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Introduction to Mining Geology
Hassan Z. Harraz
hharraz2006@yahoo.com
2010- 2011
This material is intended for use in lectures, presentations and as
handouts to students, and is provided in Power point format so as to
allow customization for the individual needs of course instructors.
Permission of the author and publisher is required for any other usage.
Please see hharraz2006@yahoo.com for contact details.
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Acknowledgments:
I acknowledge gratefully the extent to which I have leant on the work
contained in several good text books:
Introductory Mining Engineering, 2nd Edition, Howard Hartman and
Jan Mutmansky, 2007. John Wiley & Sons, Inc. 584p.
Surface and underground excavations: methods, techniques &
equipment, by Tatiya, R.R., 2005. A.A. Bakema, 579p.
Mining and the Environment: From Ore to Metal, by Karlheinz Spitz
and John Trudinger, 2009. CRC Press, Leiden.
Mine Wastes: Characterization, Treatment and Environmental
Impacts, 2nd Edition, by Bernd Lottermoser, 2007. Springer, Berlin
Heidelberg.
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Topic 1: Ore mineralogy and orebodies
Topic 2: Topic 2: The Mining Cycle
Topic 3: Mineral Resource and Reserve
Topic 4: Mining Methods
Topic 5: Mining Methods- Part I-Surface mining
Topic 6: Mining Methods-Part II: Surface Mining-Planning and Design of Open Pit
Mining
Topic 7: Mining Methods- Part III: Surface mining- Placer Mining
Topic 8: Mining Methods- Part IV: In-Situ Leaching (ISL)/ Solution Mining
Topic 9: Mining Methods- Part V- Underground Mining
Topic 10: Ore processing and metal recovery
Topic 11: Mine wastes
Topic 12: Environmental and social concerns
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
OUTLINE OF LECTURES:
An Introduction to Mining and Mineral Processing is to
geologists.
This course provides a non-technical introduction to the
basic concepts of:
Introduction
 Mineral exploration,
 Ore extraction,
 Mineral processing,
 Mine waste management
 With numerous examples, figures and images of mining.
 Also included are some key aspects of the economics of a
mining and mineral processing operation and some ideas about
the future of mining.
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Topic 1: Concepts of an Ore Deposit
2010- 2011
by
Hassan Z. Harraz
hharraz2006@yahoo.com
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
We will explore all of the above in Topic 1.
Outline of Topic 1:
 INTRODUCTION
 What is mining?
 Why do we need mines?
 What is a mineral ?
 What is an Ore Deposit?
 Concentrations of Metals
 Metals enrichment factors
 Types of Ore Deposit
 GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS:
1) Shape of ore deposits
2) Dip ore deposits
3) Thickness ore deposits
4) Depth of ore deposits
5) Structure of ore deposits
6) Ore value and profitability of mining
7) Stability of ore rocks
8) Chemical and mineral characteristics of ores
9) Lessening of ore deposit
10)Degree of breakability
 Life Cycle of a Metal Resource
 Mineral Supply and Demand
 Conservation
 Economic Impact on Mineral Supplies
2 February 2016 Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Mining Geology
• This is one of three employment centers for
geologists, and it is presently enjoying a
boom. The other boom employers are:
• The Petroleum Industry
• The Environmental Industry
7
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Modern safety standards mean that most modern mines, at least those
constructed by large corporations, are engineering marvels. They are
expensive, and are not constructed unless the commodity sought is known
to be present in profitable quantities and is recoverable.
Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
82 February 2016
What its all about!
Gold Bullion
9
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
What is mining?
Mining
The activity that removes
from the earth’s crust the
abnormal concentration of
metal found in the deposit
Mining is extracting ore or
minerals from the ground
10
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Mine
An opening or excavation of
the earth from which minerals are
extracted
Why do we need mines?
• Houses
• Cars
• Toothpaste
• Plumbing
• Wiring
• Planes
• Electronics
• Jewelry
• Glass
If we can’t grow it,
it has to be mined!
11
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
http://en.wikipedia.org/wiki/File:Pyrite_foolsgold.jpg
The mineral pyrite
(FeS2) in its
characteristic
cubic crystal form
Mineral is a solid naturally-occurring compound having a
definite chemical composition which under the
present technological can be extracted.
