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1 
Minotaur Exploration Limited | ASX: MEP 
The Artemis Cu-Au Deposit 
A. P. Belperio 
The Mining 2014 Resources Convention 
Brisbane, 30 October 2014
2 
Cloncurry Cu-Au 
This time last year 
• Minotaur merger with BRW 
was underway primarily to 
gain access to the BRW 
Eloise tenements 
• The $6M Eloise JV poised 
to commence with private 
equity partner GFR 
• The best available AEM 
system at the time was 
poised to commence flying
3 
Artemis Cu-Au Discovery 
Artemis polymetallic Cu-Au-Zn-Ag discovery 
was announced 31 July 2014. 
• How was the discovery made? 
• What is it? 
• What are the plans going forward?
4 
IOCG - ISCG 
IOCG Focus Areas 
• Gawler Craton 
• Cloncurry 
Mineralisation Styles 
• Haematite-hosted IOCG 
• Magnetite-hosted IOCG 
• Pyrrhotite-hosted ISCG 
Targeting undercover, particularly the 
highly reduced and conductive cover 
marginal to Cloncurry, necessitates a 
focused and selective geophysical 
approach
5 
IOCG – ISCG Geophysical characteristics 
IOCG deposits (magnetite-rich) 
(Ernest Henry, Osborne, Mt Elliott-Swan): 
 Significant positive magnetic anomalies 
 Positive gravity anomalies 
 Strong IP chargeability anomalies 
 Weak to no EM anomalies 
 Broad alteration haloes 
Osborne 
ISCG deposits (pyrrhotite-rich) 
(Eloise, Artemis, Kulthor, East Osborne, Lady Clayre, Cormorant): 
 No positive magnetic anomalies 
 Limited gravity anomalism 
 Limited alteration haloes 
 Positive IP chargeability anomalies 
 Strong ground EM anomalies 
Ernest Henry 
Kulthor 
Eloise 
Artemis
6 
Cormorant ISCG 
JOGMEC JV 
• Several years of work on the Naraku tenements 
north of Cloncurry 
• Successfully penetrated ultra-conductive cover 
beneath black soil plains 
• Major Iron Sulphide Copper Gold system (ISCG) 
encountered 
• 15km, 20+m thick, massive & breccia pyrrhotite, 
persistently mineralised Cu-Au-Co 
MIN04 : 20m @ 0.2% Cu, 0.02% Co from 160m 
MIN07 : 56m @ 0.1% Cu, 0.03 g/t Au from 186m 
MIN10 : 72m @ 0.21% Cu, 0.02% Co from 414m 
Cormorant
7 
Eloise ISCG 
Shift towards Eloise driven by: 
• Recognition of the ISCG style as a 
significant and different style of Cu-Au 
mineralisation 
• Understanding of different exploration 
tools required, particularly EM and AEM 
• Requirement for shallower ground that 
would allow airborne techniques to be 
used as a more rapid screening tool
8 
Eloise JV 
November 2013 
• $1.7M Year 1 Work Program 
commenced 
 Primary AEM survey 
(Nov-Dec13) 
 Ground EM follow-up at 
16 targets (Feb-Apr14) 
 Drill test 10 best targets 
(May-July 2014)
9 
EVT54 
Late-time, Z-component VTEM image 
VTEM target EVT 54 
Late-time VTEM image and line profile 
• VTEM target EVT54 of particular 
interest – 350m west of the Sandy 
Creek inferred resource (see slide 19) 
• Outcropping BIF and some ironstone 
“gossan” had attracted some past 
attention, some historic EM, and “sniffs” 
of copper and gold mineralisation 
encountered 
• EVT54 therefore became a priority 
target for ground EM follow-up
10 
EVT54 
Late-time, Z-component VTEM image 
VTEM Target EVT 54 - Ground EM 
• Ground EM at EVT54 confirmed a 
steeply dipping, high conductance 
body, from c. 80m below ground level 
• Original plate model from the fixed 
loop ground EM neatly fitted between 
historic drillholes in the vicinity 
• EVT54 recommended as the premier 
target based on conductance and 
associated gold and copper hits 
nearby. 
