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Workshop on the Establishment of a Geological Model of ...

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As indicated by Figure 42, <strong>the</strong>re is no correlati<strong>on</strong> between nickel and cobalt c<strong>on</strong>centrati<strong>on</strong>s <strong>on</strong> a global<br />

scale for most <strong>of</strong> <strong>the</strong> CCZ. A positive relati<strong>on</strong>ship between nickel and cobalt anomalies may be detected in<br />

<strong>the</strong> western‐central part between l<strong>on</strong>gitude 137 o W and 147 o W.<br />

Figure 42: Nickel and Cobalt<br />

As shown in <strong>the</strong> figure, <strong>the</strong>re is, in general, <strong>the</strong> inverse correlati<strong>on</strong> between copper and cobalt c<strong>on</strong>tent<br />

for most <strong>of</strong> <strong>the</strong> Z<strong>on</strong>e, which in some places is less pr<strong>on</strong>ounced and sometimes (between l<strong>on</strong>gitude 138 o W and<br />

142 o W) high copper values coincide with high cobalt values in nodules.<br />

Nodule deposits<br />

One <strong>of</strong> <strong>the</strong> most important geological parameters <strong>of</strong> polymetallic nodules is <strong>the</strong>ir ability to form<br />

c<strong>on</strong>centrati<strong>on</strong>s with high abundance and metal c<strong>on</strong>tent, which can be c<strong>on</strong>sidered as nodule deposits with<br />

certain cut‐<strong>of</strong>f grades, which may have potential for ec<strong>on</strong>omic development in future.<br />

For <strong>the</strong> purpose <strong>of</strong> locating such deposits in <strong>the</strong> reserved areas, <strong>the</strong> author, <strong>on</strong> a c<strong>on</strong>sultancy with <strong>the</strong><br />

Authority, undertook in 1997 <strong>the</strong> study <strong>of</strong> estimating <strong>the</strong> resource potential <strong>of</strong> <strong>the</strong> reserved areas. Such basic<br />

criteria as nodule abundance and cumulative metal c<strong>on</strong>tent <strong>of</strong> three metals ‐ nickel, copper and cobalt – was<br />

used. A criteri<strong>on</strong> based <strong>on</strong> nickel equivalent was not used, since <strong>the</strong> pi<strong>on</strong>eer investors had applied a different<br />

formula to calculate that value. Besides, owing to <strong>the</strong> slight variati<strong>on</strong> in manganese c<strong>on</strong>tent values over<br />

different areas and low prices for manganese, that formula by itself will mostly represent values <strong>of</strong> c<strong>on</strong>tent <strong>of</strong><br />

<strong>the</strong> three metals, namely, nickel, copper and cobalt.<br />

The nodule resources that may be favourable for possible future first and sec<strong>on</strong>d generati<strong>on</strong> mining<br />

operati<strong>on</strong>s were defined by us as those with nodule abundance <strong>of</strong> more than 5 kg/ m 2 and Ni+Cu+Co c<strong>on</strong>tent<br />

<strong>of</strong> more than 2 per cent (basic assumpti<strong>on</strong>s used in 1980s during <strong>the</strong> drafting <strong>of</strong> <strong>the</strong> United Nati<strong>on</strong>s<br />

C<strong>on</strong>venti<strong>on</strong> <strong>on</strong> <strong>the</strong> Law <strong>of</strong> <strong>the</strong> Sea).<br />

They were divided into four nodule grades:<br />

Grade“A” Nodule deposits with abundance <strong>of</strong> more than 10 kg/ m 2 and Ni+Cu+Co metal<br />

c<strong>on</strong>tent <strong>of</strong> more than 2.5 per cent.<br />

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