What is a mineral ?
Chalcopyrite
(CuFeS2)
http://en.wikipedia.org/wiki/File:chalcopyrite.jpg
12
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
Ore is a natural material with a high concentration of economically valuable
minerals that can be mined for a profit
2 February 2016
What is an Ore Deposit?
Ore deposits may be considered as:
Ore deposit is an occurrence of minerals or metals in
sufficiently high concentration to be profitable to mine
and process using current technology and under
current economic conditions.
Commercial mineral deposits (i.e., Ore: suitable for mining
in the present times) or
non-commercial ore deposits (i.e., Protore: problems in
mining, transportation, prices....etc).
13
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
What is Ore Grade?
Ore grade is the concentration of economic mineral
or metal in an ore deposit.
Weight percentage (wt.%)Base metals
grams/tonne
oz/ton
ppm
Precious metals
( gold, silver, platinum)
Grade units
14
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Concentrations of Metals
Earth is a big planet
 The crust is the outer 20 km of earth.
 It is underlain by the mantle which is about 3000 km thick.
 The mantle is underlain by the earth's core which is about 3400 km thick.
 The radius of the Earth is about 6500 km.
 We have mined as only as deep as 2 km !!!!
By comparison, the crustal concentration of silicon is 28% and that of oxygen is 46%.
15
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Metal
In Earth's crust concentration
(Clarke)
In Ore Deposit Typical Grade
(wt.%) (ppm) (wt.%) (ppm)
Aluminum 8.0 80,000 47 470,000
Iron 6.3 63,000 62 620,000
Copper 0.005 50 0.4 - 1 4,000 -10,000
Nickel 0.008 80 1.22 12,200
Zinc 0.0062 62 7.1 71,000
Uranium 0.00025 2.5 0.1 – 20 1,000- 200,000
Lead 0.00126 12.6 5 50,000
Silver 0.0000063 0.063 0.021 210
Gold 0.0000004 0.004 0.0001 - 0.0005 1 – 5
Molybdenum 0.000016 1.6 0.21 2,100
1 ppm = 1 part per million.
1 ppm = 0.0001% = 1 gram/tonne
These relationships are illustrated by a plot of the data in Figure 2 below.
The grade of a typical gold deposit is of the order of thousands of times greater than the
average concentration of gold in the earth's crust.
In contrast, the grade of an iron deposit is only 10 times greater.
16
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Figure 6. Orebody and crustal concentrations - if we were happy with average concentrations in the
crust, all orebodies would line up along the y = x line.
(Note the logarithmic scale - one large division equals one order of magnitude, i.e multiply by 10)
17
Iron and aluminum are
abundant in crust - not
much concentration is
needed.Gold and silver
are not abundant
- lots of
concentration is
needed, more
than one order of
magnitude.
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Metals enrichment factors
Metals require significant enrichment above their
normal background levels in the Earth’s crust to form
a mineable orebody.
Minerals are enriched to form orebodies through a wide
range of different geological processes.
The enrichment factor required to make a mine viable
(i.e., profitable – within today’s economic framework
for minerals exploitation) will vary from time to time,
depending on commodity prices, and the ease of
extraction of both the orebody from the ground and
the target metal from the orebody.
 The concentrations of metals in ore deposits depends
on the current price of the metal since ore is what
can be mined under current economic conditions.
 Thus, as price goes up, the concentration of metal
required to make rock an ore deposit, goes down.
Figure from Spitz and Trudinger, 2009.
18
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Useful metals come from rocks and
minerals in the Earth’s crust.
Galena sample – a main ore of lead. Image: Stonetrust, Inc.
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
19
Types of Ore Deposit
There are several types of ore deposits:
 Magmatic: crystallization of minerals within a body. of magma
 Hydrothermal: hot fluids released as magma cools, minerals
precipitate from fluids.
 Sedimentary: precipitation of minerals from a lake or ocean water
 Placer deposits: deposition of metals in a river or stream (causing
people to pan for them).
 Residual: concentrations of minerals produced by weathering and
chemical reactions with oxygen and water.
This is a very broad classification. There are many sub-types and even
more types - nature provides much complexity.
