Volcanogenic Massive Sulphide

Overview:


VMS deposits are defined as a massive accumulation of pyritic sulfides formed during discharge of hydrothermal fluids on the seafloor ("black smokers"). When economic, they tend to exhibit high grades of base metals. The metal distribution is zoned with a decrease in Cu/(Zn + Pb) upward and outward from the base of the lens-shaped massive sulfide deposit. Many deposits display a chloritized remnant feeder pipe. VMS deposits are important sources of copper, zinc, lead, gold and silver, with cobalt, tin, barium, sulfur, selenium, manganese, cadmium, indium, bismuth, tellurium, gallium and germanium as co- or by-products.

The video on VMS and SedEx has been provided by Andrew Jackson of Sprott Global Resource Investments Ltd.

Download (VMS.pptx)

VMS References (free):


  • Volcanogenic Massive Sulfide Occurrence Model
    (2010) Shanks, W.C.P. III, and Thurston, R., eds., Chapter C of Mineral Deposit Models for Resource Assessment, U.S. Geological Survey Scientific Investigations Report 2010−5070-C, 345 p.
  • Volcanogenic Massive Sulfide Deposits of British Columbia
    (1991) Hoy, T., in Ore Deposits, Tectonics and Metallogeny in the Canadian Cordillera, Paper 1991 - 4 by W.J. McMillan, T. Höy, D.G. MacIntyre, J.L. Nelson, G.T. Nixon, J.L. Hammack, A. Panteleyev, G.E. Ray and I.C.L. Webster, Geological Survey of British Columbia, Canada.