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Rare Earths - Hastings Rare Metals Limited

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WESTERN<br />

AUSTRALIA<br />

Mines, deposits, prospects<br />

and occurrences<br />

Mineralization type<br />

Carbonatite and igneous intrusions<br />

Felsic volcaniclastic rocks<br />

Hydrothermal<br />

Pegmatite<br />

Sandstone-type U–REE<br />

Lignite-hosted U–Sc–REE<br />

Regolith<br />

Exmouth<br />

Geraldton<br />

Highway<br />

Town<br />

Karratha<br />

Perth<br />

INVESTMENT OPPORTUNITIES<br />

RARE EARTHS<br />

Newman<br />

Yangibana<br />

Wabli Creek<br />

Carnarvon<br />

Errida Creek<br />

Bunbury<br />

Meekatharra<br />

Albany<br />

Leonora<br />

Coolgardie<br />

Southern Cross<br />

Norseman<br />

Broome<br />

Esperance<br />

Telfer<br />

Wyndham<br />

Derby John Galt<br />

Copperhead<br />

Brockman<br />

Halls<br />

Fitzroy Crossing<br />

Creek<br />

Browns Range<br />

Mt Weld<br />

Cummins Range<br />

Mulga Rock<br />

Ponton<br />

Cundeelee<br />

Kalgoorlie–Boulder<br />

Kununurra<br />

Killi Killi<br />

200 km<br />

*<br />

Project<br />

Mt Weld<br />

REE<br />

Mount Weld — a new supply of<br />

rare earths to the world!<br />

Ambassador (Mulga Rock) uranium<br />

— 3% of projected revenue from<br />

by-product REE<br />

Western Australia has great<br />

exploration potential for REE in:<br />

Carbonatite and alkaline to peralkaline ring<br />

complexes<br />

Alluvial placers and heavy mineral sands<br />

Ash-flow tuffs erupted from the volatile-rich<br />

roof zone of magma chambers<br />

Olympic Dam style deposits of iron oxide–<br />

copper–gold (IOCG)<br />

Hydrothermal quartz veins<br />

Sandstone-hosted detrital monazite<br />

Sandstone-hosted U–REE<br />

Ion absorption clays associated with laterite<br />

Current REE resource estimates<br />

<strong>Hastings</strong>–<br />

Brockman<br />

Cummins<br />

Range<br />

Host rocks Resources<br />

(Mt)<br />

Regolith;<br />

Carbonatite<br />

Trachytic<br />

tuff<br />

Regolith;<br />

Carbonatite<br />

Total rare earth oxides, including yttrium<br />

Average<br />

grade *<br />

(% REO)<br />

Contained<br />

REO<br />

(kt)<br />

17.49 8.08 1413<br />

36.2 0.21 549<br />

4.17 1.72 71<br />

Some historic, pre-JORC resource estimates exist for deposits<br />

at Ponton, Yangibana and in the east Kimberley region<br />

Mt Weld open pit and ore stockpiles with REO percentages<br />

Source: Lynas Corp Ltd.<br />

www.dmp.wa.gov.au<br />

Geological Survey of<br />

Western Australia


Caprock<br />

(weathered carbonatite)<br />

Alluvium<br />

Lacustrine clays<br />

Glimmerite alteration zone<br />

Archean<br />

greenstone<br />

Crown tantalum–<br />

niobium deposit<br />

Swan phosphate<br />

deposit<br />

1 km<br />

Dolerite<br />

Dyke<br />

Central Lanthanide<br />

Deposit (CLD)<br />

Supergene<br />

zone<br />

MT WELD CARBONATITE<br />

Residual zone<br />

zone<br />

alteration<br />

Glimmerite<br />

Archean<br />

greenstone<br />

Schematic section of the Mt Weld carbonatite<br />

Ponton REE Intrusive<br />

Ponton Dyke<br />

Mt Weld<br />

Cundeelee<br />

10 km 20 km<br />

Total Magnetic Intensity image (TMI) showing Mt Weld carbonatite<br />

TMI image showing Cundeelee ring-type instrusion and Ponton<br />

regolith<br />

cover<br />

Yangibana North<br />

Gossan<br />

Hook<br />

granite<br />

Hook South<br />

Kanes Gossan<br />

Tongue<br />

Yangibana<br />

Yangibana South<br />

Spider Hill<br />

Bald Hill<br />

0.5 mm<br />

Courtesy Union Oil development Corp.<br />

Ovoid apatite crystals in dolomitic matrix, Cundeelee<br />

Frasers<br />

Fraser Creek<br />

Gifford Creek (U)<br />

Stone Tank Well<br />

<strong>Rare</strong> Earth Element prospects around Gifford Creek, Yangibana<br />

<strong>Rare</strong> Earth Element (REE) prospect<br />

Uranium prospect<br />

Quartz veins<br />

Carbonatite dykes and sills<br />

Iron oxide veins<br />

www.dmp.wa.gov.au<br />

100 µm<br />

Back-scattered (BSE) image showing ferrocolumbite<br />

(grey) and monazite (white) grains from Gifford<br />

Creek carbonatite complex, Yangibana<br />

Geological Survey of<br />

Western Australia<br />

OCT 2011

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