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Geological Survey of South Australia -Industry presentation delivered at the 4th annual Resources Investment Symposium held in Broken Hill NSW Australia, 26-28 May 2014.
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From paddling in the bathtub to swimming the deep ocean: the reality of this exploration metaphor in the Curnamona Province and adjacent regions
Steve Hill
Director
Geological Survey of South Australia
OPEN THE DOOR TO SOUTH AUSTRALIA
Murphy’s “Haystacks” (Photo: S.Hill)
Pre-competitive Geoscience Data… finding mineral system “Haystacks”
Moon Plain, Stuart Shelf, SA (Photo S.Hill)
Deep Cover Exploration Impediment…
Love thy Enemy• Lots of cruel things said about the cover….• “Impediment”• “punch through” it!• The rocks “suffered” weathering• Ignore it• “Stuff”• “Overburden”• “Crud”• “Dirt”• “*^#>” !!!
4
Why are people so unkind?Fear and loathing. Where does it come from?We don’t know it properly?We don’t trust it
Be a Cover Lover!
5
This presentation1. Geological Processes in the Cover (What are some of the
special things that can happen?)
2. Implications of these processes (How the cover can be our BFF)
3. Characterising the cover (What do we really know about our new found love?)
4. How to get to know the cover better into the future (our enduring love)
5. Cover savvy geoscientists of the future (Who will be part of this love affair?) 6
Geological Processes in the Cover: What are some of the special things that can happen?
• Weathering / erosion / sediment and element accumulation• Element mobility – source, transport, accumulation,
preservation• Supergene enrichments• Biogeochemical processes• Placer concentration and recycling• Geochemical footprint enlargement• -------------------------------------------• Dilution• Barren cover (‘blind” deposits)• Erosion / poor preservation
7
Weathering
ErosionSedimentation
PreservationLeaching
Poor PreservationPhysical Dispersion
BurialRe-accumulation(“False anomaly”)
DynamicEquilibrium
Cover Processes and MaterialsWeathering
ErosionSedimentation
PreservationLeaching
DenudationPhysical Dispersion
BurialRe-accumulation(“False anomaly”)
DynamicEquilibrium
Weathering
ErosionSedimentation
In situDeep
Weathering“Residuum”
Variable profile Materials exposed
Sediments /Transported
material
PROCESS
MATERIAL
Gossans
Ferricrete
Weathered Fe-skarn
Kaolinised Granite
Joints / Faults
Basal Gravels
Reduced/Oxidised clays & sands
Regolith CarbonatesBarren aeolian sands
Supergene Cu zone
HILLSIDE REGOLITH PROFILE
Tunkillia biogeochemical model
(Lowrey & Hill, in prep.)
Central Gawler CratonDeep cover Plant biogeochemistry
UoA Honours studentsBlack oak sampling April 2009
Minotaur ExplorationDrilling April 2010
Tunkillia, Gawler Craton
Implications of these processes: How the cover can be our BFF
• Haloes / footprints
• 3D dispersion
• Secondary accumulations
• Other resources • e.g groundwater, soils …..
12
After R E Smith & B Singh, 2007
Implications of these processes: How the cover can be our BFF
14
• Eastern Gawler Craton – Curnamona Province links
• ~1590 Ma mineralising event
But dominated by differentexploration strategies
Eastern Gawler: IOCG in basementCurnamona: sedimentary U
IOCG – Porphyry – Epithermal Continuum (Claire Wade, GSSA)Into the overlying cover???
