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GeometallurgicalGeometallurgicalGeometallurgicalGeometallurgical CharacterisationCharacterisationCharacterisationCharacterisation
and Representative Metallurgicaland Representative Metallurgicaland Representative Metallurgicaland Representative Metallurgical
Sampling at Xstrata Process SupportSampling at Xstrata Process SupportSampling at Xstrata Process SupportSampling at Xstrata Process Support
45nd Annual CMP Conference January 22-24, 2013
L. Kormos, J. Sliwinski, J. Oliveira, G. Hill
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• Xstrata Process Support would like to thank Carpathian Gold and AGP Mining for their support and permission to present this work
Acknowledgements
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• Definition of Geometallurgy
• Methodology
– Choosing Geometallurgical Units – Options
– Representative Sampling
– Quantitative Mineralogy
– Metallurgical Testing
• Case Study – Rovina Valley Project - Carpathian Gold
Summary
Definition
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A cross disciplinary approach in which metallurgical performance of an ore is linked to intrinsic geological and mineralogical characteristics
Objective is to create a robust flowsheet able to treat the full range in variability and develop production strategies that maximise financial performance
Geometallurgy
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1. Statistical approach utilising the assay database and geological variables
Benefit: robust methodology if extensive database is available
Risks:
• Exploration databases are often limited to paymetals but a geometallurgical unit definition requires understanding of gangue minerals
• Scoping and pre-feasibility studies take place prior to the availability of extensive data sets
• Purely statistical methods will produce multiple populations which can require extensive testing and validation prior to consolidation into a smaller number of composites for metallurgical testing
Methodologies used in Industry
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Methodology used in Industry
2. Use of ore mineralogy, geology and spatial distribution of geological and mineralogical features along with review of relevant metallurgical data to define geometallugicalunits. Use of supporting statistics to confirm discrete populations
Benefit:
• Can apply at early stages of a project
• Cost effective
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Methodology continued
Parameters used in assessment:
Grade
Grade ratios (polymetallic ores)
Lithology
Mineralogy
Alteration
Structure
Grain Size
Hardness
Presence of deleterious elements or minerals
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• Proper sampling is key to ensuring that results of the geometallurgical study will reflect future performance
• Random sampling is not always practical
– Requirement for very large samples when test program may need only a fraction of the mass
• Non-random sampling is effective way of matching characteristics of metallurgical test samples to larger sample population
– Grade and grade distribution
– Lithology/alteration distributions
– Spatially representative
Representative Sampling
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Mineralogical Characterisation
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• Mineralogical characterisation using quantitative mineralogy (XPS uses QEMSCAN and EPMA)
– Define in-situ grain sizes
Testwork Program
97
72
84
60
127
103
72 6859
121
56
160
3124
36
19
43
28
0
20
40
60
80
100
120
140
160
180
GEOMET 1 GEOMET 2 GEOMET 3 GEOMET 4 GEOMET 5 GEOMET 6
Gra
in S
ize
(µm
)
Average Grain Sizes (µm)
sph
cpy
gal
Mineralogical Characterisation
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• Mineralogical characterisation using quantitative mineralogy (XPS uses QEMSCAN and EPMA)
– Define in-situ grain sizes
– Modal mineralogy
Testwork Program
Minerals
Chalcopyrite
Bornite
Chalcocite
Pyrite
Enargite/Tetrahedrite
Jarosite
Tetrahedrite
Other Sulphides
Chlorite
Quartz
Muscovite
Fe Al Clay
Kaolinite
Pyrophyllite
Orthoclase
Plagioclase
Zunyite
Fe Ti Oxides
Mn Oxide
Diaspore
Alunite
Barite
Phosphates
Other
()
UGM3
UGM2
UGM1
UGM0
Mass (%)
0 20 40 60 80 100
Minerals
Chalcopyrite
Bornite
Chalcocite
Pyrite
Enargite/Tetrahedrite
Jarosite
