Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments
Ferromanganese nodules are authigenic marine sediments that form over millions of years from the precipitation of Fe oxyhydroxides and Mn oxides from seawater (hydrogenetic-type growth) and sediment pore-water (diagenetic-type growth). Fe-Mn (oxyhydr)oxides grow in layers about nuclei, effectively s...
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Format: | Thesis |
Language: | unknown |
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2018
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Online Access: | https://doi.org/10.26686/wgtn.17131868 https://figshare.com/articles/thesis/Trace_elements_in_New_Zealand_ferromanganese_nodules_implications_for_deep_sea_environments/17131868 |