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COPY OF FINAL PROSPECTUS - Mirabela Nickel

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dunite .................<br />

EM ...................<br />

gabbro .................<br />

geochemical .............<br />

geophysical ..............<br />

gossan .................<br />

granodioritic .............<br />

granulitic ...............<br />

greenstone ..............<br />

harzburgite ..............<br />

igneous rock .............<br />

intercalated .............<br />

interstitial ...............<br />

isotopic ................<br />

JORC .................<br />

kelyphitic ...............<br />

lamellar ................<br />

laterite .................<br />

lithostratigraphic ..........<br />

an igneous, plutonic rock, of ultramafic composition, with coarse-grained or<br />

phaneritic texture. The mineral assemblage is typically greater than 90%<br />

olivine with minor pyroxene and chromite. Dunite is the olivine-rich<br />

end-member of the peridotite group of mantle-derived rocks.<br />

electro-magnetic.<br />

a coarse-grained intrusive igneous rock composed of greenish-white feldspar<br />

and pyroxene.<br />

prospecting techniques which measure the content of specified metals in soils<br />

and rocks for the purpose of defining anomalies for further testing.<br />

prospecting techniques which measure the physical properties (magnetism,<br />

conductivity, density, etc.) of rocks and define anomalies for further testing.<br />

a ferruginous deposit remaining after the oxidation of the original sulphide<br />

minerals in a vein or ore zone.<br />

intrusive igneous rock similar to granite, but contains more plagioclase than<br />

potassium feldspar. It usually contains abundant biotite mica and<br />

hornblende, giving it a darker appearance than true granite. Mica may be<br />

present in well-formed hexagonal crystals, and hornblende may appear as<br />

needle-like crystals.<br />

a fine-grained metamorphic rock often banded in appearance and composed<br />

chiefly of feldspar, quartz, and garnet.<br />

a term applied regionally to sequences of mafic to ultramafic rocks.<br />

an ultramafic rock that is a variety of peridotite consisting of the minerals,<br />

olivine and low-Ca pyroxene (enstatite), and named for occurrences in the<br />

Harz Mountains of Germany. It commonly contains a few percent<br />

chromium-rich spinel as an accessory mineral.<br />

a rock formed by volcanic or magmatic processes.<br />

to insert, interpose, or interpolate.<br />

being or relating to a crystalline compound in which usually small atoms or<br />

ions of a nonmetal occupy holes between the larger metal atoms or ions in<br />

the crystal lattice.<br />

any of the several different forms of an element each having different atomic<br />

mass (mass number).<br />

the Australasian Code for Reporting of Mineral Resources and Ore Reserves<br />

prepared by the Joint Ore Reserves Committee of the Australasian Institute<br />

of Mining and Metallurgy, Australian Institute of Geoscientists and Mineral<br />

Council of Australia, as amended or supplemented.<br />

a mineral zone that is usually radial about another mineral or at the area<br />

between two minerals. Also known as ‘corona’.<br />

composed of fine, alternating layers of different materials in the form of<br />

lamellae.<br />

a highly weathered red subsoil or material rich in secondary oxides of iron,<br />

aluminum or both, that occurs as a residual product of weathering.<br />

dealing with the lithology of strata and their organization into units based on<br />

the lithological characteristics and the lithological correlations between the<br />

strata.<br />

A-2

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