Curnamona Province dispersion haloes shown on radiometrics image
16
Mt Painter
Broken Hill
50 km
Scale of the distal footprint of the Broken Hill mineral system
• Lateral dispersion for >100 km– High grade garnets in beach sands
at Menindee Lakes (>100 km to SE)
– Staurolite and other high grade metamorphic minerals in sediments overlying low-grade metamorphic rocks in the Fowlers Gap and Bancannia Basin (>100 km to N)
–Lateral dispersion onto Mundi Mundi Plains (30-50 km to W and NW)
Catchment headwaters within Barrier Ranges
Mundi Mundi Plains
Umberumberka Reservoir
Umberumberka Creek - Broken Hill (Charlotte Mitchell, DET CRC)
Catchment headwaters within Barrier Ranges
Mundi Mundi Plains
Umberumberka Reservoir
Umberumberka Creek - Broken Hill (Charlotte Mitchell, DET CRC)
Mundi Mundi Plain• Lateral dispersion
and reaccumulation
• Important balance between processes of erosion, sedimentation and weathering / soil formation
Characterising the cover: What do we really know about our new found love?
• Characterising the cover – a big opportunity!
• Greater amount of surficial data but really decreases with depth
• Key attributes:• Detailed lithological logging• Whole-rock geochemistry (chemical context?)• Mineralogy (XRD and spectral)• Physical properties
21
Deep Cover Reference Sections
• Geological type sections and their associated data have received diminished attention, particularly since the GSSA work in basin areas in 1970s and 1980s
• These are important reference sections, particularly as exploration moves into surrounding covered areas.
• Modern data for these sections can include:• GPS coordinates• Lithological logging• Biostratigraphy• HyLogger mineralogy• Lithogeochemistry• Detrital zircon dating• et al……
22
Trinity Well type section, Marree 1:250k mapsheet
23
Trinity Well Reference Section
24
Deep cover atlas of SA (DET CRC)…
25
Exploration Sampling Media within the Cover (DET CRC)
• An ideal sampling medium needs to be:• Abundant• Generic (e.g. not just restricted to a particular stratigraphic
unit)• Readily identifiable (esp. down-hole)• Hosts target geochemical suite for mineral system • Can be linked to dispersion vectors (can be used as
geochemical vector to mineralisation)• Able to be effectively and efficiently sampled
Some examples of efficient and effective approaches to exploring
in covered terrains?
1. Understanding the geological history of gold dispersion at Tibooburra
2. Exploring through sediment for Broken Hill type mineralisation at the Pinnacles
3. Putting it all together for sedimentary uranium exploration through the cover at Four Mile
CASE STUDY 1: Tibooburra Au provenance...
Tors of Tibooburra Granodiorite (photo S.Hill)
Tibooburra-Milparinka Au-fields (Thomson Orogen NSW)From Hill et al 2009
Tibooburra-Milparinka Au-fieldsDepth of Basin Cover (Mesozoic and younger)
From Hill et al 2009
Radial ‘shedding’ modelTibooburra Inlier
No! This applies to contemporary drainage but not the Mesozoic system
Mesozoic hinterland-basin geochemical reconstruction needed!
Au hosted in basal Mesozoic sediments
(Hill, 2005)
Late Jurassic(basal Mesozoic) palaeolandscape
Au-bearing Basal Mesozoic palaeocurrent vectorsTibooburra Inlier (Hill et al 2009)
Tibooburra: Mesozoic palaeoflow model in relation to historic Au diggings (Hill et al 2009)
Emergent
.The Granites. Easter Monday
. Tunnel Hill
. Six Mile
Deeply buried Au Provenance? (Hill et al 2009)
Mt Browne Inlier
Au bearing Basal Mesozoic flow vectors
Buried Au source target areas
Tibooburra Inlier
Deeply Buried Au Provenance?
Tibooburra Inlier
NSW GS, 1VD magnetics
Mt Browne Inlier
CASE STUDY 2: The Pinnacles …
Looking South down Pine Creek from Middle Pinnacle
Pinnacles Mine
Pine CreekSouth
Pinnacle
S.Hill Pinnacles pilot study: river red gum leaves (~250 m sample spacing)
0
50
100
150
200
250
300
350
0 2 4 6 8 10 12
Channel Distance (km)
Pb
(p
pm
) Pinnacles mineralisation?
