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New geochemical and mineralogical constraints on the genesis of the Vani hydrothermal manganese deposit at NW Milos island, Greece: Comparison with the Aspro Gialoudi deposit and implications for the formation of the Milos manganese mineralization
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The Milos volcanic island, Greece host large Mn-Ba-Pb-Zn-Ag deposits formed in a subseafloor/seafloor environment.

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Mn-deposition is related to base- and precious metal intermediate-sulfidation epithermal mineralization.

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Mineralization is controlled by alternating cycles of deposition of sulfides and manganese oxides within major faults

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