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124    Handbook of gold exploration and evaluation

                     Table 2.11 Characteristic forms of low sulphidation and high sulphidation
                     alteration assemblages (after White and Hedenquist, 1995b)

                     Low sulphidation             High sulphidation

                     (Adularia-sericite)          (Acid sulphate)
                     Open-space veins dominant    Veins subordinate, locally dominant
                     Disseminate ore mostly minor  Disseminated ore dominant
                     Replacement of minor ore     Replacement ore common
                     Stockwork ore common         Stockwork ore minor




              Low-sulphidation ores
              Mineralising fluids in low sulphidation gold systems are typically dominated by
              deeply circulating meteoric waters which have absorbed acid magmatic gases
              (CO 2 , SO 2 , HCl). Such fluids equilibrate with their host rocks in a low
              sulphidation, epithermal gold environment, thus becoming reduced and develop-
              ing a near-neutral pH (Giggenbach, 1991). The ore association is produced by
              the near-neutral pH solutions boiling at shallow depths, and generating CO 2 and
              H 2 S-rich vapours. Condensation of these vapours in the vadose zone above the
              water table, leads to the formation of steam heated acid-sulphate waters with
              increasing pH. Eventually, the loss of H 2 S from the solution causes the solubility
              of gold to decrease, thus leading to its precipitation (Henley et al., 1984).
                 Topography is of major importance. Major low sulphidation deposits formed
              in shallow conduits in low relief areas are likely to be distributed above a feeder


              Table 2.12 Ore minerals in epithermal ores (after White and Hedenquist, 1995b and
              Buchanan, 1981)

                                    Low sulphidation     High sulphidation
              Pyrite                ubiquitous (abundant)  ubiquitous (abundant)
              Sphalerite            common (variable)    common (very minor)
              Galena                common (variable)    common (very minor)
              Chalcopyrite          common (very minor)  common (minor)
              Enargite-Luzonite     rare (very minor)    ubiquitous (variable)
              Tennantite-tetrahedrite  common (very minor)  common (variable)
              Covellite             uncommon (very minor)  common (minor)
              Stibnite              uncommon (very minor)  rare (very minor)
              Orpiment              rare (very minor)    rare (very minor)
              Realgar               rare (very minor)    rare (very minor)
              Arsenopyrite          common (minor)       rare (very minor)
              Cinnabar              uncommon (minor)     rare (very minor)
              Electrum              common (variable)    uncommon (very minor)
              Native gold           common (very minor)  common (minor)
              Tellurides-selenides  common (very minor)  uncommon (variable)
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