Wasn’t sure if this staggering result was current mine or new mineralisation? What does an academic do when they don’t know something? ……
Get a PhD student to work on it –Karen Hulme
Pine Creek… Sample spacing – every collectable RRG
• 215 River Red gums sampled– Media
• Leaves• Chest height• Sample size~300g
Middle Pinnacle
Pinnacles Mine
Staurolite Ridge
Pin
e
Creek
Lead…
•Pb up to 205 times background levels
•Geochemical footprint ~ 2.5 km
0 – 36 ppm
37 – 99 ppm
100 – 190 ppm
191 – 411 ppmHyperspectral Image, courtesy NSW DPI
N2 km
Silver…
• Ag up to 136 times background value
• Geochemical footprint 2.2 km
0.005 – 0.100 ppm
0.101 – 0.340 ppm
0.341 – 0.710 ppm
0.711 – 1.360 ppm Hyperspectral Image, courtesy NSW DPIN
2 km
Zinc…
• Zn up to 7 times background values
• Erratic pattern (repeated)– mobility– peaks related to
floodouts
17 - 47 ppm
48 - 80 ppm
81 - 141 ppm
141 – 338 ppm Hyperspectral Image, courtesy NSW DPIN
2 km
It was time to dig… Sarah ‘Gibbo’ Gibbons (earnest, hard-working CRC LEME Honours student)
Photos: Karen Hulme
Pinnacles - lodes extensions
Photographs: Steve Hill Mineralisation continues near surface but below main road!
Kangaroo Prospectors– Western Grey Kangaroos
• Selective browser• Well defined home range• Scat chemistry reflects Broken Hill mineralisation (esp. Pb, Zn, Cd)• Implications for exploration and geo-health
Kangaroo Prospectors
Broken Hill Roo Poo Pb
0
100
200
300
400
500
600
700
-60 -40 -20 0 20 40 60
Dist (km)
Pb
(p
pm
)
Broken Hill
West East
Pinnacles
Zn and Cd in roo poo
Broken Hill Roo Poo Zn
0
200
400
600
800
1000
1200
-60 -40 -20 0 20 40 60
Dist (km)
Zn
(p
pm
)
Broken Hill Roo Poo Cd
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
9.0
10.0
-60 -40 -20 0 20 40 60
Dist (km)
Cd
(p
pm
)
Broken HillBroken
Hill
West East West East
Skippy knows where to find the ore?
• The kangaroos very effectively intake chemical signatures from buried rocks when they eat plants.
• They do this over a range of 10s of kilometres• They redeposit this chemical signature in their
poo• Mineral explorer samples the poo, prepares it
and gets it analysed to look for its chemical signatures
CASE STUDY 3: Four Mile U(Steve Hore & Steve Hill, GSSA)
Four Mile East
Dead Tree SectionFour Mile Creek
Four Mile West
Beverley
F
Four Mile East
Dead Tree Section – Eyre Formation sample locations
20m
Four Mile West: Deadtree Section
Namba Fm
Pedogenic Silcrete
Eyre Fm
Bulldog Shale &Cadna-owie Fm
Saprolite
(Hill, 2005)
Late Jurassic
Mesozoic Glaciations• Widespread dispersal of U-rich detritus in
Early Cretaceous glaciers
Recorder Hill
Mesozoic Glaciations• Important context for Four Mile West U
deposit
Palaeoredox interfaces in Mesozoic diamictite at Deadtree section (Hore & Hill, 2009)
(Hill, 2005)
Early Cretaceous
Mt Babbage Inlier(U-rich granites)
Oxidised Bulldog Shale
Mt Babbage Inlier
U-rich bedrock
Mesozoic sediments
(Hill, 2005)
Palaeogene
Eyre Formation (Palaeogene)
• Flinders Ranges existed at this time– Palaeoflow along range-front (rather than across it!)– Highly weathered provenance
• Warm-wet palaeoclimate– Abundant vegetation cover– Weathering rate > erosion rate– Organic detritus
Eyre Formation (palaeo-redox fronts) – Important U host (Four Mile, Honeymoon, Goulds Dam, Oban)
Namba Fm (Miocene) – hosts Beverley
Namba Formation
Top of Namba Fm
Top of Saprolite(Wooltana Volcanics)
Willawortinna Fm outwash gravels
(Hill, 2005)
Neogene
Proterozoic basementWillawortina Ftm
Eyre Formation
geologists
~ 5 km
Four Mile East
Four Mile West
?
