A Glossary of Diamond Exploration and Mining
Terms. Within explanations, any words highlighted
blue have their own Glossary entry.
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Aeolian |
Sediment deposited by the action of wind. |
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Airborne/ Aeromagnetic Magnetic
survey |
A survey conducted from the air for the
purpose of recording the natural magnetic characteristics
of rocks on and below the surface of the earth; kimberlites,
the hostrock for diamonds, often have different magnetic
characteristics and form a magnetic anomaly. |
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Airborne Geophysics |
Taking geophysical measurements (such
as magnetometry) by airplane or helicopter. |
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Alluvial |
A sediment or gravel deposited by the
action of stream or river in a river bed, flood plain, lake,
fan at the foot of mountain slopes, or in estuaries that
may or may not contain diamonds or precious minerals or
both. |
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Alteration |
The recrystallisation of rock surrounding
an igneous intrusion in response to the heat supplied by
the intrusion. |
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Amphibolite |
A medium-grained dark coloured metamorphic
rock composed of hornblonde and other minerals. Formed by
medium grade metamorphism of basic igneous
rocks. |
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Anastomising |
A value higher or lower then the expected
which may outline a zone of potential exploration interest
but not necessarily of commercial significance. |
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Archaean craton |
Old and stable parts of the earth crust,
formed more than 2.5 billion years ago. They are good areas
for finding diamond-bearing kimberlites. |
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Archaean |
The oldest rocks of the Precambrian
era, formed over 2.5 billion years ago. |
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Artisanal |
Mining on a small scale, usually by hand
and often without the assistance of machinery or mechanical
tools. The term is sometimes extended to describe informal
mining by a person or persons outside of a registered commercial
organization. |
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Back filling |
The process of refilling a void, created
by mining, with waste rock or material resultant from successive
mining operations. |
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Basin |
A depression in the earth’s crust
filled with sediments. Laid
down by rivers or at the bottom of a lake or sea. |
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Bedrock |
The competent rock type near surface
overlain only by surficial material (soil, alluvial,
etc.). |
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Benefication |
To increase the grade of ore
after processing. |
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Blow (or Enlargement) |
A thickening (usually more than 10 m
thick) of a dyke (usually
about 1m thick). |
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Bort / boart |
Impure or discoloured diamond,
unless as a gem. Used for
industrial purposes. |
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Breccia |
Literally means ‘rubble’
and implies a rock deposited very to the source area. Also
applied to angular volcanic rocks from a volcanic vent. |
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Bulk sample |
A very large sample usually taken from
one site, and usually of several hundred tones weight. |
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Cainozoic/ Cenozoic |
Era of geological time from 65 million
years ago to date and includes the Tertiary
and Quaternary Periods. |
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Carat |
A unit of weight for diamonds,
equivalent to 0.2 of a gram. |
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Channel |
The deepest portion of stream through
which the main volume or current of water flows. |
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Chrome-diopside |
A mineral (pyroxene) rich in crome and
formed at great depth; common mineral in kimberlites. |
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Clear diamond |
A transparent diamond,
free of inclusions and fractures. |
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Concentrate sampling |
The process of sampling for kimberlite
indicator minerals. |
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Contact |
The surface along which two different
rock types are in contact. Especially applicable where igneous
rocks intrude country rocks. |
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Core drilling |
See Drillholes. |
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Country Rock |
The rock, or rocks, in which a mineral
deposit is intruded or hosted. |
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Craton |
Area of the earth’s crust, which
is no longer affected by mountain building processes and
has been stable for the last 1,000 million years. |
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Cretaceous |
The geologic period dating from 144 million
years ago to 65 million years ago. Noted for its deposition
of chalks seen at the White Cliffs of Dover. |
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Cut-off grade |
Lowest grade of ore
in a deposit that will recover mining costs; the cut-off
grade determines the workable tonnage of an ore. |
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Deposit |
Natural mass of coal, metal, or other
material for mining in the earth. |
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Diamond foundation |
Diamonds
are formed at great pressures (equivalent to depths of more
than 150 km) and at temperatures of about 1,200 to 1,400
celsius; these conditions exist under Archaean
cratons; diamonds have crystallized
and exist underneath these Archaean cratons; often for billions
of years; kimberlite volcanoes
tap the diamonds from these depths and carry them to the
surface of the volcanic explosion. |
