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Geology of gold ore deposits  123

            2.4.5 Epithermal ores

            The term epithermal is given to deposits that form at shallow depths (surface to
            about 2 km) in the Earth's crust over the temperature range 150 ëC to 300 ëC
            (Berger and Eimon, 1983). Epithermal gold tends to have a more distinctive
            primary provenance than mesothermal gold, occurring mostly in the volcanic
            rocks and shallow depth intrusives of convergent tectonic settings. Two distinc-
            tive styles of epithermal gold mineralisation are developed from fluids of
            contrasting geochemistry. Each style has its own characteristic mineralogy and
            wall rock alteration signature:
            · low sulfidation systems are formed from reduced near-neutral pH fluids with
              large meteoric water input
            · high sulfidation systems form from oxidised acidic fluids generated in the
              magmatic-hydrothermal system.
              White and Hedenquist (1995b) list the characteristic forms of the two styles
            in Table 2.10 to help distinguish between them in the field. The authors point to
            the necessity of making this distinction because `although the two styles have
            similar alteration mineralogies, the distribution of the alteration zones is differ-
            ent and the economic potential is associated with different parts of the system'.
            Alteration zoning, but only where the style is correctly identified, indicates the
            prospective parts of a system. The authors in Table 2.11 give examples of
            epithermal gold deposits. The ore minerals in epithermal gold-rich ores are
            shown in Table 2.12 in order of frequency of occurrence. This table is based
            upon compilation of mineral data from more than 130 epithermal deposits in the
            south-west Pacific region (White, 1995a) and 47 deposits in North and Central
            America (Buchanan, 1981).



                   Table 2.10 Examples of epithermal deposits (after White and Hedenquist,
                   1995b)
                   Low sulphidation               High sulphidation

                   McLaughlin, California, USA    Goldfield, Nevada, USA
                   Round Mountain, Nevada, USA    Summerville, Colorado, USA
                   Hishikari, Japan               Iwato, Kasuga and Akeshi, Japan
                   Emperor, Fiji                  La Coipa, Chile
                   Gold Cross, New Zealand        El Indio, Chile
                   Waihi, New Zealand             Pueblo Viejo, Dominican Republic
                   Lebong Tandai, Indonesia       Chinkuashih, Taiwan
                   Kelian, Indoensia              Rodalquilar, Spain
                   Porgera Zone VII, Papua New Guinea Lepanto, Philippines
                   Pajingo, Australia             Lahoca, Hungary
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