Mining_Methods_UnderGround_Mining - Mining and Blasting
Mining_Methods_UnderGround_Mining - Mining and Blasting
Mining_Methods_UnderGround_Mining - Mining and Blasting
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geOlOgy FOr <strong>Mining</strong><br />
geology for underground mining<br />
importance of<br />
geology<br />
A thorough underst<strong>and</strong>ing of the<br />
geology of a mineral deposit is<br />
fundamental to its successful<br />
exploitation, <strong>and</strong> this is especially<br />
important for underground working.<br />
As such, geology is a vital<br />
factor in the correct selection of<br />
mining method <strong>and</strong> equipment.<br />
Once a mining method is chosen,<br />
a major variance in the geology<br />
may make it difficult to change<br />
the approach to mining, compared<br />
to more flexible opencast<br />
work. This chapter reviews some<br />
of the important basic aspects of<br />
geology that may affect decisions<br />
about mining method. Atlas<br />
Copco offers a full range of drilling<br />
products for site investigation,<br />
<strong>and</strong> for mine development<br />
<strong>and</strong> production. 1. Recent alluvium, lake <strong>and</strong><br />
sea-bed deposits e.g.<br />
mud, s<strong>and</strong>s, calcite.<br />
2. Orebodies, e.g. containing<br />
The earth’s crust<br />
The earth’s crust consists of a variety<br />
of rocks, formed under different circumstances,<br />
<strong>and</strong> with a wide variety of<br />
properties. Rocks usually consist of one<br />
or more minerals, ranging from single<br />
chemical elements to complex compounds.<br />
There are known to be more<br />
than 3,000 different minerals.<br />
Of the 155 known elements, some of<br />
which do not occur naturally, oxygen<br />
is by far the most common, making<br />
up about 50% of the earth’s crust by<br />
weight. Silicon forms about 25%, <strong>and</strong><br />
the other common elements such as aluminium,<br />
iron, calcium, sodium, potassium,<br />
magnesium <strong>and</strong> titanium build up<br />
the total to 99% of the earth’s crust.<br />
Silicon, aluminium <strong>and</strong> oxygen occur<br />
in the commonest minerals such as<br />
quartz, feldspar <strong>and</strong> mica, which form<br />
part of a large group known as silicates,<br />
being compounds of silicic acid<br />
<strong>and</strong> other elements. Amphiboles <strong>and</strong> py-<br />
roxenes contain aluminium, potassium<br />
<strong>and</strong> iron. Some of the earth’s commonest<br />
rocks, granite <strong>and</strong> gneiss, are composed<br />
of silicates.<br />
galena, sphalerite,<br />
chalcopyrite <strong>and</strong> pyrite.<br />
3. Weathered shale, perhaps<br />
forming bauxite.<br />
4. Weathered s<strong>and</strong>stone, perhaps<br />
having high quartz content.<br />
Oxygen also occurs commonly in<br />
combination with metallic elements,<br />
which are often important sources for<br />
mining purposes. These compounds<br />
can form part of oxidic ores, such as<br />
the iron ores magnetite <strong>and</strong> hematite.<br />
Sulphur also readily combines with<br />
metallic elements to form sulphide ores,<br />
including galena, sphalerite, molybdenite<br />
<strong>and</strong> arsenopyrite.<br />
Other large mineral groups important<br />
in mining include halogenides such<br />
as fluorite <strong>and</strong> halite, carbonates such<br />
as calcite, dolomite <strong>and</strong> malachite, sulphates<br />
such as barite, tungstates such<br />
as scheelite, <strong>and</strong> phosphates such as<br />
apatite.<br />
Rarely, some elements can occur na-<br />
turally without combination. The important<br />
ones are the metals gold, silver<br />
<strong>and</strong> copper, plus carbon as diamonds<br />
<strong>and</strong> graphite.<br />
5. Weathered orebodies producing<br />
azurite, malachite, cuprite, etc.<br />
6. River valley deposits may include<br />
gold, platinum, diamonds,<br />
cassiterite or magnetite, as<br />
well as clays <strong>and</strong> s<strong>and</strong>s.<br />
7. Volcanic rocks – fine-grained<br />
minerals including feldspar,<br />
quartz, olivine, hornblende,<br />
magnetite <strong>and</strong> mica.<br />
Minerals<br />
8. Metamorphic s<strong>and</strong>stone<br />
– high proportion of quartz.<br />
9. Metamorphic limestone as<br />
marble, etc – calcite <strong>and</strong> dolomite.<br />
10. Metamorphic shales as<br />
slates, schists, etc. – with<br />
garnet, mica, feldspar.<br />
11. Contact zones between<br />
igneous <strong>and</strong> ‘country’ rocks –<br />
garnet, hornblende, sulphides.<br />
In some circumstances, the properties<br />
of individual minerals can be impor-<br />
tant to the means of mining, <strong>and</strong> will<br />
certainly be important for the means<br />
of extraction of the materials to be exploited.<br />
More often, however, minerals<br />
will be mixed with others to form the<br />
various types of rocks, <strong>and</strong> the pro-<br />
perties will be combined to form both<br />
homogenous <strong>and</strong> heterogeneous struc-<br />
tures. Feldspar accounts for almost<br />
50% of the mineral composition of<br />
the earth’s crust. Next come the pyrox-<br />
ene <strong>and</strong> amphibole minerals, closely<br />
followed by quartz <strong>and</strong> mica. These<br />
minerals all make up about 90% of the<br />
composition of the earth’s crust.<br />
Minerals have a wide variety of properties<br />
that can be important in their<br />
usefulness to man, <strong>and</strong> to the best way<br />
underground mining methods 7