20
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
21
GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS
1) Shape of ore deposits
2) Dip ore deposits
3) Thickness ore deposits
4) Depth of ore deposits
5) Structure of ore deposits
6) Ore value and profitability of mining
7) Stability of ore rocks
8) Chemical and mineral characteristics of ores
9) Lessening of ore deposit
10) Degree of breakability
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Parameters for dip, depth, thickness and geometry of deposits (source SME Min.
Eng. Handbook, 3ed., 2011) :
According to shape features, ore deposits can be classified into three groups as follows:
i. Isometrical group: stock, nests, irregular shapes but their dimensions in space do not differ
greatly,...etc.
ii. Tabular Groups
iii. Columnar group: extend in one direction, like; veins, layer, bed, seam, sheet, lenses,
iv. Impregnation or disseminated ore group
22
1) Shape of ore deposits:-
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
2) Dip ore deposits
Class Dip Rock Strength Bulk Handling Mode
Flat ≤ 20° Weak rock (surficial) Use mobile equipment (or conveyors)
Inclined 20 - 45° Average rock Use slashers (metal plate can also vibrate – as
gravity slides)
Steep ≥45° Strong rock (at depth) Gravity flow of bulk solids
Tabular deposits classified by dip and related to handling and rock strength as
follows:
3) Thickness ore deposits
according to amounts of thickness of ore body, the
deposits can be classified into:
23Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Class Deposit Thickness (m) Comments
Coal Ore
Tabular deposit
Thin
≤0.9 - 1.2 ≤0.9 - 1.8 Low profile or narrow mine
equipment
Medium 1.2 – 2.4 1.8 – 4.6 Past and Stulls ≤3.1 m
Thick
2.4 – 4.6 4.6 – 5.3 Small surface equipment;
crib problems
Massive (Very
thick)
>4.6 >5.3 Pillar problems or poor
recovery, benching
necessary; caving
considered
4) Depth of ore deposits:
2 February 2016 Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
24
Deposit Depth (m)
Underground
(a measure of overburden pressure)
Class Coal Ore Surface
Shallow ≤61
Slope Entries possible
3≤05 ≤61
Moderate 122 – 244
Pillar problems
305 - 457 61 -305
Deep ≥915
Bumps, Burst, Closure
≥1830 ≥305 – 915
Open pit
Deposits classified by depth into:-
5) Structure of ore deposits
according to structure of ore body, the deposits can be
classified into:-
I. Massive ore.
II. Laminated ore.
III. Jointed ore.
IV. Loose ore.
25
Depend on Lumpiness of broken ore (i.e., size
of lumps obtained on breaking parts), ore may
be divided into:
a) Fine size ores Dust to lumps (<100 mm)
b) Medium size ores 100 -300 mm
c) Large size ores 300 - 600 mm
d) Very large size ores >600 mm
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
6) Ore value and profitability of mining
according to relative value of assay, the deposits
can be classified into:
I. Rich ore
II. Medium ore.
III. Lean ore (Uneconomic): Only extracted by
cheapest techniques like hand methods.
26
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
7) Stability of ore rocks
Stability is ability of massif to resist caving for a certain period
of time.
The stability of ore rocks is usually depending on
amounts of joints and laminations in the ore rocks as
well as hardness of the ore rocks.
Therefore, the ore rocks may be divided into:-
I. Very unstable ore rock (like friable sandstones)
II. Unstable ore rock.
III. Medium ore rock.
IV. Stable ore rock.
V. Very stable ore rock.
27
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
8) Chemical and mineral characteristics of ores
I. Native ores
II. Noble metals.
III. Sulphide ores: chalcopyrite (CuFeS2), Galena (PbS), pyrite
(FeS), sphalerite (ZnS), stibnite (Sb2S3), and molybdnite
(MoS2).
IV.Oxidized ores: Hematite (Fe2O3), Magnetite (Fe3O4),
Goethite (Fe2O3.nH2O), (MnO2), Cuprite (CuO2), Cassiterite
(SnO2), and Chromite (FeCrO3).
