The spectrum of uranium-bearing mineral systems in South ...€¦ · The spectrum of...
Transcript of The spectrum of uranium-bearing mineral systems in South ...€¦ · The spectrum of...
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The spectrum of uranium-bearing mineral systems in South Australia and global exploration implications.
Martin FaircloughChief Geoscientist, Geological Survey of South Australia
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Overview• Overview of South Australia and PACE
• Update of Existing Uranium Mining Operations
• Exploration Projects to Watch
• Exploration Overview
• Mineral Potential Modelling (IOCG U)
• Implications and summary
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2004: 5 Major Mines
South Australia’s Major Mines 2004
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Target: 11 mines in 200916 mines in 2010
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January 2004
Mineral Exploration Licence Coverage
November 2009January 2008
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PACE – Building on the first 5 yearsPartnerships
• Continuing commitment to Research Centres
• Substantial seed funding for a new CRC – Deep Exploration Targetting– New Adelaide-based Centre and CEO– South Australian case studies
• Partnership with Saskatchewan Ministry of Mines
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PACE – Drill Intersections Highlights
Dominion Mining – Barton Area
Dominion Mining – Challenger Project
Goldstream Mining – Mount Woods Inlier
Havilah Resources – Curnamona Copper-Gold
Hillgrove Resources – Kanmantoo Copper-Gold Exploration
Minotaur Exploration – Mount Woods Inlier
Petratherm – Callabonna Geothermal
RMG Services – CarrapateenaStellar Resources – Coolybring Magnetite Project
Tasman Resources – Marathon South
Tasman Resources – Parkinson Dam
Vintage Exploration and Mining – Kiki Ultramafic Project
Lynch Mining – Archaean Copper Zinc
Iluka Resources – Gulliver’s HMS Prospect
Quasar / Alliance – 4 Mile Uranium
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South Australian Exploration Expenditure
South Australia’s Advantage:
• 39% - national share of uranium exploration
• 35% - national share of copper exploration
MINERAL EXPLORATION BY COMMODITY 2008/09
$1, 0%$3m 1%
$14m 6%$14m 7%
$2m 1% $42m 20%
$62m 29%$73m 36%
Copper
Silver, Lead, Zinc
Nickel, Cobalt
other BaseMetalsGold
Iron Ore
Mineral Sands
Uranium
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Uranium exploration expenditure in Australia - 2008
$94m 43%
$58m 26%
$34m 15%
$35m 16%
SANTQldOther
•South Australia continued to lead the nation as the primary state to explore for uranium in 2008.
•Expenditure for uranium exploration in 2008 was $94 million accounting for 43%of Australia’s total uranium exploration expenditure.
•Hosts two of Australia’s three uranium mines, Olympic Dam & Beverley, with a third under construction at Honeymoon.
•Recent discoveries include: – Four Mile (Quasar & Alliance Resources)– Hillside (Rex Minerals)– Mullaquana (Uranium SA)
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Tarcoola
Port Augusta
Moonta
Ceduna
Coober Pedy
Oodnadatta
Moomba
Renmark
Robe
Mt Gambier
Adelaide
Kingscote
Marla
Moonta
Port LincolnVein
Roll front
Breccia
Unconformity
OLYMPIC DAM
YARRANNA
RADIUM HILL
HONEYMOON
MT PAINTER
BEVERLEY
Andamooka
WARRIOR
TYPES OF URANIUM DEPOSITS(known and potential)
• Breccia complex e.g. OD• Sandstone(roll-front) e.g.
Beverley, Honeymoon, Warrior
• U/C redox related?• Vein style e.g. Crocker
Well, Radium Hill• Calcrete-hosted?
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Solid Geology of the Gawler Craton
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Olympic Dam – Copper-Gold-Uranium-Silver BHP Billiton Ltd
• Largest uranium deposit, fourth largest remaining copper deposit and fifth largest gold deposit in the world. Also contains significant quantities of silver.
• Total Resource 9 080 Mt at 0.87% Cu, 0.027% U3O8, 0.32 g/t Au and 1.5 g/t Ag
– Gold only (non-sulfide) resource 151 Mt at 1.0 g/t Au.
• Reserve (ore) 473 Mt at 1.86% Cu, 0.06% U3O8, 0.76 g/t Au and 3.95 g/t Ag
Production 2008/09 – 194 100 t Cu, 4007 t U3O8, 108 000 oz Au, 937 000 oz Ag
Olympic Dam
www.bhpbilliton.com
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IOCG Deposits - Size & Au Grade Comparison with Global Cu-Au Mines
Ernest Henry
Prominent Hill
(modified after Corriveau, 2005)
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Olympic Dam – Copper-Gold-Uranium-SilverBHP Billiton Ltd
Current activities:• Environmental Impact Statement closed in
August 2009. Government decision in 2010
• New 60 Mtpa Olympic Dam will have an approximate annual production of:
– 750 000 t Cu, – 19 000 t U3O8
– 800 000 oz Au, – 2 900 000 oz Ag– incl. 2 Million tonnes concentrate to
China
Olympic Dam
www.bhpbilliton.com
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Olympic Dam Expansion BHP – Billiton
Olympic Dam – Copper-Gold-Uranium-SilverBHP Billiton Ltd
Olympic Dam
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Beverley Mine – UraniumHeathgate Resources Ltd
• Largest in-situ leach operation in the world.
