Metalliferous Sediments and Sedimentary Rock-Hosted Stratiform and/or Stratabound Hydrothermal Mineral Systems
作者： Franco Pirajno
DOI: 10.1007/978-1-4020-8613-7_8
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摘要: In this chapter I discuss and describe a range of hydrothermal mineral systems that are generated at passive margins, in basin structures intracontinental or back-arc rifts, with without obvious connection to igneous activity, seafloor metalliferous sediments iron manganese oxide accumulations. Passive margins rift-related ore deposits include those known as Mississipi Valley-type (MVT), sedimentary exhalative polymetallic massive sulphides (SEDEX) the Cu-rich stratabound stratiform disseminated sulphides, all which can be broadly grouped under wider family sedimentary-hydrothermal systems.
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