V. Silicate ores: Zircon (ZrSiO4) and Beryl (Al2Be3Si6O8).
28
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
9) Lessening of ore deposit
I. Oxidation (iron deposit, sulphide deposits)
II. Caking (Mn deposits)
III. Self ignition (Sulphur, coal)
29
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
10) Degree of breakability
• According to its breakability, every rock falls into one of the following five groups:
• Friable and flowing (ex. sand, peat, topsoil);
• Soft (like. Clay);
• Brittle (ex. Sandstone, limestone, shale, coal);
• Strong (ex. granite, magnetite);
• Very strong (ex. quartzite, diabase, porphyry).
30
Breakability is the resistance of a rock parts to separation
from the mass.
The choice of the proper method of breaking ground depends first of all on the degree of
breakability of the rock.
The following properties of rock must be distinguished:
i) Hardness: the resistance to penetration by a pointed tool;
ii) Strength,
iii) Toughness: the resistance of the mass to the separation of pieces from it;
iv) Elasticity or resilience: the resistance to impact.
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
31
For classifying a rock in one of the last three groups, no strict
criteria exist, therefore the classification suffers from a high degree of
subjectivity, the more so as the properties of a rock can be vary with its
structure (fissuring, foliation) and condition (weathering).
In this classification, a standard classification of rocks according to their
amenability to drilling and blasting.
The reason for this classification is that drilling and blasting are
very widely used in mining and yet many investigations have found no
direct correlation between hardness or strength and the amenability of a
rock to drilling and blasting.
In this classification, the amenability to drilling is evaluated by
the speed of pure drilling in mm/minute and by the time of drilling 1 m of
hole.
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
2 February 2016
Conversion
to product
Surface
mining Metal ore Separation
of ore from
gangue
Smelting Melting
metal
Discarding
of product
Recycling
Life Cycle of a Metal Resource
Smelting : heating to release metals but creating air polluting by-products
Chemical removal processes such as using cyanide to remove gold can
create Toxic holding ponds
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
32
Mining Ore
A) Ore has two components: gangue(waste) and desired
metal.
B) Separation of ore and gangue which leaves tailings.
C) Smelting (air and water pollution and hazardous waste
which contaminates the soil around the smelter for
decades).
D) Melting Metal.
E) Conversion to product and discarding product.
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
33
Life Cycle of Metal Resources (fig. 14-8)2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
34
Mineral Supply and Demand
 World Scenario:
 Assumptions:
 Present demand = present production
 Future projection is based on constant 1995 figures
 Unrestricted distribution
 Iron, Aluminum, Chromium, Cobalt and Platinum will last centuries
 Copper, Lead, Zinc, Gold and Silver will last several decades only
 Ditto for phosphates and sulfur
 Alleviating Factors:
 More exploration
 Better technology
 Reclassification of sub-economic resources to reserve
 Reduce consumptions:
 Smaller households, more leisure and travel, convenience, status etc. make it unlikely
even in developed economies.
 New technology adds to the existing needs e.g., cellular phones, computers, microwave
oven.
 In the US, population grew by 65% and consumption grew by 130% between 1950-1990.
 Great demand for resources in the developing countries where there is a genuine need
and where the great majority lives.
 If demand cannot be reduced, supplies must be increased or extended.
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
35
Conservation
Substitution:
 Increases consumption of the substituting metal or nonmetal
(often petroleum) which itself might be limited in amount
Recycling:
 In USA 60% of lead, 40% of copper, 1/3rd of nickel and almost ¼
of Al, Cr, Co and Zn is recycled
 Recycled Al requires 20 times less energy than new Al
 Difficult to do with finished products like cars or fridges
 Special problem with alloys
 Road salt, fertilizers, lead in gasoline gets too disperse
 Reduces waste disposal problem
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
36
Economic Impact on Mineral Supplies
A) Mineral prices are low because of subsidies: depletion allowances and deduct cost of
finding more.
B) Mineral scarcity does not raise the market prices.
C) Mining Low Grade Ore: Some analysts say all we need to do is mine more low grade
ores to meet our need:
1) We are able to mine low grade ore due to improved technology.
2) The problem is cost of mining and processing, availability of fresh water,
environmental impact.