• Drillhole EL14D09 successfully tested 
the target, named Artemis
11 
Artemis 
• Discovery hole 22m @ 3.02% Cu, 3.81 g/t 
Au, 6.64% Zn, 1.35% Pb, 112 g/t Ag from 157 to 
179 m 
• Two further holes 50m up-dip and 
down-dip 
• Drillhole EL14D10 : 21m @ 0.84% Cu, 0.73 
g/t Au, 5.06% Zn,, 1.85% Pb, 69 g/t Ag 
• Drillhole EL14D12 : 24m @ 1.58% Cu, 2.12 
g/t Au, 4.74% Zn, 1.13% Pb, 54 g/t Ag 
• 122m vertical section drilled to date 
plus down-hole EM can “see” a further 
50m incrementally 
• Drilling suspended to allow new 
heritage clearance surveys, new 
geophysics, planning of systematic drill 
programs and Joint Venture approvals.
12 
Artemis 
What is Artemis: 
• Blind deposit of late fracture fill 
massive sulphide 
• Fe-Cu-Zn-Pb sulphides. Very limited 
alteration halo or host rock brecciation 
• Steep, tabular body, structurally 
controlled. No significant magnetic or 
gravity expression 
• Responsive to Down-hole and Across-hole 
EM
13 
Artemis Drillhole EL14D09 
166.6m: coarse, massive sulphides including chalcopyrite (yellow), sphalerite (black), 
pyrrhotite (bronze-grey) and calcite (white to pale grey) – no host rock brecciation. 
Metre interval assay: 36% Fe, 2.7% Cu, 1.5 ppm Au, 6.7% Zn, 1.1% Pb, 111 ppm Ag
14 
Artemis - mineralogy 
Cu Zn Au
15 
Artemis – Eloise Comparison 
• Mineralogical associations (Eloise after Baker, 1998) 
Element Artemis Eloise Major mineral 
EL14D09 
Fe 20-38% - Pyrrhotite 
Cu 0.2-8% 0.1-25% Chalcopyrite 
Zn 0.02-14% 0.1-1.0% Sphalerite 
Au 0.1-20 ppm 0.1-15 ppm Electrum 
Ag 0.1-289 ppm 0.1-60 ppm Electrum 
Pb 0.1-36,000 ppm 0.1-300 ppm Galena 
As 0.1-9000 ppm 0.1-500 ppm Arsenopyrite 
Bi 0.1-500ppm 0.1-100 ppm Bismuthinite 
Co 0.1-2200 ppm 5-750 ppm Cobaltite 
Bright whitish-yellow gold grains (or 
possible electrum) (2μm to 20μm) 
circled, mostly in pyrrhotite, some in and 
on margins of chalcopyrite.
16 
Artemis 
• Re-surveying of historic drill holes in 
the immediate vicinity allowed 
earlier mineralisation to be placed in 
context 
• Rock chip sampling has tracked 
controlling structure for 400m north 
and 400m south 
• New ground geophysics underway 
to aid drill collar siting 
• Numerous similarities to the Eloise 
Cu-Au mine have been noted:
17 
Artemis – Eloise Comparison 
• Mineralogical association, tabular parameters and structural 
style at Artemis appear similar to Eloise 
• Eloise comprise a number of offset massive sulphide lenses 
of short strike length (<200m) but great down dip extent 
• Early evidence at Artemis similarly suggests late brittle 
structures exert significant control on mineralised slabs.
18 
Artemis – Eloise Comparison 
• Eloise had an original resource at 
Decision To Mine of 3.1 Mt @ 5.5% 
Cu, 1.4 g/t Au and 16 g/t Ag (Amalg 
1996) 
• Since 1996, over 10 Mt has been 
mined at an average grade of 3.50% 
Cu, 0.93 g/t Au. Mining currently 
continues below the -1300m level 
• From what we currently know of 
Artemis – the first 3 drillhole 
intercepts and EM conductor plates 
neatly fit the Eloise mineralisation 
long section model 
• Expect clarification as down dip 
drilling advances.
19 
Artemis 
Relation to Sandy Creek 
• New geophysical surveys underway 
• Common surveys to extend north, 
south and east to Sandy Creek 
• Looking for potential linkages to 
Sandy Creek and other historic 
mineralisation 
• Sandy Creek inferred resource  : 
2.0 Mt @ 1.32% Cu, 0.30 g/t Au and 
open below 200-250m depth. A 
peripheral zinc zone to the south 
has not been properly investigated. 
 A resource of 2.0 Mt @ 1.32% Cu, 0.30 g/t Au for 26,400 t contained copper and 21,400 oz contained gold at the Sandy Creek deposit was estimated by Optiro for Breakaway Resources 
in 2013 and classified by the Competent Person, Mr Michael Andrew, as an Inferred Resource under the 2012 JORC Code. See Breakaway Resources ASX Release 26 February 2013. 
