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: | Master Thesis |
| Language: | English |
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Victoria University of Wellington
2018
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| Online Access: | http://researcharchive.vuw.ac.nz/handle/10063/7738 |