Ferromanganese Nodules and Crusts from the Christmas Island Region, Indian Ocean

A sampling expedition has shown that largely hydrogenetic marine ferromanganese deposits occur in the Christmas Island region south of Java (~10°S), as small nodules on seamount slopes and abyssal plains (red clay), and as thick crusts on volcanic ridges and seamounts. Vernadite is dominant, with bi...

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Bibliographic Details
Published in:Marine georesources & geotechnology 2002-10, Vol.20 (4), p.275-297
Main Authors: Exon, N. F., Raven, M. D., Carlo, E. H. De
Format: Article
Language:English
Subjects:
Christmas Island
Deep Ocean
Diagenetic
Ferromanganese Crusts
Ferromanganese Nodules
Hydrogenetic
Indian Ocean
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Summary:A sampling expedition has shown that largely hydrogenetic marine ferromanganese deposits occur in the Christmas Island region south of Java (~10°S), as small nodules on seamount slopes and abyssal plains (red clay), and as thick crusts on volcanic ridges and seamounts. Vernadite is dominant, with birnessite, jacobsite and todorokite common. Nodules were recovered in 25% of free-fall grab stations in water 4600-5900 m deep, and are not abundant where present. The nodules average 9.6% Fe, 19.7% Mn, 0.51% Ni, 0.49% Cu, and 0.12% Co. Crusts are common in water 1450-3700 m deep, with average deposition rates of 1-1.5 mm / m.y. The crusts average 13.9% Fe, 16.2% Mn, 0.35% Ni, 0.11% Cu, and 0.44% Co. Cobalt grades are higher (~0.8%) in shallower water ( < 2500 m), so future exploration should concentrate on depths of 500-1500 m near the oxygen minimum zone.
ISSN:1064-119X
1521-0618
DOI:10.1080/03608860290051958