COPY OF FINAL PROSPECTUS - Mirabela Nickel
COPY OF FINAL PROSPECTUS - Mirabela Nickel
COPY OF FINAL PROSPECTUS - Mirabela Nickel
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
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