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Minerals Report - International Seabed Authority

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At Niau, the tonnage of material with economic merit has been<br />

estimated to be 1 million dry tonnes with average cobalt content of 1.2%,<br />

based on recovering only the first 2 cm of the crusts. Dilution of this layer by<br />

the underlying material will certainly occur, but it seems possible to separate<br />

the crust by ore processing techniques. Several similar deposits have been<br />

discovered in the vicinity [26] that could increase this speculative inferred<br />

resource to five Mt, which could then produce 50 000 t of cobalt.<br />

Total resources of cobalt from Co-rich crusts in the central Pacific have<br />

been estimated to 500 million tonnes [30] (100 deposits similar to Niau).<br />

The exploration techniques must be improved considerably in order to<br />

provide the necessary parameters for the design of mining and processing<br />

methods. A better knowledge of the micro topography can be obtain by using<br />

deep-towed multibeam sonar associated with continuous high resolution TV<br />

recordings. Sampling methods must be completely retailored. Rotary<br />

diamond drilling machines equipped with a multicorer system must be<br />

developed to provide a fast and cheap sampling method with better recovery.<br />

2.2.3. Massive sulphides deposits<br />

Unlike polymetallic nodules and crusts, massive sulphides were<br />

discovered rather recently. In February 1978, the French manned submersible<br />

Cyana went to an area where it found tall conical mounds made of<br />

scoriaceous material that was sampled. Several months later, the samples<br />

proved to be mostly composed of zinc and copper sulphides [31]. One year<br />

later, from the American submersible Alvin, hot springs were observed<br />

blowing black smoke at the top of similar "chimneys". Since, many<br />

occurrences of black smokers and massive sulphides mounds have been<br />

discovered, not only on spreading ridges, but also in back-arc subduction<br />

zones and the flanks of intraplate volcanoes, as predicted from fossil massive<br />

sulphides deposits [32-34].<br />

In spite of the considerable amount of survey work that has been done,<br />

the available information is still inadequate to evaluate the economic potential<br />

of these occurrences.<br />

INTERNATIONAL SEABED AUTHORITY 431

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