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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

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