• Total Resource 7.7 Mt at 0.27% U3O8 for a contained commodity of 21 000 t U3O8.
• Production 2007/08 – 719 t U3O8.
• Expansion of the Beverley Uranium Mine approved August 2008.
CURRENT ACTIVITIES:
• Mining of Beverley 4 Mile arrpoved
• New Pepagoona discovery
Beverley
www.heathgateresources.com.au
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Honeymoon – Uranium Uranium One Inc – Mitsui & Co. Ltd
• Construction commenced, production to commence in 2010.
• Indicated Resource 1.2 Mt at 0.24% containing 2900 t (6.5 Mlb) U3O8.
• Estimated annual production of 400 t U3O8.
• Deposit occurs as five discrete mineralised sand packages in the Yarramba Palaeochannel.
• Structural influence to mineralisation.
Honeymoon
www.uranium1.com
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Four Mile – UraniumQuasar Resources – Alliance Resources Ltd
• Tertiary sandstone-hosted mineralisation in two distinct zones: Four Mile West and Four Mile East.
• Inferred resource of 3.9 Mt at 0.37% U3O8containing 15 000 t U3O8.
• Mining Lease Application submitted in May 2008.
• First Stage mining proposed for early 2010.
• Production estimated between 680-2045 tpaU3O8.
• Mining approved – awaiting joint venture resolution
Four Mile
www.quasarresources.com.auwww.allianceresources.com.au
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Crocker Well – Mt Victoria – UraniumPepinNini Minerals Ltd – Sinosteel
• Inferred JORC compliant resource 12.5 Mt at 0.5 kg/t (0.05%) U3O8 (cut off grade 300 ppm).
• Production scheduled to commenced in 2011.
• Mineral lease application submitted to investigate production of ~ 600 t of U3O8 for at least 10 years.
Crocker Well
www.pepinnini.com.au
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Uranium Projects to Watch • Yarranna – 1: 8m at 626ppm U3O8.
• Goulds Dam: Indicated resource 1.7 Mt at 0.12% containing 2000 t U3O8.
• Oban: Drillhole CEY376 intersected >5m (above 100ppm eU3O8) grade thickness of 0.28m% eU3O8.
• Mt Gee: Inferred 51 Mt at 615ppm for 31 400t U3O8 .
• Hillside: 18m @ 297ppm U3O8, 2m @ 887ppm U3O8.
• Mullaquana: Pirie Basin, Eyre Peninsula. Inferred resource estimate 12 Mt at 0.02% eU3O8 for 2700 t U3O8.
Projects to watch• Major Mine
Adelaide
Olympic Dam Wirrda WellAcropolis
Oak Dam
Other Deposits
Cane Grass
Four MileMt Painter
Beverley
Oban
Honeymoon Goulds Dam
Radium Hill
Crocker Well
Mt Gee
Prominent Hill
Hillside
Yarranna – 1
Mullaquana
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Undiscovered Resources• Where to from here?
• “how “to from here?
• Mineral Deposit Models and/or Mineral Systems modelling?
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Uranium Deposit Classification - IAEA1. UNCONFORMITY-RELATED2. SANDSTONE3. QUARTZ-PEBBLE CONGLOMERATE4. VEIN5. BRECCIA COMPLEX6. INTRUSIVE7. PHOSPHORITE8. COLLAPSE BRECCIA PIPE9. VOLCANIC10. SURFICIAL 11. METASOMATITE12. METAMORPHIC13. LIGNITE14. BLACK SHALE15. OTHERS
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Uranium Deposit Classification - IAEA1. UNCONFORMITY-RELATED2. SANDSTONE3. QUARTZ-PEBBLE CONGLOMERATE4. VEIN5. BRECCIA COMPLEX6. INTRUSIVE7. PHOSPHORITE8. COLLAPSE BRECCIA PIPE9. VOLCANIC10. SURFICIAL11. METASOMATITE12. METAMORPHIC13. LIGNITE14. BLACK SHALE15. OTHERS
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Mineral Systems
• Based upon understanding all the geological ingredients which comprise the mineralsystem, and how they vary and relate to each other........................ PROCESSES!
