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Gold Chapter (855 KB) - Ministry of Mines and Energy

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Mineral Resources <strong>of</strong> Namibia Precious Metals - <strong>Gold</strong><br />

Figure 9: Cross-section through the Navachab orebody (line 2600) (Navachab <strong>Gold</strong> Mine, 1997)<br />

chalcopyrite, calc-silicate minerals, garnet,<br />

biotite <strong>and</strong> quartz in the distinctly b<strong>and</strong>ed<br />

calc-silicate marble unit.<br />

- The hanging wall b<strong>and</strong>ed grey marbles (M<br />

zone) <strong>and</strong> mottled dolomitic marbles (DM<br />

zone) host two sets <strong>of</strong> intersecting <strong>and</strong><br />

crosscutting vein stockworks that also<br />

plunge to the north. Here the gold<br />

mineralisation occurs in the quartz-calcite<br />

veins that although individually exhibiting<br />

very high grades result in a low recoverable<br />

grade due to dilution as a result <strong>of</strong> the<br />

irregular vain frequency. <strong>Gold</strong> particle size<br />

tends to be coarser in this zone, which<br />

increases the nugget effect <strong>and</strong> makes ore/<br />

waste forecasting very difficult.<br />

The bulk <strong>of</strong> the gold is present in fractures<br />

along grain boundaries in the calc-silicate<br />

minerals, accompanied by very fine quartz. Rare<br />

coarse gold is contained in a quartz-rich calcitebiotite<br />

gangue. Native gold accounts for more<br />

than 85% <strong>of</strong> the total gold, with most <strong>of</strong> the<br />

reminder occurring as maldonite (Au 2 Bi). The<br />

gold to silver ratio is approximately 15:1.<br />

4.1 - 22<br />

Sulphides, mainly pyrrhotite with accessory<br />

pyrite, minor chalcopyrite <strong>and</strong> sphalerite are<br />

locally abundant <strong>and</strong> even massive. Scheelite is<br />

occationally associated with the sulphides. The<br />

sulphides do not host gold mineralisation<br />

although they are <strong>of</strong>ten in close proximity. None<br />

<strong>of</strong> the minor minerals is present in sufficient<br />

quantity to warrant recovery <strong>and</strong>, as far as is<br />

known, do not interfere in gold extraction.<br />

Currently Navachab’s ore reserve is 10.4 Mt<br />

at an average grade <strong>of</strong> 2.56 g/t <strong>and</strong> cut-<strong>of</strong>f grade<br />

<strong>of</strong> 0.8 g/t, giving a life-<strong>of</strong>-mine <strong>of</strong> seven years.<br />

This should be extended once the ore reserves<br />

are recalculated after the two-year, 30 000-m<br />

reverse-circulation drilling programme is<br />

completed (mid 1997). An additional 3 000 m <strong>of</strong><br />

drilling (RC with some diamond coring) is to be<br />

done to confirm the second shoot.<br />

While management, exploration, mine<br />

planning, grade control <strong>and</strong> the plant are the<br />

responsibilities <strong>of</strong> Navachab itself, the mining<br />

operation is done under contract.<br />

A geotechnical programme covering rock

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