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
37
Present Depletion
time A
Depletion
time B
Depletion
time C
Time
Production
C
B
A
Recycle, reuse, reduce
consumption; increase
reserves by improved
mining technology,
higher prices, and
new discoveries
Recycle; increase reserves
by improved mining
technology, higher prices,
and new discoveries
Mine, use, throw away;
no new discoveries;
rising prices
Fig. 14.9, p. 329
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
38
Fig. 14.10, p. 329
2 February 2016
Prof. Dr. H.Z. Harraz Presentation
Mining Geology, Introduction
39

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Introduction to Mining Geology

  • 1. Introduction to Mining Geology Hassan Z. Harraz hharraz2006@yahoo.com 2010- 2011 This material is intended for use in lectures, presentations and as handouts to students, and is provided in Power point format so as to allow customization for the individual needs of course instructors. Permission of the author and publisher is required for any other usage. Please see hharraz2006@yahoo.com for contact details. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
  • 2. Acknowledgments: I acknowledge gratefully the extent to which I have leant on the work contained in several good text books: Introductory Mining Engineering, 2nd Edition, Howard Hartman and Jan Mutmansky, 2007. John Wiley & Sons, Inc. 584p. Surface and underground excavations: methods, techniques & equipment, by Tatiya, R.R., 2005. A.A. Bakema, 579p. Mining and the Environment: From Ore to Metal, by Karlheinz Spitz and John Trudinger, 2009. CRC Press, Leiden. Mine Wastes: Characterization, Treatment and Environmental Impacts, 2nd Edition, by Bernd Lottermoser, 2007. Springer, Berlin Heidelberg. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
  • 3. Topic 1: Ore mineralogy and orebodies Topic 2: Topic 2: The Mining Cycle Topic 3: Mineral Resource and Reserve Topic 4: Mining Methods Topic 5: Mining Methods- Part I-Surface mining Topic 6: Mining Methods-Part II: Surface Mining-Planning and Design of Open Pit Mining Topic 7: Mining Methods- Part III: Surface mining- Placer Mining Topic 8: Mining Methods- Part IV: In-Situ Leaching (ISL)/ Solution Mining Topic 9: Mining Methods- Part V- Underground Mining Topic 10: Ore processing and metal recovery Topic 11: Mine wastes Topic 12: Environmental and social concerns Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction OUTLINE OF LECTURES:
  • 4. An Introduction to Mining and Mineral Processing is to geologists. This course provides a non-technical introduction to the basic concepts of: Introduction  Mineral exploration,  Ore extraction,  Mineral processing,  Mine waste management  With numerous examples, figures and images of mining.  Also included are some key aspects of the economics of a mining and mineral processing operation and some ideas about the future of mining. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
  • 5. Topic 1: Concepts of an Ore Deposit 2010- 2011 by Hassan Z. Harraz hharraz2006@yahoo.com Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
  • 6. We will explore all of the above in Topic 1. Outline of Topic 1:  INTRODUCTION  What is mining?  Why do we need mines?  What is a mineral ?  What is an Ore Deposit?  Concentrations of Metals  Metals enrichment factors  Types of Ore Deposit  GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS: 1) Shape of ore deposits 2) Dip ore deposits 3) Thickness ore deposits 4) Depth of ore deposits 5) Structure of ore deposits 6) Ore value and profitability of mining 7) Stability of ore rocks 8) Chemical and mineral characteristics of ores 9) Lessening of ore deposit 10)Degree of breakability  Life Cycle of a Metal Resource  Mineral Supply and Demand  Conservation  Economic Impact on Mineral Supplies 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
  • 7. Mining Geology • This is one of three employment centers for geologists, and it is presently enjoying a boom. The other boom employers are: • The Petroleum Industry • The Environmental Industry 7 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction
  • 8. Modern safety standards mean that most modern mines, at least those constructed by large corporations, are engineering marvels. They are expensive, and are not constructed unless the commodity sought is known to be present in profitable quantities and is recoverable. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 82 February 2016
  • 9. What its all about! Gold Bullion 9 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 10. What is mining? Mining The activity that removes from the earth’s crust the abnormal concentration of metal found in the deposit Mining is extracting ore or minerals from the ground 10 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction Mine An opening or excavation of the earth from which minerals are extracted
