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Applied Earth Science
Transactions of the Institutions of Mining and Metallurgy: Section B
Volume 126, 2017 - Issue 2
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Abstracts

Fe-rich cap lithologies in the TAG hydrothermal field: implications for the preservation of extinct seafloor massive sulphide deposits

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References

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  • Jones S, Gemmell JB, Davidson GJ. 2006. Petrographic, geochemical, and fluid inclusion evidence for the origin of siliceous cap rocks above volcanic-hosted massive sulfide deposits at Myra Falls, Vancouver Island, British Columbia, Canada. Econ Geol. 101:555–584. doi: 10.2113/gsecongeo.101.3.555
  • Petersen S, Krätschell A, Augustin N, Jamieson J, Hein RH, Hannington MD. 2016. News from the seabed – geological characteristics and resource potential of deep-sea mineral resources. Mar Policy. 70:175–187. doi: 10.1016/j.marpol.2016.03.012
  • Slack JF. 2012. Exhalites in volcanogenic massive sulfide occurrence model. U.S. Geological Survey Scientific Investigations Report 2010-5070-C, Chapter 10, 6 p.

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