Minotaur further confirms that it is not aware of any new information or data that materially affects the information included in that announcement and that all material assumptions and 
technical parameters underpinning the estimates in that announcement continue to apply and have not materially changed.
20 
Sandy Creek mineralisation 
Chalcopyrite + pyrrhotite mineralisation 
12BERD119: 175.1m 
12BERD119: 223.8m 
Younger chalcopyrite + calcite mineralisation
21 
Artemis – Proposed Work 
Accelerated $6M workplan from 
Oct 2014 to Jun 2015 
• Systematic drill testing at Artemis 
• Along strike and down dip extent 
to be guided by systematic downhole surveys 
• Thickness – grade variation mapping 
• 40+ holes, 18,000m, 2 DDH Rigs 
• Metallurgy, petrology and resource definition 
• Along-structure extensions to north and south
22 
Artemis – Proposed Work 
Accelerated $6M workplan from 
Oct 2014 to Jun 2015 
• Systematic drill testing at Artemis 
• Along strike and down dip extent 
to be guided by systematic downhole surveys 
• Thickness – grade variation mapping 
• 40+ holes, 18,000m, 2 DDH Rigs 
• Metallurgy, petrology and resource definition 
Artemis 
• Along-structure extensions to north and Sandy south 
Creek 
• Connections with Sandy Creek and greater Artemis area 
• Greenfield targeting: Drill testing a further 10 regional target 
• Greenfield targeting: Deep EM along the Levuka Shear
23 
Artemis – Proposed Work 
Accelerated $6M workplan from 
Oct 2014 to Jun 2015 
• Systematic drill testing at Artemis 
• Along strike and down dip extent 
to be guided by systematic downhole surveys 
• Thickness – grade variation mapping 
• 40+ holes, 18,000m, 2 DDH Rigs 
• Metallurgy, petrology and resource definition 
• Along-structure extensions to north and south 
• Connections with Sandy Creek and greater Artemis area 
• Greenfield targeting: Drill testing a further 10 regional targets 
• Greenfield targeting: Deep EM along the Levuka Shear
24 
Artemis – Proposed Work 
Accelerated $6M workplan from 
Oct 2014 to Jun 2015 
• Systematic drill testing at Artemis 
• Along strike and down dip extent 
to be guided by systematic downhole surveys 
• Thickness – grade variation mapping 
• 40+ holes, 18,000m, 2 DDH Rigs 
• Metallurgy, petrology and resource definition 
• Along-structure extensions to north and south 
• Connections with Sandy Creek and greater Artemis area 
• Greenfield targeting: Drill testing a further 10 regional targets 
• Greenfield targeting: Deep EM along the Levuka Shear
25 
Disclaimer 
Disclaimer 
This presentation has been prepared by the management of Minotaur Exploration Limited (“Minotaur”, ASX: MEP) for the general benefit of analysts, brokers and 
investors and does not constitute specific advice to any particular party or persons. Information herein is based on publicly available information, internally developed 
data and other sources. Where an opinion, projection or forward looking statement is expressed in this presentation, it is based on the assumptions and limitations 
mentioned herein and is an expression of present opinion only. No warranties or representations are made or implied as to origin, validity, accuracy, completeness, 
currency or reliability of the information. Minotaur specifically disclaims and excludes all liability (to the extent permitted by law) for losses, claims, damages, demands, 
costs and expenses of whatever nature arising in any way out of or in connection with the information, its accuracy, completeness or by reason of reliance by any 
person on any of it. Where Minotaur expresses or implies an expectation or belief as to the success of future exploration and the economic viability of future project 
evaluations, such expectation or belief is expressed in good faith and is believed to have a reasonable basis. However, such projected outcomes are subject to risks, 
uncertainties and other factors which could cause actual results to differ materially from projected future results. Such risks include, but are not limited to, exploration 
success, metal price volatility, changes to current mineral resource estimates or targets, changes to assumptions for capital and operating costs as well as political and 
operational risks and government regulatory outcomes. MEP disclaims any obligation to advise any person if it becomes aware of any inaccuracy in or omission from 
any forecast or to update such forecast. 