• One side effect of utilising the Mineral Systems approach and concentrating on processes is that we are forced to consider related deposit types through time and space
• Case study - Regional IOCG U potential, particularly using geophysics in areas of limited outcrop (which should work in outcropping areas)
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Magmatic-hydrothermal
fluids
‘Metamorphic’fluids
(incl. metamorphicrock-buffered)
Meteoric, seawater
Groundwaters
Formation waters / connate waters
Diagenetic fluids
mixing
URANIUM MINERAL SYSTEMS and FLUIDS(a better process-driven classification)
Deep (mgt) IOCG
(1) Shallow U-bearing hematite
IOCG
(2) Unconformity U (PGE, Au)
(3) Sandstone U
(4) Calcrete U
(7) Volcanic(8) Intrusive(9) Vein
BASIN- and SURFACE-RELATED
U SYSTEMS
‘METAMORPHIC’-RELATED
U SYSTEMS(6)
MAGMATIC-RELATED
U SYSTEMSHYBRID
U SYSTEMS(1,5,9,10,11)
(5) Metasomatic(9) Vein
(10,12,13,14)
(7) Volcanic
(#) represent deposit types from IAEA Red Book & Dahlkamp (1990). Skirrow et al, 2009, Geoscience Australia
Courtesy GeoscienceAustralia
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Mineral Systems
• Based upon understanding all the geological ingredients which comprise the mineralsystem, and how they vary and relate to each other........................ PROCESSES!
• One side effect of utilising the Mineral Systems approach and concentrating on processes is that we are forced to consider related deposit types through time and space.
• We can then delineate the consequences of these processes as mappable criteria
• In SA we can map criteria for sandstone-hosted, unconformity related and IOCG Upotential, particularly using geophysics in areas of limited outcrop (which should work in outcropping areas)
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Mineral Systems• Mappable criteria
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Fairclough, M.C., McAvaney, S.O. and Wilson, T.C. (compilers) 2009. South Australian Uranium Occurrences – Updated second edition. 1:2 000 000 scale. Department of Primary Industries and Resources SA.
Uranium Occurrences Map
• Known uranium occurrences and significant geological parameters for each deposit type have been collated and represented spatially as ‘key ingredients’ maps.
• First step in predictive modelling for different uranium deposit types:
– IOCG U– Groundwater gradients, chemistry
and distance from source.– Basement controlling structures.– Pandurra Formation 3D Model.
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Mineral Systems• In detail for hard rock systems......
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ADELAIDE
Prominent Hill
Carrapateena
Iron Oxide - Copper - Gold Uranium
Olympic Dam
200 kmMoonta - Wallaroo
Hillside
Gawler Range Volcanics44 000sq km
Hiltaba Intrusions
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Mineral Systems• In detail for soft rock systems......
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ADELAIDE
Olympic Dam
Prominent Hill
Carrapateena
Rollfront/ Palaeochannel Uranium Moonta - Wallaroo
Eucla Basin
Eromanga Basin
Murray Basin
Warrior
Narlaby
Yaninee
~ 55 to 2 Ma
Honeymoon
BeverleyMt Gee
Crockers Well
Oban
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“hematite in” REDOX front
“pyrite out” REDOX front
oxidised granite
oxidised basin fillelevated U
reduced layers
oxidised layers
Palaeochannel
12 km
Reactive Transport Modelling
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Mineral Systems• In detail for hard/soft rock systems......
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View from SECariewerloo Basin (top and bottom of Pandurra Formation draped on geology)
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Basementhighs
Basement+/- basin faulting
U-richHiltaba Suite
OlderReducingsediments
RestrictedSub-basins
PandurraFormation
Pandurra Formation – unconformity related U (key ingredients)
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Mineral Systems• In detail for IOCG systems......
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• Important characteristics for this class include Age, Tectonic Setting, Association with Igneous Activity, Structural Control, Morphology
• Three of the most important are alteration, mineralogy and structure
- Host rocks are intensely altered (sodic potassic, potassic or hydrolytic alteration)
- Abundance of Fe-oxide (not iron sulphides) and a suite of metals that may include U, Cu, Au, Ag, Mo, Co, As, Zn and minor REE’s
- Strong potential field characteristics – easily mappable!