  • 11. Why do we need mines? • Houses • Cars • Toothpaste • Plumbing • Wiring • Planes • Electronics • Jewelry • Glass If we can’t grow it, it has to be mined! 11 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 12. http://en.wikipedia.org/wiki/File:Pyrite_foolsgold.jpg The mineral pyrite (FeS2) in its characteristic cubic crystal form Mineral is a solid naturally-occurring compound having a definite chemical composition which under the present technological can be extracted. What is a mineral ? Chalcopyrite (CuFeS2) http://en.wikipedia.org/wiki/File:chalcopyrite.jpg 12 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction Ore is a natural material with a high concentration of economically valuable minerals that can be mined for a profit 2 February 2016
  • 13. What is an Ore Deposit? Ore deposits may be considered as: Ore deposit is an occurrence of minerals or metals in sufficiently high concentration to be profitable to mine and process using current technology and under current economic conditions. Commercial mineral deposits (i.e., Ore: suitable for mining in the present times) or non-commercial ore deposits (i.e., Protore: problems in mining, transportation, prices....etc). 13 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 14. What is Ore Grade? Ore grade is the concentration of economic mineral or metal in an ore deposit. Weight percentage (wt.%)Base metals grams/tonne oz/ton ppm Precious metals ( gold, silver, platinum) Grade units 14 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 15. Concentrations of Metals Earth is a big planet  The crust is the outer 20 km of earth.  It is underlain by the mantle which is about 3000 km thick.  The mantle is underlain by the earth's core which is about 3400 km thick.  The radius of the Earth is about 6500 km.  We have mined as only as deep as 2 km !!!! By comparison, the crustal concentration of silicon is 28% and that of oxygen is 46%. 15 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 16. Metal In Earth's crust concentration (Clarke) In Ore Deposit Typical Grade (wt.%) (ppm) (wt.%) (ppm) Aluminum 8.0 80,000 47 470,000 Iron 6.3 63,000 62 620,000 Copper 0.005 50 0.4 - 1 4,000 -10,000 Nickel 0.008 80 1.22 12,200 Zinc 0.0062 62 7.1 71,000 Uranium 0.00025 2.5 0.1 – 20 1,000- 200,000 Lead 0.00126 12.6 5 50,000 Silver 0.0000063 0.063 0.021 210 Gold 0.0000004 0.004 0.0001 - 0.0005 1 – 5 Molybdenum 0.000016 1.6 0.21 2,100 1 ppm = 1 part per million. 1 ppm = 0.0001% = 1 gram/tonne These relationships are illustrated by a plot of the data in Figure 2 below. The grade of a typical gold deposit is of the order of thousands of times greater than the average concentration of gold in the earth's crust. In contrast, the grade of an iron deposit is only 10 times greater. 16 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 17. Figure 6. Orebody and crustal concentrations - if we were happy with average concentrations in the crust, all orebodies would line up along the y = x line. (Note the logarithmic scale - one large division equals one order of magnitude, i.e multiply by 10) 17 Iron and aluminum are abundant in crust - not much concentration is needed.Gold and silver are not abundant - lots of concentration is needed, more than one order of magnitude. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 18. Metals enrichment factors Metals require significant enrichment above their normal background levels in the Earth’s crust to form a mineable orebody. Minerals are enriched to form orebodies through a wide range of different geological processes. The enrichment factor required to make a mine viable (i.e., profitable – within today’s economic framework for minerals exploitation) will vary from time to time, depending on commodity prices, and the ease of extraction of both the orebody from the ground and the target metal from the orebody.  The concentrations of metals in ore deposits depends on the current price of the metal since ore is what can be mined under current economic conditions.  Thus, as price goes up, the concentration of metal required to make rock an ore deposit, goes down. Figure from Spitz and Trudinger, 2009. 18 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 19. Useful metals come from rocks and minerals in the Earth’s crust. Galena sample – a main ore of lead. Image: Stonetrust, Inc. 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 19