?
~ 5 km
~ 5 km
Preserved Tertiary
Exposed Mesozoic
Four Mile Stream Sediments (GSSA Radiometrics)
NB. High U content of detritus from ranges overlying basin prospective for buried sedimentary U
Four Mile Prospect soil U
Neimanis et al 2007
Four Mile Stream Sediments (McMahon & Hill, 2007)
0
20
40
60
80
100
120
0 1000 2000 3000 4000 5000 6000 7000
Sample distance downstream (m)
U (
pp
m)
Fine sediment fraction(-80 mesh)
Mineralisation surface projection
Four Mile Regolith Carbonates (Gallasch & Hill, 2007)
Media Comparison of U vs Th (Four Mile Catchment)
0
50
100
150
200
250
300
350
0 50 100 150 200 250 300
U (ppm)
Th (ppm)
Carbonate
Bedrock
Th > U
U > Th
Radium Ridge
Image: Steve Hill
Eucalyptus gillii
0.12 – 6.59 ppm U
4.79 – 33.42 ppm Cu
0.01 – 0.02 ppm ThEucalyptus intertexta
0.06 – 6.49 ppm U
2.74 – 12.21 ppm Cu
0.01 – 0.04 ppm Th
FOUR MILE BIOGEOCHEMISTRY: TARGET SPECIESAllows subsurface access to culturally and environmentally sensitive sites
River Red Gum
Inland tea-tree
Neimanis, Hill & Hore, 2007
Inland Tea-tree shows similar results to stream sediments!(shallow alluvial aquifer)
Neimanis, Hill & Hore, 2007
River red gum shows deeper mineralisation expression along structures(deeper fractured aquifer)
U2 / Thriver red gum
leaves
Ant biogeochemistry (Iridomyrmex spp.)
Meat Ant Distributionwww.ento.csiro.au/science/ants
Courtesy Deanne Gallasch
Ant Nest Soils
Projected MineralisationLegend
Uranium (nest material)
Value (ppm)
3.5 - 30.0
30.1 - 57.0
57.1 - 118.0
´0 1,000 2,000500
Metres
GRID NORTHGDA 1994 (Zone 54)
351500.000000 352500.000000
353500.000000
353500.000000
354500.000000
354500.000000
355500.000000
355500.000000
356500.000000
356500.000000
357500.000000
357500.000000
358500.000000 359500.000000
666
00
00.0
00
00
066
61
00
0.00
00
00
666
20
00.0
00
00
066
63
00
0.00
00
00
666
45
00.0
00
00
066
65
50
0.00
00
00
666
65
00.0
00
00
0
(Jennings, Hill, Wright & Kirby, 2007)
Ant Biogeochemistry (Jennings, Hill, Wright & Kirby, 2007)
Projected MineralisationLegend
Uranium (ants)
Value (ppm)
0.027 - 1.417
1.418 - 4.302
4.303 - 13.035
´0 1,000 2,000500
Metres
GRID NORTHGDA 1994 (Zone 54)
351500.000000 352500.000000
353500.000000
353500.000000
354500.000000
354500.000000
355500.000000
355500.000000
356500.000000
356500.000000
357500.000000
357500.000000
358500.000000 359500.000000
666
00
00.0
00
00
066
61
00
0.00
00
00
666
20
00.0
00
00
066
63
00
0.00
00
00
666
45
00.0
00
00
066
65
50
0.00
00
00
666
65
00.0
00
00
0
Roo Poo Biogeochemistry (McMahon & Hill, 2007)
86
Four Mile Uranium: summary
• Long history of U dispersion (at least Mesozoic) across landscape
• Abundant surface anomalism but links to buried mineralisation challenging
• Vegetation and to some extent carbonates have best links with buried mineralisation (via groundwater)
So what have we learnt
• The cover can be our friend and host some advantages to exploration (e.g. enlarged “footprints”)
• The cover needs to be dealt with the same geological rigor as hard rocks (e.g. palaeodrainage reconstruction)
• A range of sampling media are available within the cover and be efficiently and effectively used in different ways (e.g. the provide an exploration tool kit)
Plant biogeochemistry providing surficial expression of sub-surface chemistry