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Diamond / kimberlite Pipe |
Nearly vertical, cylindrical body or
opening in rock. Near surface the kimberlite
pipes are found in clusters, at depth they coalesce and
link up with dykes. |
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Diamond |
A crystallized variety of pure carbon,
which may be of gem quality. |
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Diamondiferous |
Containing diamonds. |
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Diatreme |
The carrot shaped volcanic vent that
has formed by explosive action and is characteristic of
kimberlite pipes. Diatremes
typically cut through non-volcanic basement rocks. |
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Dip |
The angle of inclination of a mineral
deposit. The true dip is
always measured in a vertical plane perpendicular to the
strike. |
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Discontinuity |
Sudden interruption of a continuous phenomenon. |
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DMS |
Dense media separation; a process used
to separate and concentrate the mineral being recovered
from the other constituent minerals of the ore
being mined. |
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Dolerite |
A dark coloured, medium grained igneous
rock. |
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Drill / drilled |
The process of making/having made a hole,
usually into the earth. |
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Drillholes |
A hole drilled into a rock or mineral
deposit for the purpose of identifying its physical and
chemical characteristics. Where a sample of the rock is
to be recovered diamond impregnated
drill bits are used and a core recovered. |
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Duricrust |
Deposit of the weathering zone, especially
in subtropical environments, which may ultimately develop
into a hardened mass. |
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Dyke or Fissure |
A wall-like body of igneous
rock formed as the effect of having been pushed up into
a crack in the material over it when in heated and liquid
condition. Kimberlites move
from great depths toward the surface along fissures; a few
kilometers from the surface, the confining pressure of the
overlying rocks is sufficient to contain the explosive gaseous
kimberlite magma and a volcanic eruption results forming
an explosive crater; a pipe or diatrema is formed, containing
a chaotic mixture of kimberlite magma with shattered pieces
of surrounding rocks (the kimberlite breccia)
and with tuff layers on top
formed by the falling back of ash into the volcano. Along
the fissures underneath, the kimberlite cools and solidifies
forming walls (dykes). |
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Eclogite |
Very rare, course grained, igneous
rock with a chemical composition similar to that of basalt
but noted for the presence of the rare, bright green pyroxene
omphacite, and red, almandine-pyrope garnets. |
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Elluvial |
sediment formed in place by the weathering
of underlying rocks. |
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En-echelon |
The parallel or sub parallel alignment
of separate structural features, which are arranged obliquely
to a specific directional axis. |
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Enlargement |
See Blow. |
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Exploitation |
Mining of a natural resource deposit. |
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Exploration |
The search, using varied techniques,
with the objective to discover and evaluate natural resource
deposits of economic value. |
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Exposure |
Any geological feature that is visible,
whether on surface or underground. |
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Fancy / fancies |
Attractive, valuable and unusually rare
colour of a gem. |
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Fault |
Approximately plane surface of fracture
in a rock-body, caused by brittle failure, and along observable
relative displacement has occurred between adjacent blocks. |
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Fault zone |
A region which is bounded by major faults
within which subordinate faults may be found. |
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Fissure |
See Dyke. |
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Flats |
See Alluvial. |
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Fluvial |
Deposits in or pertaining to rivers. |
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Gem |
Attractive minerals used as jewellery.
A diamond free of flaws,
as far as can be determined by a trained observer with the
aid of a 10-power magnifying glass, and having a colour
and other characteristics that do not deleteriously affect
its value for use as a faceted ornamental diamond. |
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Gem quality |
Possessing the qualities of a gem. |
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Geochemical survey |
The sampling of rocks, stream sediments,
and soils in order to locate abnormal concentrations of
metallic elements or minerals. The samples are usually assayed
by various methods to determine the qualities of elements
or minerals in each sample. |
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Geophysical survey |
The exploration of an area in which physical
properties relating to geology are used. Geophysical methods
include seismic, magnetic, electromagnetic, gravity and
induced polarization techniques. |
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Geophysics |
Science of the physical properties of
the earth, its motion and forces and their effect. |
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Gneisses |
General petrological
term applied to course-grained, banded rocks that formed
during high-grade regional metamorphism. |
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Grades |
Internally, diamond
grades for primary deposits are stated both in carats
per tonne (ct / t) and carats per 100 tones (ct / 100t).
