Prospectus - Kingsrose Mining

Conduits
Conglomerate
Country rock
Craton
Cumulate
Deformation
Deposition
Diamond drilling
Diorite
Dip
Displacement
Disseminated
Distal
DoIRE
Dolerite
Down dip
Dragfold
Drainage
Dyke
EL(A)
Electromagnetic survey
(EM)
EM
Epidote
Epigenetic
Epithermal
Extrusive
Facies
Fault
Feldspar
Felsic
Fold
Foliation
Fracturing
g/t
Gabbro
Galena
Channelways.
A sedimentary rock containing large rounded rock fragments.
The enclosing rock around a body of ore.
A relatively immobile part of the earth’s crust, generally of a large size.
Rocks in layered igneous intrusions which appear to have formed by the
accumulation of crystals.
Process by which rocks are folded or faulted.
The precipitation of mineral matter from solution.
Method of obtaining a cylindrical core of rock by drilling with a diamond
impregnated bit.
Coarse-grained intrusive rock of intermediate composition.
The angle at which layered rocks, foliation, a fault, or other planar structures, are
inclined from the horizontal.
Relative movement of the two sides of a fault.
Mineral grains scattered throughout host rock.
Sediments formed far from the source area.
Department of Industry, Resources and Environment
Medium-grained crystalline basalt.
Direction which is most likely downwards on a lithological structure or surface.
Any fold that is a subsidiary part of a large fold.
The process of discharge of water from an area by stream or sheet flow and
removal of excess water from soil by downward flow.
Tabular igneous intrusion cutting across the bedding or other planar structures in
the country rocks.
Exploration licence (application).
Method of measuring the alternate magnetic fields associated with electrical
currents artificially or naturally maintained in the subsurface.
Electromagnetic survey.
Calcium aluminium silicate mineral.
A mineral deposit formed later than the enclosing rock.
Mineral deposit formed in faults and fractures, mainly in volcanic rocks within
about 1km of the Earth’s surface, from low temperature hydrothermal fluids.
Igneous rocks that have flowed out onto the Earth’s surface.
The general appearance or nature of one part of rock body as contrasted with
other parts.
A fracture in rocks along which rocks on one side have been moved relative to
the rocks on the other. The movement may provide a channel for the passage of
mineral bearing solutions.
A very abundant group of rock-forming silicate minerals in which calcium,
sodium and potassium are in combination with aluminium.
Fine grained igneous rocks with a very low content of mafic minerals.
A bend in rock strata.
Laminated structure in rocks resulting from the parallelism of the constituent
minerals or by segregation of different minerals into layers.
Natural or induced breaks in a rock which enhance its reservoir properties.
Grams per tonne – measure of gold content of rock or sample.
Coarse grained dark igneous rock of similar composition to basic volcanics.
Lead sulphide mineral.
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