to combine evidential maps result in a
             mineral prospectivity model.
                The process of evaluating or cross-validating a mineral prospectivity map involves a
             number  of steps (Fig  7-2). Firstly, a table histogram of descending classes  of
             prospectivity values (proscl) is obtained in order to determine the number of unit cells
             or pixels per class  (npixcl), cumulative number  of class pixels  (npixclc), total
             number of pixels (npixclt) and proportion of prospective areas (proparea). Values
             in the column proparea are derived by dividing values in the column npixclc with
             corresponding values in the column npixclt. Descending or decreasing prospectivity
             values are used in the table histogram because the objective is to study the predictive
             performances of increasing  proportions of prospective areas (i.e., from high to low
             prospectivity values). In the creation of a table histogram of descending prospectivity
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