  • 20. Types of Ore Deposit There are several types of ore deposits:  Magmatic: crystallization of minerals within a body. of magma  Hydrothermal: hot fluids released as magma cools, minerals precipitate from fluids.  Sedimentary: precipitation of minerals from a lake or ocean water  Placer deposits: deposition of metals in a river or stream (causing people to pan for them).  Residual: concentrations of minerals produced by weathering and chemical reactions with oxygen and water. This is a very broad classification. There are many sub-types and even more types - nature provides much complexity. 20 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 21. 21 GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS 1) Shape of ore deposits 2) Dip ore deposits 3) Thickness ore deposits 4) Depth of ore deposits 5) Structure of ore deposits 6) Ore value and profitability of mining 7) Stability of ore rocks 8) Chemical and mineral characteristics of ores 9) Lessening of ore deposit 10) Degree of breakability Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016 Parameters for dip, depth, thickness and geometry of deposits (source SME Min. Eng. Handbook, 3ed., 2011) :
  • 22. According to shape features, ore deposits can be classified into three groups as follows: i. Isometrical group: stock, nests, irregular shapes but their dimensions in space do not differ greatly,...etc. ii. Tabular Groups iii. Columnar group: extend in one direction, like; veins, layer, bed, seam, sheet, lenses, iv. Impregnation or disseminated ore group 22 1) Shape of ore deposits:- Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016 2) Dip ore deposits Class Dip Rock Strength Bulk Handling Mode Flat ≤ 20° Weak rock (surficial) Use mobile equipment (or conveyors) Inclined 20 - 45° Average rock Use slashers (metal plate can also vibrate – as gravity slides) Steep ≥45° Strong rock (at depth) Gravity flow of bulk solids Tabular deposits classified by dip and related to handling and rock strength as follows:
  • 23. 3) Thickness ore deposits according to amounts of thickness of ore body, the deposits can be classified into: 23Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016 Class Deposit Thickness (m) Comments Coal Ore Tabular deposit Thin ≤0.9 - 1.2 ≤0.9 - 1.8 Low profile or narrow mine equipment Medium 1.2 – 2.4 1.8 – 4.6 Past and Stulls ≤3.1 m Thick 2.4 – 4.6 4.6 – 5.3 Small surface equipment; crib problems Massive (Very thick) >4.6 >5.3 Pillar problems or poor recovery, benching necessary; caving considered
  • 24. 4) Depth of ore deposits: 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 24 Deposit Depth (m) Underground (a measure of overburden pressure) Class Coal Ore Surface Shallow ≤61 Slope Entries possible 3≤05 ≤61 Moderate 122 – 244 Pillar problems 305 - 457 61 -305 Deep ≥915 Bumps, Burst, Closure ≥1830 ≥305 – 915 Open pit Deposits classified by depth into:-
  • 25. 5) Structure of ore deposits according to structure of ore body, the deposits can be classified into:- I. Massive ore. II. Laminated ore. III. Jointed ore. IV. Loose ore. 25 Depend on Lumpiness of broken ore (i.e., size of lumps obtained on breaking parts), ore may be divided into: a) Fine size ores Dust to lumps (<100 mm) b) Medium size ores 100 -300 mm c) Large size ores 300 - 600 mm d) Very large size ores >600 mm Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 26. 6) Ore value and profitability of mining according to relative value of assay, the deposits can be classified into: I. Rich ore II. Medium ore. III. Lean ore (Uneconomic): Only extracted by cheapest techniques like hand methods. 26 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 27. 7) Stability of ore rocks Stability is ability of massif to resist caving for a certain period of time. The stability of ore rocks is usually depending on amounts of joints and laminations in the ore rocks as well as hardness of the ore rocks. Therefore, the ore rocks may be divided into:- I. Very unstable ore rock (like friable sandstones) II. Unstable ore rock. III. Medium ore rock. IV. Stable ore rock. V. Very stable ore rock. 27 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 28. 8) Chemical and mineral characteristics of ores I. Native ores II. Noble metals. III. Sulphide ores: chalcopyrite (CuFeS2), Galena (PbS), pyrite (FeS), sphalerite (ZnS), stibnite (Sb2S3), and molybdnite (MoS2). IV.Oxidized ores: Hematite (Fe2O3), Magnetite (Fe3O4), Goethite (Fe2O3.nH2O), (MnO2), Cuprite (CuO2), Cassiterite (SnO2), and Chromite (FeCrO3). V. Silicate ores: Zircon (ZrSiO4) and Beryl (Al2Be3Si6O8). 28 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 29. 9) Lessening of ore deposit I. Oxidation (iron deposit, sulphide deposits) II. Caking (Mn deposits) III. Self ignition (Sulphur, coal) 29 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 30. 10) Degree of breakability • According to its breakability, every rock falls into one of the following five groups: • Friable and flowing (ex. sand, peat, topsoil); • Soft (like. Clay); • Brittle (ex. Sandstone, limestone, shale, coal); • Strong (ex. granite, magnetite); • Very strong (ex. quartzite, diabase, porphyry). 