Tetrahedrite
Other Sulphides
Chlorite
Quartz
Muscovite
Fe Al Clay
Kaolinite
Pyrophyllite
Orthoclase
Plagioclase
Zunyite
Fe Ti Oxides
Mn Oxide
Diaspore
Alunite
Barite
Phosphates
Other
()
UGM3
UGM2
UGM1
UGM0
Mass (%)
0 20 40 60 80 100
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Mineralogical Characterisation
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• Mineralogical characterisation using quantitative mineralogy (XPS uses QEMSCAN and EPMA)
– Define in-situ grain sizes
– Modal mineralogy
– Element deportments
Testwork Program
0%
20%
40%
60%
80%
100%
GEOMET 1 GEOMET 2
Ce DeportmentOther
Micas
Zircon
Apatite
Rutile/Ilmenite
Perovskite
Crichtonite
CaTiNb REE
Fe Synchysite
Synchysite0%
20%
40%
60%
80%
100%
GEOMET 1 GEOMET 2
Ce DeportmentOther
Micas
Zircon
Apatite
Rutile/Ilmenite
Perovskite
Crichtonite
CaTiNb REE
Fe Synchysite
Synchysite
Metallurgical Benchmarking
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• Use of same flowsheet, reagent suite and conditions so a direct comparison can be made between the geometallurgical units
• Flowsheet may be adjusted after the first phase, geometallurgical units are reviewed and may be consolidated prior to additional testing
Testwork Program
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Case Study:
Carpathian Gold
Geometallurgical Study
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Geometallurgical Study
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Rovina Valley Gold Copper Project
• Located in west central Romania
• Mining District known as Golden Quadrilateral
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Site Visit
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• Site visit to review geology, work with project geologists to come up with a list of 5 preliminary geometallurgical units
• Spatial distribution, lithology, alteration, grade, grade ratios were the main criteria used
• Previous metallurgical data reviewed
• Representative composites created
Geometallurgical Study
Total Population vs. Metallurgical Composite
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Representative Samples – Head Grade
6576
277
0
1000
2000
3000
4000
5000
6000
7000
Total Geomet Population
Geomet Subsample Composite
Core Intersections
6576
277
0
1000
2000
3000
4000
5000
6000
7000
Total Geomet Population
Geomet Subsample Composite
Core Intersections
0.790.82
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Total Geomet Population
Geomet Subsample Composite
Au Grade (ppm)
0.790.82
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Total Geomet Population
Geomet Subsample Composite
Au Grade (ppm)
1629 1673
0
200
400
600
800
1000
1200
1400
1600
1800
2000
Total Geomet Population
Geomet Subsample Composite
Cu Grade (ppm)
1629 1673
0
200
400
600
800
1000
1200
1400
1600
1800
2000
Total Geomet Population
Geomet Subsample Composite
Cu Grade (ppm)
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Total Population vs. Metallurgical Composite
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Representative Samples – Grade Distribution
0%
20%
40%
60%
80%
100%
0
10
20
30
40
50
60
70
80
Fre
qu
en
cy
Grade ppm
Au - Geomet Subsample Composite MET-27
0%
20%
40%
60%
80%
100%
0
10
20
30
40
50
60
70
80
Fre
qu
en
cy
Grade ppm
Au - Geomet Subsample Composite MET-27
0%
20%
40%
60%
80%
100%
0
200
400
600
800
1000
1200
Fre
qu
en
cy
Grade ppm
Cu - Total Geomet Population Ciresata Sediment
0%
20%
40%
60%
80%
100%
0
200
400
600
800
1000
1200
Fre
qu
en
cy
Grade ppm
Cu - Total Geomet Population Ciresata Sediment
0%
20%
40%
60%
80%
100%
0
500
1000
1500
2000
2500
Fre
qu
en
cy
Grade ppm
Au - Total Geomet Population Ciresata Sediment
0%
20%
40%
60%
80%
100%
0
500
1000
1500
2000
2500
Fre
qu
en
cy
Grade ppm
Au - Total Geomet Population Ciresata Sediment
0%
20%
40%
60%
80%
100%
0
5
10
15
20
25
30
35
40
45
Fre
qu
en
cy
Grade ppm
Cu - Geomet Subsample Composite MET-27
0%
20%
40%
60%
80%
100%
0
5
10
15
20
25
30
35
40
45
Fre
qu
en
cy
Grade ppm
Cu - Geomet Subsample Composite MET-27
Total Population vs. Metallurgical Composite
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Representative Sampling – Alteration Distribution
0%
5%
10%
15%
20%
25%
30%
35%
0
500
1000
1500
2000
2500
NA VWK WK MOD INT PER
Quartz Stockwork - Total Geomet Population Ciresata Sediment
Number
Percentage
0%
5%
10%
15%
20%
25%
30%
35%
0
500
1000
1500
2000