Biogeochemistry
→
Cost and Time efficient subsurface chemical information(help focus and rank drilling targets)
Advantages of plant biogeochemical exploration
• Provided sampling procedure is orientated and systematic:• Time efficient• Minimal environmental impact• Minimal cultural impact• Flexible site access needs• Cost equivalent to soil geochemistry
Cover savvy geoscientists of the future: Who will be part of this love affair?
• Part of integrated geoscience workflow• Given the expanse of cover …. Where are our
cover savvy geoscientists coming from?• Are training institutions engaged and providing
the relevant foundations?
91
Photo: Steve Hill92
Western Gawler Craton – Eucla Basin….
South Australian Mineral Exploration Licences
January 2004 September 2013
Pre-competitive Geoscience workflow for western Gawler Craton – Eucla Basin
94
Regional GeophysicsRegional Geochemistry
Regional Geological MappingLithospheric Architecture
Stratigraphic Drilling250k Geological Mapping
Targeted Geophysics and Geochemistry4D Geodynamic & Metallogenic evolution
Regional Mineral System DrillingGeophysical & Geochemical Case studies
‘Distal Footprint’ Characterisation
Mineral Occurrence StudiesCollaborative / Targeted drilling
Tenement Exploration
PACE FRONTIERS in 2014• Eucla Seismic Line• Regional MT survey• New airborne geophysics• Regional Biogeochemistry
Western Gawler / Eucla Basin Continental Seismic Transect (TMI backdrop)
95
CoompanaAnomaly Fowler
DomainGawlerRanges
Eucla Basin – Gawler Craton MT
Western Gawler / Eucla Basin Regional Geophysics
• Magnetics
• RadiometricsOlder airborne surveys1600-3000 line spacing(did not always collect radiometrics)
Western Gawler / Eucla Basin Geochemistry / Biogeochemistry
• Regional Geochemistry– 2013-14
• Hydrogeochemistry• Soil • Calcrete • Biogeochemistry
~450 plant samples~170 sample sites
Western Gawler / Eucla Basin Future Program
• Gravity survey• Soil Geochemistry• Integration, Interpretation and value-add• REGIONAL DRILLING
• Coompana Competition?• Phase I: service provider data acquisition• Phase II: Geological Interpretations• Phase III: Regional Drilling and ‘real time’ reinterpretations
Thank-you….
Yours LovinglySteve
(Your Cover Lover Brother)
101
DisclaimerThe information contained in this presentation has been compiled by the Department for Manufacturing, Innovation, Trade, Resources and Energy (DMITRE) and originates from a variety of sources. Although all reasonable care has been taken in the preparation and compilation of the information, it has been provided in good faith for general information only and does not purport to be professional advice. No warranty, express or implied, is given as to the completeness, correctness, accuracy, reliability or currency of the materials.
DMITRE and the Crown in the right of the State of South Australia does not accept responsibility for and will not be held liable to any recipient of the information for any loss or damage however caused (including negligence) which may be directly or indirectly suffered as a consequence of use of these materials. DMITRE reserves the right to update, amend or supplement the information from time to time at its discretion.