30 Breakability is the resistance of a rock parts to separation from the mass. The choice of the proper method of breaking ground depends first of all on the degree of breakability of the rock. The following properties of rock must be distinguished: i) Hardness: the resistance to penetration by a pointed tool; ii) Strength, iii) Toughness: the resistance of the mass to the separation of pieces from it; iv) Elasticity or resilience: the resistance to impact. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 31. 31 For classifying a rock in one of the last three groups, no strict criteria exist, therefore the classification suffers from a high degree of subjectivity, the more so as the properties of a rock can be vary with its structure (fissuring, foliation) and condition (weathering). In this classification, a standard classification of rocks according to their amenability to drilling and blasting. The reason for this classification is that drilling and blasting are very widely used in mining and yet many investigations have found no direct correlation between hardness or strength and the amenability of a rock to drilling and blasting. In this classification, the amenability to drilling is evaluated by the speed of pure drilling in mm/minute and by the time of drilling 1 m of hole. Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 2 February 2016
  • 32. Conversion to product Surface mining Metal ore Separation of ore from gangue Smelting Melting metal Discarding of product Recycling Life Cycle of a Metal Resource Smelting : heating to release metals but creating air polluting by-products Chemical removal processes such as using cyanide to remove gold can create Toxic holding ponds 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 32
  • 33. Mining Ore A) Ore has two components: gangue(waste) and desired metal. B) Separation of ore and gangue which leaves tailings. C) Smelting (air and water pollution and hazardous waste which contaminates the soil around the smelter for decades). D) Melting Metal. E) Conversion to product and discarding product. 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 33
  • 34. Life Cycle of Metal Resources (fig. 14-8)2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 34
  • 35. Mineral Supply and Demand  World Scenario:  Assumptions:  Present demand = present production  Future projection is based on constant 1995 figures  Unrestricted distribution  Iron, Aluminum, Chromium, Cobalt and Platinum will last centuries  Copper, Lead, Zinc, Gold and Silver will last several decades only  Ditto for phosphates and sulfur  Alleviating Factors:  More exploration  Better technology  Reclassification of sub-economic resources to reserve  Reduce consumptions:  Smaller households, more leisure and travel, convenience, status etc. make it unlikely even in developed economies.  New technology adds to the existing needs e.g., cellular phones, computers, microwave oven.  In the US, population grew by 65% and consumption grew by 130% between 1950-1990.  Great demand for resources in the developing countries where there is a genuine need and where the great majority lives.  If demand cannot be reduced, supplies must be increased or extended. 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 35
  • 36. Conservation Substitution:  Increases consumption of the substituting metal or nonmetal (often petroleum) which itself might be limited in amount Recycling:  In USA 60% of lead, 40% of copper, 1/3rd of nickel and almost ¼ of Al, Cr, Co and Zn is recycled  Recycled Al requires 20 times less energy than new Al  Difficult to do with finished products like cars or fridges  Special problem with alloys  Road salt, fertilizers, lead in gasoline gets too disperse  Reduces waste disposal problem 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 36
  • 37. Economic Impact on Mineral Supplies A) Mineral prices are low because of subsidies: depletion allowances and deduct cost of finding more. B) Mineral scarcity does not raise the market prices. C) Mining Low Grade Ore: Some analysts say all we need to do is mine more low grade ores to meet our need: 1) We are able to mine low grade ore due to improved technology. 2) The problem is cost of mining and processing, availability of fresh water, environmental impact. 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 37
  • 38. Present Depletion time A Depletion time B Depletion time C Time Production C B A Recycle, reuse, reduce consumption; increase reserves by improved mining technology, higher prices, and new discoveries Recycle; increase reserves by improved mining technology, higher prices, and new discoveries Mine, use, throw away; no new discoveries; rising prices Fig. 14.9, p. 329 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 38
  • 39. Fig. 14.10, p. 329 2 February 2016 Prof. Dr. H.Z. Harraz Presentation Mining Geology, Introduction 39