2500
NA VWK WK MOD INT PER
Quartz Stockwork - Total Geomet Population Ciresata Sediment
Number
Percentage
0%
5%
10%
15%
20%
25%
30%
35%
0
10
20
30
40
50
60
70
80
90
100
NA VWK WK MOD INT PER
Quartz Stockwork - Geomet Subsample Composite MET-27
Number
Percentage
0%
5%
10%
15%
20%
25%
30%
35%
0
10
20
30
40
50
60
70
80
90
100
NA VWK WK MOD INT PER
Quartz Stockwork - Geomet Subsample Composite MET-27
Number
Percentage
9 7 0
2
258
1
Alteration - Geomet Subsample Composite MET-27
A
PH
TRPH
SIL
PT
MACE
9 7 0
2
258
1
Alteration - Geomet Subsample Composite MET-27
A
PH
TRPH
SIL
PT
MACE
219184
4
53
6572
20
Alteration - Total Geomet Population Ciresata Sediment
A
PH
TRPH
SIL
PT
MACE
219184
4
53
6572
20
Alteration - Total Geomet Population Ciresata Sediment
A
PH
TRPH
SIL
PT
MACE
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Representative Sampling – Spatial Distribution
Top ViewTop ViewTop ViewTop View Section Looking WestSection Looking WestSection Looking WestSection Looking West
Modal Analysis
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Geometallurgical Unit Characterisation
Minerals
ChalcopyritePyritePyrrhotiteQuartzChlorite
MuscoviteOrthoclasePlagioclaseBiotite
AmphibolesKaoliniteEpidote/Zoisite
Other Silicate GangueCarbonatesFe Oxide/Spinels
Other
Su
rve
y N
ame
MET-32
MET-31
MET-30
MET-28
MET-27
Mass (%)0 50 100
Minerals
ChalcopyritePyritePyrrhotiteQuartzChlorite
MuscoviteOrthoclasePlagioclaseBiotite
AmphibolesKaoliniteEpidote/Zoisite
Other Silicate GangueCarbonatesFe Oxide/Spinels
Other
Su
rve
y N
ame
MET-32
MET-31
MET-30
MET-28
MET-27
Mass (%)0 50 100
Minerals
Chalcopyrite
Pyrite
Pyrrhotite
MET-32
MET-31
MET-30
MET-28
MET-27
Mass (%)0 2 4 6 8 10
Minerals
Chalcopyrite
Pyrite
Pyrrhotite
MET-32
MET-31
MET-30
MET-28
MET-27
Mass (%)0 2 4 6 8 10
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Copper and Gold
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Rougher Flotation Benchmarking
0
5
10
15
20
25
0 50 100
Go
ld G
rad
e
Gold Recovery
MET-27
MET-28
MET-30
MET-31
MET-32
0
5
10
15
20
25
0 50 100
Go
ld G
rad
e
Gold Recovery
MET-27
MET-28
MET-30
MET-31
MET-32
0
1
2
3
4
5
6
0 50 100
Co
pp
er
Gra
de
Copper Recovery
MET-27
MET-28
MET-30
MET-31
MET-32
0
1
2
3
4
5
6
0 50 100
Co
pp
er
Gra
de
Copper Recovery
MET-27
MET-28
MET-30
MET-31
MET-32
Is Consolidation Required?
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Geometallurgical Unit Review
0.05 0.1 0.15 0.2
MET 27
MET 28
MET30
MET31
MET32
Head Grade
0.05 0.1 0.15 0.2
MET 27
MET 28
MET30
MET31
MET32
Head Grade
0 10 20
MET 27
MET 28
MET30
MET31
MET32
Biotite
0 10 20
MET 27
MET 28
MET30
MET31
MET32
Biotite
0 10 20
MET 27
MET 28
MET30
MET31
MET32
Pyrite/Chalcopyrite Ratio
0 10 20
MET 27
MET 28
MET30
MET31
MET32
Pyrite/Chalcopyrite Ratio
0 10 20
MET 27
MET 28
MET30
MET31
MET32
Mass Pull
0 10 20
MET 27
MET 28
MET30
MET31
MET32
Mass Pull
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• Cu grade vs recovery are distinct (with exception of MET-27 and MET-28)
• Pyrite/chalcopyrite ratio is higher in MET-28, impacting mass pull and Cu recovery
• Cu grade at a given Cu recovery is linked to the pyrite/chalcopyrite ratio in MET-30 and MET-32
• Overall Cu recovery varies and are not specifically driven by head grade
• Filtration rates are very slow for MET-27 due to the high biotite content
• As a result – five geometallurgical units were allowed to stand as distinct entities
Geometallurgical Unit Review
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• Screening tests to evaluate primary grind size, reagent type, pH, viscosity modifiers and gangue depressants
– Use of benchmarking data, mineral grain size, modal analysis used as an input in the design of test program
• DOE program to optimise pH, collector dosage, collector type
• Locked cycle tests
Next Steps
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• Geometallurgical studies define range of mineralogical characteristics and metallurgical performance that can be expected from an orebody
• Definition of geometallurgical units is best achieved by teams consisting of project geologists and metallurgical/process mineralogy staff
• Creation of representative composites is of key importance
• Use of quantitative mineralogy combined with metallurgical testing can define the geometallurgical character of the deposit even at early project stages
Conclusions