In the case of alluvial deposits,
industry practice is to quote grades in carats per tonne
or carats per cubic metre. |
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Granite |
A light coloured, course-grained, igneous
rock. |
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Granulite |
A course-grained, equigranular metamorphic
rock, consisting of quartz, feldspar and the anhydrous ferromagnesium
minerals pyroxene and garnet. |
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Gravel |
A course mixture of sand with pebbles
and cobbles, laid down by rivers, with pebbles and cobbles
derived from the erosion of rocks upstream in the catchment
area of the river. Diamondiferous
gravel contains diamonds
derived from the erosion of other diamond-bearing rocks
upstream. |
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Grease table |
A gently sloping table covered with grease
which serves as a concentrator of diamonds. |
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Groundmass |
The finer grained materials of igneous
rocks in which larger crystals and xenoliths are enclosed. |
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Hanging wall |
The upper rock wall in a flat or inclined
deposit (as opposed to footwall). |
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HMS |
Heavy Media Separation; a process used
to separate and concentrate the mineral being recovered
from the other constituent minerals of the ore
being mined. |
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Hydrology |
The science of water, its properties
and distribution, specifically of water under the earth. |
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Igneous rock |
Applied to those rocks that have crystallized
from a magma. |
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Ilmenite |
Natural ferrous titanite, a black, massive
substance important as an ore of Titanium. |
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Indicator minerals |
Minerals formed together with diamonds
at great depths and brought to the surface by the same kimberlites,
indicator minerals are much more abundant than diamonds
and are therefore much easier to trace in sample taken downstream
in rivers draining knimberlite pipes or dykes;
common indicator minerals are pyrope, ilmenite and chrome-diopside. |
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Intersection |
A specific feature intersected in a drillhole. |
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Intrusion / intrusive |
A volume of igneous
(molten) rock which was injected into older rock. |
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Jig |
Vibrating sleeve, moving up and down
in water, concentrating the heavy minerals of a sand or
gravel sample. |
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Karroo |
A geographical area of Southern Africa,
but also the name for a group of geological formations laid
down in the late Paleozoic and Mesozoic age (about 300 to
100 million years ago). |
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Kimberlite |
An uneven grained, ultramafic, intrusive
rock in which the visible minerals may include olivine,
phlogopite, pyrope garnet, picroilmenite and chrome-diopside
cemented by a groundmass,
which may include serpentine,
calcite and chromate. Kimberlite may be diamondiferous
and, along with olivine lamproites, are the only know primary
source of diamonds. |
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Lamproite |
Another type of deep volcanic rock, that
just as kimberlites, may
bring diamonds from great
depths to the surface. |
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Laterite |
Weathered product of rock, composed mainly
of hydrated iron and aluminum oxides and hydroxides, and
clay minerals. It is formed in humid tropical settings. |
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Macrodiamonds |
Macrodiamonds are generally defined as
diamonds larger than 0.5mm
in size. |
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Mafic |
Applied to any igneous
rock, which has a high proportion of pyroxene and olivine,
such that it’s colour index is between 50 and 90 (i.e.
dark). |
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Magnetic anomaly |
Zone where the magnitude and/or orientation
of the earth’s magnetic field is notably higher or
lower than adjacent areas. |
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Magnetite |
A magnetic iron oxide mineral. |
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Metamorphism |
The process of changing the characteristics
of a rock in response to changes in temperature, pressure
or volatile content. |
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Microdiamonds |
Current practice in Australia defines
Microdiamonds as diamonds
which will pass through a screen with 0.4mm in size. |
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Mineable reserves |
A natural aggregate of one or more minerals
which, at a specified and place, may be mined and sold at
a profit, or from which some part may be profitably separated. |
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Materialization |
A natural aggregate of one or more minerals. |
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Mining Grade |
The quality of a mineral ore
after it has been mined and may reflect the effect of dilution
from wall rock. |
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Mining lease |
Rights granted, usually by a government
under specific legislation, to exploit a mineral subject
to certain conditions. |
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Open cut mining |
Mining in which large amounts of waste
rock are excavated at surface in order to extract materials
without sub-surface tinseling. |
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Ore |
A mineral or rock which can be worked
economically. |
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Ore body |
Accumulation of minerals, distinct from
the host rock, and rich enough in metal or commodity to
be worth commercial exploitation. |
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Ore grade |
The concentration of an element of interest
in a potentially mineable ore
deposit. |
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Outcrop |
The part of a rock formation, which is
exposed at the earth’s surface. |
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Oxidation |
The act or process of oxidizing. |
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Paleochannels |
Old, ancient or past stream channels
cut into the bedrock and which may be accompanied by remnant
alluvial deposits. |
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Pan |
A rotary dish used to separate and concentrate
the mineral being recovered from the other constituent minerals
of the ore being mined. |
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Parcel of Diamonds |
A group of many diamonds,
valued or sold as a group. |
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Petrology |
The study of rocks in general, including
their occurrence, field relations, origins and history,
and their mineralogy and textures. |
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Phlogopite |
A member of the mica group of minerals;
occurs in metamorphosed limestones
and less frequently in ultrabasic
igneous rocks. |
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Pitting |
The digging of a pit, in exploration,
sampling of alluvial sediments
by shallow trial pits. |
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Placer |
A surficial mineral deposit formed by
the mechanical concentration of mineral particles from weathered
debris. |
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Pluton |
General term for a body of intrusive
igneous rock irrespective
