Iron mineral structure, reactivity, and isotopic composition in a South Pacific Gyre ferromanganese nodule over 4 Ma
Deep-sea ferromanganese nodules accumulate trace elements from seawater and underlying sediment porewaters during the growth of concentric mineral layers over millions of years. These trace elements have the potential to record past ocean geochemical conditions. The goal of this study was to determi...
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Veröffentlicht in: | Geochimica et cosmochimica acta 2015-12, Vol.171 (C), p.61-79 |
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Sprache: | eng |
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