Competent Person’s Statement 
Information in this presentation that relates to exploration results for Minotaur Exploration Ltd is based on information compiled by Dr. A. P. Belperio, who is a Director 
and full-time employee of the Company and a Fellow of the Australian Institute of Mining and Metallurgy. Dr. Belperio has sufficient experience relevant to the style of 
mineralisation and type of deposits under consideration and to the activity that he has undertaken to qualify as a Competent Person as defined in the 2012 Edition of 
the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves” (JORC Code). Dr. Belperio consents to inclusion of this information 
in the form and context in which it appears. 
Artemis 
Daughter of Zeus and Leto and the twin sister of Apollo. She was the Hellenic goddess of the hunt.

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The Artemis Cu-Au Deposit by A.P.Belperio

  • 1. 1 Minotaur Exploration Limited | ASX: MEP The Artemis Cu-Au Deposit A. P. Belperio The Mining 2014 Resources Convention Brisbane, 30 October 2014
  • 2. 2 Cloncurry Cu-Au This time last year • Minotaur merger with BRW was underway primarily to gain access to the BRW Eloise tenements • The $6M Eloise JV poised to commence with private equity partner GFR • The best available AEM system at the time was poised to commence flying
  • 3. 3 Artemis Cu-Au Discovery Artemis polymetallic Cu-Au-Zn-Ag discovery was announced 31 July 2014. • How was the discovery made? • What is it? • What are the plans going forward?
  • 4. 4 IOCG - ISCG IOCG Focus Areas • Gawler Craton • Cloncurry Mineralisation Styles • Haematite-hosted IOCG • Magnetite-hosted IOCG • Pyrrhotite-hosted ISCG Targeting undercover, particularly the highly reduced and conductive cover marginal to Cloncurry, necessitates a focused and selective geophysical approach
  • 5. 5 IOCG – ISCG Geophysical characteristics IOCG deposits (magnetite-rich) (Ernest Henry, Osborne, Mt Elliott-Swan):  Significant positive magnetic anomalies  Positive gravity anomalies  Strong IP chargeability anomalies  Weak to no EM anomalies  Broad alteration haloes Osborne ISCG deposits (pyrrhotite-rich) (Eloise, Artemis, Kulthor, East Osborne, Lady Clayre, Cormorant):  No positive magnetic anomalies  Limited gravity anomalism  Limited alteration haloes  Positive IP chargeability anomalies  Strong ground EM anomalies Ernest Henry Kulthor Eloise Artemis
  • 6. 6 Cormorant ISCG JOGMEC JV • Several years of work on the Naraku tenements north of Cloncurry • Successfully penetrated ultra-conductive cover beneath black soil plains • Major Iron Sulphide Copper Gold system (ISCG) encountered • 15km, 20+m thick, massive & breccia pyrrhotite, persistently mineralised Cu-Au-Co MIN04 : 20m @ 0.2% Cu, 0.02% Co from 160m MIN07 : 56m @ 0.1% Cu, 0.03 g/t Au from 186m MIN10 : 72m @ 0.21% Cu, 0.02% Co from 414m Cormorant
  • 7. 7 Eloise ISCG Shift towards Eloise driven by: • Recognition of the ISCG style as a significant and different style of Cu-Au mineralisation • Understanding of different exploration tools required, particularly EM and AEM • Requirement for shallower ground that would allow airborne techniques to be used as a more rapid screening tool
  • 8. 8 Eloise JV November 2013 • $1.7M Year 1 Work Program commenced  Primary AEM survey (Nov-Dec13)  Ground EM follow-up at 16 targets (Feb-Apr14)  Drill test 10 best targets (May-July 2014)
  • 9. 9 EVT54 Late-time, Z-component VTEM image VTEM target EVT 54 Late-time VTEM image and line profile • VTEM target EVT54 of particular interest – 350m west of the Sandy Creek inferred resource (see slide 19) • Outcropping BIF and some ironstone “gossan” had attracted some past attention, some historic EM, and “sniffs” of copper and gold mineralisation encountered • EVT54 therefore became a priority target for ground EM follow-up
  • 10. 10 EVT54 Late-time, Z-component VTEM image VTEM Target EVT 54 - Ground EM • Ground EM at EVT54 confirmed a steeply dipping, high conductance body, from c. 80m below ground level • Original plate model from the fixed loop ground EM neatly fitted between historic drillholes in the vicinity • EVT54 recommended as the premier target based on conductance and associated gold and copper hits nearby. • Drillhole EL14D09 successfully tested the target, named Artemis
  • 11. 11 Artemis • Discovery hole 22m @ 3.02% Cu, 3.81 g/t Au, 6.64% Zn, 1.35% Pb, 112 g/t Ag from 157 to 179 m • Two further holes 50m up-dip and down-dip • Drillhole EL14D10 : 21m @ 0.84% Cu, 0.73 g/t Au, 5.06% Zn,, 1.85% Pb, 69 g/t Ag • Drillhole EL14D12 : 24m @ 1.58% Cu, 2.12 g/t Au, 4.74% Zn, 1.13% Pb, 54 g/t Ag • 122m vertical section drilled to date plus down-hole EM can “see” a further 50m incrementally • Drilling suspended to allow new heritage clearance surveys, new geophysics, planning of systematic drill programs and Joint Venture approvals.
