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Investigates rare-earth elements in hydrogenous Fe-Mn formations, suggesting their role as geochemical indicators.
Contents of trace elements and their distribution are considered in the hydrogeneous Fe-Mn formations elevated on the La Monte Guyot. The nodules under study have, been shown to be geochemically specific, which is due to high REE content and stable, although variable in size, positive Ce-anomaly. Rare-earth elements are investigated as indicators of the conditions under which ferromanganese deposits form.
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Vasilieva et al. (1991) studied this question.
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