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australia's identified mineral resources 2005 - Geoscience Australia

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AUSTRALIA’S IDENTIFIED MINERAL RESOURCES <strong>2005</strong><br />

DAP (20% P and 18% N) is used on broad-acre crops such as cereal, legume, fodder, horticultural<br />

and row crops, and dairy and newly-established pastures. MAP (22% P and 10% N) assists with early<br />

crop growth and enhances phosphorous uptake in broad-acre crops.<br />

Resources<br />

EDR of phosphate rock decreased by 5% in 2004 compared to the previous year. All EDR is<br />

sedimentary phosphate rock (phosphorites), with an average grade of about 24% P 2 O 5 at Phosphate<br />

Hill. The decrease resulted from production depletion and exclusion of small zones at the peripheries<br />

of the Phosphate Hill deposit, which are no longer regard as practical to mine. There is no publicly<br />

available information on Christmas Island’s phosphate <strong>resources</strong>. <strong>Geoscience</strong> <strong>Australia</strong>, however,<br />

has reasonably detailed knowledge of this deposit and known <strong>resources</strong> remaining within the<br />

existing mining lease on the island.<br />

Most of <strong>Australia</strong>’s demonstrated <strong>resources</strong> of phosphate occur in the Georgina Basin and are<br />

classified as paramarginal. Two deposits, Swan and Emu, occur within carbonatite at Mount Weld,<br />

26 km southeast of Laverton (WA), where a phosphate-rich zone has formed by the solution and<br />

weathering of a primary carbonatite.<br />

The bulk of <strong>Australia</strong>’s inferred phosphate <strong>resources</strong> are in phosphorites in the Georgina Basin,<br />

and these are distributed between Queensland, Western <strong>Australia</strong> and the Northern Territory.<br />

Exploration<br />

Data relating to exploration for phosphate are not available.<br />

Production<br />

<strong>Australia</strong> produced 2 039 kt of fertiliser in 2004 (649 kt DAP and 1 390 kt MAP). DAP came from rock<br />

phosphate ore treated at WMC Resources’ Queensland Fertiliser Operations (QFO) at Phosphate<br />

Hill. MAP was manufactured from domestic (Phosphate Hill) and imported rock phosphate.<br />

World Ranking<br />

<strong>Australia</strong>’s EDR of phosphate rock comprises less than 1% of the world’s total EDR of 18 Gt,<br />

which occurs principally as sedimentary marine phosphorites.<br />

Industry Developments<br />

WMC Fertilisers’ QFO is the only <strong>Australia</strong>n producer of DAP and MAP, both of which are sold in<br />

<strong>Australia</strong> and overseas. Its major production-based operations – phosphate mine and beneficiation,<br />

phosphoric acid, ammonia and granulation plants – are at Phosphate Hill. Supporting facilities are<br />

located at Mt Isa (sulphuric acid plant) and Townsville (storage and ship handling facilities).<br />

Ore reserves at Phosphate Hill are sufficient to support production for more than 30 years.<br />

In 2004, WMC Fertilisers sold 75% of its fertiliser in <strong>Australia</strong> and 25% in Asia and produce a new<br />

product, sulphur-fortified MAP, which is expected to capture greater marketing opportunities in the<br />

future. Sulphur-fortified MAP provides a high-quality, low cadmium and low-heavy-metal alternative<br />

for pastures and cropping requiring sulphur.<br />

61<br />

Shale Oil<br />

Oil shale is organic-rich shale that yields substantial quantities of oil (shale oil) by heating and<br />

distillation. One tonne of oil shale may contain over 200 litres of oil. The organic material in oil shale<br />

is kerogen, which can be a precursor to conventional oil reservoirs given appropriate conditions in<br />

the crust. <strong>Australia</strong>n oil shale deposits of commercial interest are predominantly in a series of narrow<br />

and deep extensional-basins near Gladstone and Mackay in central Queensland. These are thick<br />

Tertiary lacrustine (lake-formed) deposits that are relatively easy to mine. They contrast with<br />

generally harder carbonate bearing oil shales (marls) found elsewhere in the world that are more<br />

difficult to mine and process.

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