  • 12. 12 Artemis What is Artemis: • Blind deposit of late fracture fill massive sulphide • Fe-Cu-Zn-Pb sulphides. Very limited alteration halo or host rock brecciation • Steep, tabular body, structurally controlled. No significant magnetic or gravity expression • Responsive to Down-hole and Across-hole EM
  • 13. 13 Artemis Drillhole EL14D09 166.6m: coarse, massive sulphides including chalcopyrite (yellow), sphalerite (black), pyrrhotite (bronze-grey) and calcite (white to pale grey) – no host rock brecciation. Metre interval assay: 36% Fe, 2.7% Cu, 1.5 ppm Au, 6.7% Zn, 1.1% Pb, 111 ppm Ag
  • 14. 14 Artemis - mineralogy Cu Zn Au
  • 15. 15 Artemis – Eloise Comparison • Mineralogical associations (Eloise after Baker, 1998) Element Artemis Eloise Major mineral EL14D09 Fe 20-38% - Pyrrhotite Cu 0.2-8% 0.1-25% Chalcopyrite Zn 0.02-14% 0.1-1.0% Sphalerite Au 0.1-20 ppm 0.1-15 ppm Electrum Ag 0.1-289 ppm 0.1-60 ppm Electrum Pb 0.1-36,000 ppm 0.1-300 ppm Galena As 0.1-9000 ppm 0.1-500 ppm Arsenopyrite Bi 0.1-500ppm 0.1-100 ppm Bismuthinite Co 0.1-2200 ppm 5-750 ppm Cobaltite Bright whitish-yellow gold grains (or possible electrum) (2μm to 20μm) circled, mostly in pyrrhotite, some in and on margins of chalcopyrite.
  • 16. 16 Artemis • Re-surveying of historic drill holes in the immediate vicinity allowed earlier mineralisation to be placed in context • Rock chip sampling has tracked controlling structure for 400m north and 400m south • New ground geophysics underway to aid drill collar siting • Numerous similarities to the Eloise Cu-Au mine have been noted:
  • 17. 17 Artemis – Eloise Comparison • Mineralogical association, tabular parameters and structural style at Artemis appear similar to Eloise • Eloise comprise a number of offset massive sulphide lenses of short strike length (<200m) but great down dip extent • Early evidence at Artemis similarly suggests late brittle structures exert significant control on mineralised slabs.
  • 18. 18 Artemis – Eloise Comparison • Eloise had an original resource at Decision To Mine of 3.1 Mt @ 5.5% Cu, 1.4 g/t Au and 16 g/t Ag (Amalg 1996) • Since 1996, over 10 Mt has been mined at an average grade of 3.50% Cu, 0.93 g/t Au. Mining currently continues below the -1300m level • From what we currently know of Artemis – the first 3 drillhole intercepts and EM conductor plates neatly fit the Eloise mineralisation long section model • Expect clarification as down dip drilling advances.
  • 19. 19 Artemis Relation to Sandy Creek • New geophysical surveys underway • Common surveys to extend north, south and east to Sandy Creek • Looking for potential linkages to Sandy Creek and other historic mineralisation • Sandy Creek inferred resource  : 2.0 Mt @ 1.32% Cu, 0.30 g/t Au and open below 200-250m depth. A peripheral zinc zone to the south has not been properly investigated.  A resource of 2.0 Mt @ 1.32% Cu, 0.30 g/t Au for 26,400 t contained copper and 21,400 oz contained gold at the Sandy Creek deposit was estimated by Optiro for Breakaway Resources in 2013 and classified by the Competent Person, Mr Michael Andrew, as an Inferred Resource under the 2012 JORC Code. See Breakaway Resources ASX Release 26 February 2013. Minotaur further confirms that it is not aware of any new information or data that materially affects the information included in that announcement and that all material assumptions and technical parameters underpinning the estimates in that announcement continue to apply and have not materially changed.
