Characteristics of Co-rich ferromanganese nodules and crusts sampled in French Polynesia
In: Marine Geology. Elsevier: Amsterdam. ISSN 0025-3227; e-ISSN 1872-6151, meer
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| Trefwoorden |
Aquatic sciences > Marine sciences > Geology > Marine geology
Chemical elements > Metals > Transition elements > Heavy metals > Cobalt
Chemistry > Geochemistry > Sediment chemistry
Earth sciences > Geology
Earth sciences > Geology > Sedimentology
Earth sciences > Geophysics
Resources > Natural resources > Mineral resources > Mineral deposits > Seabed deposits > Nodules > Ferromanganese nodules
Sedimentation > Diagenesis > Authigenesis
Marien/Kust |
| Auteurs | | Top |
- Pichocki-Seyfried, C.
- Hoffer, M.
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| Abstract |
Co-rich ferromanganese nodules and crusts were sampled at water depths of about 1000 m on the southern flanks of the Tuamotu Archipelago in French Polynesia. Crusts developed on a hard sedimentary substrate form a continuous ferromanganese encrustation, about 2.5 cm in average thickness, on the plateaus and slopes of seamounts. Nodule clusters occur within the crusts on the tops of the plateaus. The characteristics of samples from French Polynesia are similar to those of Co-rich crusts from other regions of the North Pacific. Co-rich nodules and crusts from the Tuamotu Archipelago should be considered as a potential metal resource, similarly to those from the Hawaiian-Emperor Archipelago and the Line Islands-Mid-Pacific Mountains system. (DBO) |
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