Metalliferous Sediments and Sedimentary Rock-Hosted Stratiform and/or Stratabound Hydrothermal Mineral Systems


In this chapter I discuss and describe a range of hydrothermal mineral systems that are generated at passive margins, in basin structures of intracontinental or back-arc rifts, with or without obvious connection to igneous activity, seafloor metalliferous sediments and iron and manganese oxide accumulations. Passive margins and rift-related ore deposits include those known as Mississipi Valley-type (MVT), sedimentary exhalative polymetallic massive sulphides (SEDEX) and the Cu-rich stratabound and stratiform disseminated sulphides, all of which can be broadly grouped under the wider family of sedimentary-hydrothermal ore systems.


Fluid Inclusion Hydrothermal Fluid Mantle Plume Massive Sulphide Iron Formation 
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© Springer Science+Business Media B.V. 2009

Authors and Affiliations

  1. 1.Geological Survey of Western AustraliaEast PerthAustralia

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