  • 20. 20 Sandy Creek mineralisation Chalcopyrite + pyrrhotite mineralisation 12BERD119: 175.1m 12BERD119: 223.8m Younger chalcopyrite + calcite mineralisation
  • 21. 21 Artemis – Proposed Work Accelerated $6M workplan from Oct 2014 to Jun 2015 • Systematic drill testing at Artemis • Along strike and down dip extent to be guided by systematic downhole surveys • Thickness – grade variation mapping • 40+ holes, 18,000m, 2 DDH Rigs • Metallurgy, petrology and resource definition • Along-structure extensions to north and south
  • 22. 22 Artemis – Proposed Work Accelerated $6M workplan from Oct 2014 to Jun 2015 • Systematic drill testing at Artemis • Along strike and down dip extent to be guided by systematic downhole surveys • Thickness – grade variation mapping • 40+ holes, 18,000m, 2 DDH Rigs • Metallurgy, petrology and resource definition Artemis • Along-structure extensions to north and Sandy south Creek • Connections with Sandy Creek and greater Artemis area • Greenfield targeting: Drill testing a further 10 regional target • Greenfield targeting: Deep EM along the Levuka Shear
  • 23. 23 Artemis – Proposed Work Accelerated $6M workplan from Oct 2014 to Jun 2015 • Systematic drill testing at Artemis • Along strike and down dip extent to be guided by systematic downhole surveys • Thickness – grade variation mapping • 40+ holes, 18,000m, 2 DDH Rigs • Metallurgy, petrology and resource definition • Along-structure extensions to north and south • Connections with Sandy Creek and greater Artemis area • Greenfield targeting: Drill testing a further 10 regional targets • Greenfield targeting: Deep EM along the Levuka Shear
  • 24. 24 Artemis – Proposed Work Accelerated $6M workplan from Oct 2014 to Jun 2015 • Systematic drill testing at Artemis • Along strike and down dip extent to be guided by systematic downhole surveys • Thickness – grade variation mapping • 40+ holes, 18,000m, 2 DDH Rigs • Metallurgy, petrology and resource definition • Along-structure extensions to north and south • Connections with Sandy Creek and greater Artemis area • Greenfield targeting: Drill testing a further 10 regional targets • Greenfield targeting: Deep EM along the Levuka Shear
  • 25. 25 Disclaimer Disclaimer This presentation has been prepared by the management of Minotaur Exploration Limited (“Minotaur”, ASX: MEP) for the general benefit of analysts, brokers and investors and does not constitute specific advice to any particular party or persons. Information herein is based on publicly available information, internally developed data and other sources. Where an opinion, projection or forward looking statement is expressed in this presentation, it is based on the assumptions and limitations mentioned herein and is an expression of present opinion only. No warranties or representations are made or implied as to origin, validity, accuracy, completeness, currency or reliability of the information. Minotaur specifically disclaims and excludes all liability (to the extent permitted by law) for losses, claims, damages, demands, costs and expenses of whatever nature arising in any way out of or in connection with the information, its accuracy, completeness or by reason of reliance by any person on any of it. Where Minotaur expresses or implies an expectation or belief as to the success of future exploration and the economic viability of future project evaluations, such expectation or belief is expressed in good faith and is believed to have a reasonable basis. However, such projected outcomes are subject to risks, uncertainties and other factors which could cause actual results to differ materially from projected future results. Such risks include, but are not limited to, exploration success, metal price volatility, changes to current mineral resource estimates or targets, changes to assumptions for capital and operating costs as well as political and operational risks and government regulatory outcomes. MEP disclaims any obligation to advise any person if it becomes aware of any inaccuracy in or omission from any forecast or to update such forecast. Competent Person’s Statement Information in this presentation that relates to exploration results for Minotaur Exploration Ltd is based on information compiled by Dr. A. P. Belperio, who is a Director and full-time employee of the Company and a Fellow of the Australian Institute of Mining and Metallurgy. Dr. Belperio has sufficient experience relevant to the style of mineralisation and type of deposits under consideration and to the activity that he has undertaken to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves” (JORC Code). Dr. Belperio consents to inclusion of this information in the form and context in which it appears. Artemis Daughter of Zeus and Leto and the twin sister of Apollo. She was the Hellenic goddess of the hunt.