| The occurrence of gold has been studied in (1) seafloor sulfides from the N.E. Pacific and Mid-Atlantic, (2) metalliferous sediments, hydrothermal plumes, and vent waters from the East Pacific Rise and Explorer Ridge, (3) sub-seafloor stockwork mineralization from DSDP Hole 504B and Agrokipia B, Cyprus and (4) supergene sulfides and Fe-oxide gossans from the mid-Atlantic Ridge. A routine method for analysis of gold and associated elements by direct neutron activation with a low-flux reactor was developed for this study. Gold contents of seafloor sulfides range from ;Quenched products from high-temperature vents (up to 350... |