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152                                                             Chapter 6

             TABLE 6-II

             Numbers of different orders of reflexive nearest neighbours (RNNs) in the point pattern of
             occurrences of epithermal Au deposits in Aroroy district (Philippines).

             Order of RNNs           Observed number         Expected number in CSR
                   1 st                    8                    8.08
                   2 nd                    4                    4.28
                   3 rd                    4                    3.16
                   4 th                    0                    2.62
                   5 th                    2                    2.29
                   6 th                    2                    2.06

             rather than with respect to the study area. However, edge effects can be compensated by
             way of a number of methods (see Boots and Getis (1988) for details).
                Despite this slight discrepancy, the results of analysis of arrangement and analysis of
             dispersion of  the occurrences of epithermal Au  deposits in the case  study area are
             coherent. Thus, a generalisation can be made from the results of point pattern analysis
             shown in Tables 6-I and 6-II that the spatial distribution of occurrences of epithermal Au
             deposits in the Aroroy district is not random but assumes a regular pattern. The results of
             the analysis can imply that  more-or-less regularly-spaced geological features (e.g.,
             faults/fractures) may have controlled the circulation of mineralising hydrothermal fluids
             and thus the localisation of epithermal Au deposits at certain locations. This implication
             can be examined further via applications of fractal analysis and Fry analysis.
             Fractal analysis

                As  defined in Chapter  4, a fractal pattern  has  a  dimension  D f, known as the
             Hausdorff-Besicovitch dimension, which  exceeds its topological  (or Euclidean)
             dimension D (Mandelbrot, 1982, 1983). Fractal analysis of a point pattern of occurrences
             of certain types of mineral deposits has been demonstrated by Carlson (1991), Cheng
             and Agterberg (1995),  Cheng et al.  (1996),  Wei and  Pengda (2002), Weiberg  et  al.
             (2004), Hodkiewicz et al. (2005) and Ford and Blenkinsop (2008).
                The fractal dimension  of a  point pattern  can be determined  by the  box-counting
             method (see Fig. 4-1). A square grid or raster with a cell or pixel size δ (i.e., length or
             width of a pixel) is overlaid on a map of points. The number of pixels n(δ) containing
             one or more points is counted. The procedure is repeated for different values of δ and the
             results are plotted in a log-log graph. If the point pattern is a fractal, the plots of n(δ)
             versus δ satisfy a power-law relation (Mandelbrot, 1985; Feder, 1988), thus:

             n () Cδ=δ  − D b                                                    (6.1)
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