Hydrothermal sediments are characterized by high concentrations of metals, mainly Fe and Mn, but also Cu, Zn, and Au, originating from hydrothermal sources (Gurvich, 2006;Shearme et al., 1983). In the ocean, these metal-rich sediments form in the vicinity of seafloor hydrothermal systems, for example, in back-arc basins and at mid-oceanic ridges (Gurvich, 2006;Hannington et al., 2011). A number of different hydrothermal processes are known to generate these metalliferous sediments, including the settling of primary hydrothermal plume particles,