Page 118 - Handbook of Gold Exploration and Evaluation
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98     Handbook of gold exploration and evaluation

                 Discoveries of evolving gold-bearing polymetallic sulphide deposits in
              marine settings, made initially as a result of submarine investigations at mid-
              ocean ridges, have similarly been extended to other parts of the marine
              environment including volcanic and tectonic settings in shallow marine, island
              arc environments. Smaller marginal basins developed between island arc and
              nearby continental masses are somewhat analogous to the larger oceans in
              having spreading axes which involve separation of the lithosphere and upwelling
              of magma from the mantle to form new oceanic lithosphere. Differences in
              chemical composition of seafloor metal-rich sulphides and their precious metal
              contents are shown in Table 2.1 in relation to samples derived from a range of
              mid-ocean ridges and back-arc spreading centres.
                 A polymetallic sulphide ore body located in the Atlantis Deep, due west of
              Mecca in the Red Sea, represents the style of mineralisation that may occur at an
              early stage of seafloor spreading during the opening of an ocean basin (Fig.
              2.18). The metalliferous muds of this deposit are estimated to contain 30 million
              tonnes of iron, zinc and copper, some 6,000 tonnes of silver and 50 tonnes of
              gold at an average grade of about 2 ppb Au (Rona, 1986). The Red Sea deposit



              Table 2.1 Bulk chemical composition of seafloor polymetallic sulphides from mid-
              ocean ridges and back-arc spreading centres

                              Mid-ocean ridges             Back-arc ridges

                           Volcanic-    Sediment-   Intraoceanic 3  Intracontinental 4
                            hosted 1     hosted 2

              N             890           57          317            28
              Fe (wt%)       23.6         24.0         13.3           7.0
              Zn             11.7          4.7         15.1          18.4
              Cu              4.3          1.3          5.1           2.0
              Pb              0.2          1.1          1.2          11.5
              As              0.03         0.3          0.1           1.5
              Sb              0.01         0.06         0.01          0.3
              Ba              1.7          7.0         13.0           7.2
              Ag (ppm)      143          142          195          2766
              Au              1.2          0.8          2.9           3.8
              1
               Explorer Ridge, Endeavour Ridge: MainVent and High Rise Fields, Axial Seamount: AHSES and
              CASAM, Cleft Segment: N and S Fields, East Pacific Rise: 11ëN, 13ëN, 21ëN, 7ë30 S. 16ë45 S.
                                                                             0
                                                                       0
                  0
              18ë30 S. 21ëS. Galapagos Rift,TAG: Active Mound, Mir and Alvin Zones, Snake Pit Mid-Atlantic
              Ridge 24.5ëN.
              2
               EscanabaTrough, Guaymas Basin.
              3
               MarianaTrough, Manus Basin, North Fiji Basin: KingsTriple Junction,White Church,Vai Lili, Hine
              Hina Fields.
              4
               OkinawaTrough,
              Data compiledby Geological Surveyof Canada and Freiberg Universityof MiningandTechnology,
              Germany.
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