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Minerals Report - International Seabed Authority

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The global data of both abundance and composition are compiled<br />

on a 1° latitude and longitude grid. Interpolation of data between sampled<br />

localities is based on a minimum surface tension routine (Smith and<br />

Wessel, 1990). This method has the advantage of adjusting value gradients<br />

locally according to the actual sample values, their location and frequency<br />

of occurrence. Interpolation is not believed to give meaningful results<br />

beyond 10° ranges from known localities and, therefore, the data grids do<br />

not extend beyond that limit.<br />

Where abundance, density and compositional data are absent, the<br />

likelihood of occurrence of specific resource types have had to be<br />

estimated from predictive models. These models use knowledge of the<br />

presence or absence of conditions favourable for resource formation to<br />

establish often non-unique predictions of likely occurrence. This method is<br />

especially applicable for gas hydrates and conventional hydrocarbon<br />

resources, although the latter are also described with reference to adjacent<br />

known reserves and estimated resources.<br />

Finally, a value is placed on the resources at current (June 2000)<br />

commodity prices. These estimates are valid only as far as they describe<br />

the total abundance and hence value of the resource in question. They do<br />

not include any recovery, treatment or other production costs that would<br />

be incurred but which, at present, are unknown. A state-by-state summary<br />

of the non-living resources within ELCS areas is given in appendix 1.<br />

4 Non-Living Resources on the Seafloor: Their Formation, Occurrence<br />

and Magnitude<br />

4.1 Marine Placer deposits<br />

4.1.1 What marine placer deposits comprise<br />

Marine placers are detrital heavy metallic minerals which have<br />

become separated from their normally associated light minerals, and can<br />

form in economic concentrations. The most economically important of<br />

these minerals are: cassiterite (tin), ilmenite (titanium), rutile (titanium),<br />

zircon (zirconium), chromite (chromium), monazite (thorium), magnetite<br />

(iron), gold and diamonds (Harben and Bates, 1990).<br />

INTERNATIONAL SEABED AUTHORITY 683

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