australia's identified mineral resources 2005 - Geoscience Australia
australia's identified mineral resources 2005 - Geoscience Australia
australia's identified mineral resources 2005 - Geoscience Australia
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AUSTRALIA’S IDENTIFIED MINERAL RESOURCES <strong>2005</strong><br />
Golden Grove (WA): Oxiana Ltd acquired the<br />
Golden Grove base and precious metals mine<br />
from Newmont Mining Corporation. Reserves at<br />
Golden Grove total 4.77 Mt at 6.9% Zn, 2.1%<br />
Cu, 0.9% Pb, 75 g/t Ag, and 1.3 g/t Au with an<br />
additional 12 Mt of <strong>resources</strong> for which drilling<br />
is being carried out to convert 70% of these to<br />
reserve status.<br />
Eloise (Qld): Barminco, a mining contractor<br />
company, purchased the Eloise copper mine<br />
from Breakaway Resources Ltd.<br />
Sulphur Springs (WA): CBH Resources Ltd<br />
acquired the Sulphur Springs copper-zinc<br />
deposit from Sipa Resources Ltd and announced<br />
it could bring the project online within 18<br />
months. Sulphur Springs has a reserve of 4.4 Mt<br />
at 1.8% Cu and 5.6% Zn.<br />
Telfer (WA): Newcrest Mining Ltd’s redevelopment<br />
of Telfer as a gold-copper mine<br />
commenced with staged production in early<br />
<strong>2005</strong>. It is expected to produce 800 000oz of<br />
gold and 55 000t of copper in 2006 with an<br />
expected mine life of 25 years.<br />
Underground blast-hole drilling, Golden Grove mine,<br />
Western <strong>Australia</strong> (Newmont <strong>Australia</strong> Ltd)<br />
Tritton (NSW): The Tritton copper mine, near Girilambone, commenced operations in 2004 (based<br />
on a total resource of 15.2 Mt at 2.7% Cu). It is expected to produce around 24 000 tpa of copper<br />
in concentrate over a 11-year life. Tritton will mainly be an underground operation with some ore<br />
extracted from a small open pit.<br />
Diamond<br />
Diamond is composed of carbon and is the hardest known natural substance, but a sharp blow can<br />
shatter it. It also has the highest thermal conductivity of any known material at room temperature.<br />
Diamonds are thought to form 150–200 km below the Earth’s surface at high temperatures (1 050–<br />
1 200°C) and pressures (45–55 kilobars). They are carried to the surface within kimberlite and<br />
lamproites that intrude through the crust. These intrusions form narrow cylindrical bodies, called<br />
‘pipes’ and only a very small proportion have significant diamond content. When pipes are eroded,<br />
liberated diamonds may accumulate in alluvial deposits. Diamonds may be found far from their<br />
source as their hardness allows them to survive multiple episodes of erosion and deposition.<br />
The quality of diamonds is subdivided into gem, near gem and industrial categories. In rare cases,<br />
up to 90% of diamonds in a deposit are of gem quality but most economic deposits contain 20 to<br />
40% gem quality diamonds. Current uses for diamond include jewellery, stone cutting and polishing,<br />
computer chip manufacture, machinery manufacture, mining and exploration, construction and<br />
transportation services. A large proportion of industrial diamond is manufactured and it is also<br />
possible to produce synthetic diamonds of gem quality.<br />
29<br />
Resources<br />
EDR for gem/near gem was 53.4 Mc and industrial 55.6 Mc, both down 26% compared with 2003 due<br />
to Argyle mine production and introduction of a new resource model and revised mine plan, which<br />
resulted in some ore reserve being classified as <strong>mineral</strong> resource.