Volcanogenic Massive Sulfide Deposit Geology

Summary

Volcanogenic massive sulphide (VMS) deposits are stratiform to lens-shaped accumulations of sulphide minerals formed by submarine hydrothermal venting at convergent margins, back-arc basins and seafloor spreading centres. Metal-rich fluids ascend through a feeder zone and discharge at the seafloor, precipitating layers of pyrite, chalcopyrite, sphalerite and galena interbedded with volcanic and sedimentary rocks. These deposits commonly exhibit a zoned mineralogy, with copper-rich cores grading outward to zinc-lead and iron-rich assemblages. Host sequences often comprise bimodal volcanic suites, pelagic sediments and turbidites, which record episodic hydrothermal pulses. Stockwork vein networks beneath the main ore lens and surrounding hydrothermal alteration halos provide key exploration targets. VMS systems represent major sources of copper, zinc, lead and precious metals, and their study enhances models of crustal fluid flow, metal remobilisation during orogenic events and basin evolution. Global examples include the Iberian Pyrite Belt, the Kuroko district and the Noranda camp, each illustrating variations in tectonic setting, volcanic host lithology and metal endowment. Understanding the interplay between magmatic processes, structural architecture and fluid chemistry underpins both exploration strategies and environmental management of legacy mine sites.

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Volcanogenic Massive Sulfide Deposit Geology publication trend

The graph below shows the total number of articles in volcanogenic massive sulfide deposit geology across all publications each year (not limited to Nature Index journals).

Technical terms

Volcanogenic Massive Sulphide (VMS) deposit: A stratabound sulphide ore body formed by submarine hydrothermal fluids at volcanic-hosted sites, rich in sulphide minerals such as pyrite, chalcopyrite, sphalerite and galena.

Stockwork: A network of interconnecting veins or veinlets of hydrothermal origin that serve as conduits for mineralising fluids from a deeper feeder zone.

Hydrothermal alteration: Chemical and mineralogical changes in host rocks caused by interaction with hot, mineral-laden fluids, often producing zoned assemblages of chlorite, sericite and quartz.

Geochemical halo: A concentric zone surrounding an orebody characterised by anomalous concentrations of indicator elements such as copper, zinc, lead, antimony, thallium and barium.

Bimodal volcanism: The occurrence of coeval felsic and mafic volcanic rocks within a single volcanic sequence, reflecting diverse magma sources and contributing to the metal fertility of VMS systems.

References

  1. Unveiling High-Tech Metals in Roasted Pyrite Wastes from the Iberian Pyrite Belt, SW Spain. Sustainability (2023).
  2. Vectors to ore in replacive volcanogenic massive sulfide (VMS) deposits of the northern Iberian Pyrite Belt: mineral zoning, whole rock geochemistry, and application of portable X-ray fluorescence. Solid Earth (SE) (2021).
  3. The bimodal Fii-A2-type and calc-alkaline volcanic sequence of the Aljustrel brownfield region, Iberian Pyrite Belt, SW Iberian Massif. Geochemistry (2024).

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