IMIS | Flanders Marine Institute

Flanders Marine Institute

Platform for marine research


Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Printer-friendly version

Polymetallic massive sulfides and gold mineralization at mid-ocean ridges and in subduction-related environments
Herzig, P.M.; Hannington, M.D. (2000). Polymetallic massive sulfides and gold mineralization at mid-ocean ridges and in subduction-related environments, in: Cronan, D.S. (Ed.) Handbook of marine mineral deposits. pp. 347-368
In: Cronan, D.S. (Ed.) (2000). Handbook of marine mineral deposits. CRC Marine Science Series, 17. CRC Press: Boca Raton. ISBN 0-8493-8429-X. 406 pp., more
In: Kennish, M.J.; Lutz, P.L. (Ed.) CRC Marine Science Series., more

Available in  Authors 
    VLIZ: Geochemistry [9088]


Authors  Top 
  • Herzig, P.M.
  • Hannington, M.D.

    Polymetallic massive sulfide deposits on the modern ocean floor have been found on fast- and slow- spreading ridges, axial and off-axis volcanoes, in sedimented rifts adjacent to continental margins, and in subduction-related arc and back-arc settings. The rnineralogy of these deposits includes both high (>300 to 350°C) and lower-temperature (<300°C) assemblages consisting of varying proportions of pyrrhotite, pyrite/marcasite, sphalerite/wurtzite, chalcopyrite, bornite, isocubanite, barite, anhydrite, and amorphous silica. Massive sulfides in back-arc spreading centers additionally may contain abundant galena, Pb-As-Sb sulfosalts (including jordanite, tennantite and tetrabedrite), realgar, orpiment, and locally native gold. Initial sampling of sulfides from subduction-related back-arc rifts suggests that these deposits have higher average concentrations of Zo, Pb, As, Sb, and Ba than deposits at the sediment-starved rnid-ocean ridges. Gold concentrations are locally high in samples from a number of rnid-ocean ridge deposits (up to 7 p pm) but may reach concentrations of more than 50 p pm Au in massive sulfides from immature back-arc rifts. Geochernical studies indicate that factors such as source rock compositions and rock-buffering of the hydrothermal fluids are important controls on the formation of gold-rich massive sulfides. Recent exploration of shallow-marine island arc environments of the western Pacific have also led to the discovery of several new types of seafloor hydrothermal activity with distinctive epithermal characteristics and notabIe enrichments of gold.

All data in IMIS is subject to the VLIZ privacy policy Top | Authors