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Concentration of iron and manganese in deep sea nodules

Varying percentages of iron and manganese in nodules from different environments. The iron/manganese ratio is controlled by the ratio of hydrogenetic/diagenetic input and whether or not the sediments involved in diagenesis are oxic, containing measurable amounts of oxygen. The Cook Islands nodules are almost solely hydrogenetic.

Year: 2014

From collection: Deep Sea Minerals Volume 1B

Cartographer: GRID-Arendal

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