of its shape, size or composition. |
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Porphyritic |
Of or like smaller grained igneous
rocks with separate crystals of greater size. |
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Positive gravity anomaly |
Relatively elevated readings within a
gravity survey which measures variations in the gravitational
force across the earth’s surface. |
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Precambrian |
The geological time period extending
from formation of the earth to 600 million years before
the present. |
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Processing plant |
The chemical and, or, physical process
required to recover and concentrate the mineral being mined
into a sellable commodity. |
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Prospective area |
A possible area of valuable minerals
for mining, oil producing etc. |
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Proterozoic |
Rocks formed between 2,500 and 600 million
years ago. |
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Pseudomorph |
A secondary mineral, which has replaced
an earlier mineral but retained its shape. |
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Pyrope Garnet |
Member of the garnet group of minerals,
often mantle derived. |
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Radiometric dating |
The most precise method of dating rocks
in which the relative percentage of isotopes of a given
radioactive element are estimated. |
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Ramp |
Inclined shaft. |
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Recovery |
The percentage of the situ commodity
being mined for that is actually recovered after the beneficiation
process. |
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REE |
Rare Earth Elements, including cerium
and yttrium and others. |
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Residual enrichment |
The concentration of diamond
in-situ by the removal by weathering processes of other
constituent parts of its host rock. |
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Resistivity |
The electrical resistance per unit length
of a unit cross-sectional area of a material, can be measured
in geological materials. |
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Rock mechanics |
The study of the physical behavior of
rocks and the mechanics of rock structures. |
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Rutile |
A natural form of titanium dioxide, a
red-brown crystalline substance with a look of bright metal. |
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Sampling |
To take a small amount of a substance
as an example, for testing purposes etc. |
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Schist |
Any of a number of sorts of rocks having
a structure of thin parallel plates or leaves and a tendency
to become separated into them, formed from other rocks by
heat and pressure acting on certain materials. |
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Sediment |
Matter deposited by water or wind. |
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Serpentinised |
The process whereby the high temperature
primary ferromagnesian minerals in an igneous
rock undergo alteration to a member of the serpentine group
of minerals. |
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Shear Zone |
A region, narrow in comparison with its
length, within which rocks have undergone intense deformation. |
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Silcrete |
Deposit of the weathering zone, especially
in sub-tropical environments, which may ultimately develop
into a hardened mass. |
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Siltstone |
A fine-grained sedimentary
rock composed mainly of silt, intermediate in grain size
between sandstone and shale, lacking the fissility of the
latter. |
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Statabound |
Said of a mineral deposit confined to
a single stratigraphic unit. |
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Spectrometry |
Measuring the natural radio-activity
of rocks; This radio-activity is due to potassium, thorium
and uranium, contained in the rocks; an airborne spectrometric
survey measures the radio-activity due to potassium, thorium
and uranium in the rocks and as a consequence gives some
information about the composition of the rocks. |
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Sortex machine |
Mechanical device, which produced the
final concentrate of diamonds and the associated heavy minerals
by use of x-ray. |
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Strike |
The lineament of a geologic structure
measure at 90 to its steepest altitude. |
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Structurally-hosted |
Said of mineral deposits
that are contained in geologic structures like faults
or folds. |
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Sub-parallel / vertical |
"Nearly" parallel, "nearly"
vertical. |
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Sulphide |
Minerals consisting of a chemical combination
of sulfur with a metal. |
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Surface mining |
Mining from surface of materials without
sub-surface tinseling. |
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Tectonic |
Deformation with the earth’s crust. |
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Terrace (alluvial) |
Sediments
(sand with gravel) laid down
by older (10,000 to million years ago) rivers and visible
as flattened areas a few metres above the present river
level. |
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Tertiary |
First sub-era of the Cenozoic
Era, which began about 65 Ma ago and lasted approximately
63 Ma. |
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TMI |
Total Magnetic Intensity, refers to the
total magnitude of the intensity of the earth’s magnetic
field. |
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Trenching |
The process of locating the position
of a dyke by digging trenches
perpendicular to its expected strike. |
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Tuff |
The compacted (lithified) equivalent
of a volcanic ash deposit. |
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Ultrabasic |
An igneous
rock that consists of ferromagnesian minerals and possesses
no free quartz, and with less than 45% silica. |
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Ultramafic |
See Ultrabasic. |
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UTM |
Universal Transverse Mercator; a map
grid reference system. |
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Volcanogenic |
Formed by processes directly connected
with volcanism. |
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Water table |
The upper surface of ground water, or
the level below which an unconfined aquifer is permanently
saturated with water. |
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Weathered |
Having undergone the processes of chemical
and physical change caused in rock exposed to the operation
of air, rain, ice, snow, ground water, the sun’s rays,
and so on. |
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Xenolith |
An inclusion
of a pre-existing rock in an igneous
rock, often derived from the country
rocks that have been intruded through. |
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X-ray Diffraction Analysis |
Laboratory technique used to identify
minerals using X-rays. |
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1VD |
First vertical derivative refers to a
particular processing of total magnetic intensity data to
highlight certain features in the data. |
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