Deposit Style
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Ernest Henry• Magnetite• K-feldspathization• Cpy• Breccia-hosted• Minor shearing
Sue Dianne• Hematite• K-feldspathization• Cpy-Bnt• Breccia-hosted
Olympic Dam• Hematite• Sericitization• Cpy-Bnt-Cct• Breccia-hosted
High T Low T
Reduced Oxidized
Deep (5-6 km) Shallow (<2 km)Courtesy BHP BilltonAnd Geordie Mark
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Olympic Dam
Geology and structure
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Contributors to the formation of Olympic DamRoxbyDownsGranite
OlympicDam
Co-evalfelsic
volcanismstructure
magmaticfluids
hydrothermalfluids
surficialfluids
Courtesy BHP Billiton
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Contributors to the formation of Olympic DamRoxbyDownsGranite
OlympicDam
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Proactive
Petratherm
EdenPerilya/Green
Rock
Eden
Eden
Eden
Scopenergy
Pacific Hydro
Petratherm
Geodynamics
South Australian heat flow anomaly
Scopenergy
Havilah
Electricity supply
GeothermalResources
As an aside........HOT GRANITES
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Heat Flow Profile across the Olympic Dam Deposit
HOT GRANITES
Courtesy Chris Matthews
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Geophysics – Total Magnetic Intensity00)POTENTIAL FIELD - MAGNETICS
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POTENTIAL FIELD - GRAVITY
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POTENTIAL FIELD - COMBINED
offset ofanomalypeaks
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S N
50 km
V=H
OD
Courtesy GeoscienceAustralia
Major ?Archaean/Proterozoic boundary beneath Olympic Dam and acoustically “bland” zone (fluid alteration?)
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Heinson, Direen and Gill, 2006
Graphite after CO2 degassing?
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POTENTIAL-FIELD INVERSION
1.5% “magnetite”Includes all susceptible minerals as their magnetite equivalent
0.5% “hematite”Includes hematite,sulfides, other dense minerals, and remanent magnetisation
25 km
N
Courtesy GeoscienceAustralia
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10 km
POTENTIAL-FIELD INVERSION
Courtesy GeoscienceAustralia
structural controlon magnetite –haematite
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Targeting of zones of (dilatant) high fluid flow eastern Gawler Craton
Courtesy Pmd*CRCAnd MonaxMining
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Mineral Potential Modelling
IOCG U Potential – Method• Area selection.
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IOCG U Potential – Method• Area selection.• Residual gravity and residual RTP TMI.
Mineral Potential Modelling
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IOCG U Potential – Method• Area selection.• Residual gravity and residual RTP TMI.• Contouring.
Mineral Potential Modelling
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IOCG U Potential – Method• Area selection.• Residual gravity and residual RTP TMI.• Contouring.• Selection of anomalies.
Mineral Potential Modelling
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IOCG U Potential – Method• Area selection.• Residual gravity and residual RTP TMI.• Contouring.• Selection of anomalies.• Determine geophysical highs - gravity.
Mineral Potential Modelling
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IOCG U Potential – Method• Area selection.• Residual gravity and residual RTP TMI.• Contouring.• Selection of anomalies.• Determine geophysical highs - gravity.• Determine geophysical highs -
magnetics.
Mineral Potential Modelling
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IOCG U Potential – Result
• The result, coincident gravity and magnetic anomalies offset by no more than 1 000 metres.
Mineral Potential Modelling
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Mineral Potential Modelling
IOCG U Potential – Uses
• Preliminary exploration site selection.• Key Ingredients Mapping:
– Coincident anomalies.– Hiltaba Granites.– Gawler Range Volcanics.– Faults.– Depth to basement.
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Mineral Potential Modelling
IOCG U Potential – Uses
• Preliminary exploration site selection.• Key Ingredients Mapping.• Mineral Potential Models:
– Weights of evidence.– Neural network.– Expert system.
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Mineral Potential Modelling
IOCG U Potential – Uses
• Preliminary exploration site selection.• Key Ingredients Mapping.• Mineral Potential Models:
– Weights of evidence.– Neural network.– Expert system.
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Olympic Dam
Carapateena
Mineral Potential Modelling
IOCG U Potential – Uses
• Preliminary exploration site selection.• Key Ingredients Mapping.• Mineral Potential Models.• 3D visualisation.
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Mineral Potential Modelling
IOCG U Potential – Uses
- Complexity of geoprocessing
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Mineral Potential Modelling
IOCG U Potential – Further Work
• Shape recognition properties:– Elongation– Compactness
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Mineral Potential Modelling
IOCG U Potential – Uses
- Extrapolating to other areas
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Mineral Potential Modelling – structural density
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Mineral Potential Modelling – peak anomalies
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Mineral Potential Modelling - overlapping U
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Summary
• South Australia has 40% of known resources in Uranium.
• Underlying Hiltaba event has generated the largest single uranium deposit in the world and subsequently........
• Overlying sedimentary successions provide excellent trap sites for world class projects ( eg. Four Mile).
• The Mineral Systems approach is a powerful predictive tool for undiscovered resources
Acknowledgments: Laz Katona, Tania Wilson, Goeoge Gouthas, Tania Dhu, Steve Petrie, Phil Heath (PIRSA), Geoscience Australia, pmd*CRC (CSIRO), Monax Mining