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Volcanogenic massive sulphide (VMS) deposits form at or near the seafloor from metal-rich hydrothermal fluids associated with submarine volcanic activity. They typically occur as lenses of polymetallic massive sulphide and are major sources of base metals and precious metals. VMS deposits have two components - a mound-shaped stratabound massive sulphide body underlain by stockwork veins and disseminated sulphides. They are classified based on their base metal content and host rock lithology. Sedimentary exh
- Author
- Didar Koçyiğit
- Language
- EN