2015 broken hill resources investment symposium - geology survey of south australia - stephan thiel
TRANSCRIPT
Deep crustal architecture as a context for mineral discovery in the Curnamona. Stephan Thiel
Geological Survey of South Australia
Broken Hill Symposium, 27th May 2015
www.statedevelopment.sa.gov.au
UNCOVER – template for mineral exploration
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1. Characterising the cover
2. Australia’s whole lithosphere architecture
3. 4D geodynamic and metallogenic evolution
4. Characterising and detecting distal footprints
Themes Scale
Continental scale
Regional scale
Camp scale
Deposit scale
MT images from a few tens of meters to hundreds of kilometers
Exploration across scales
3 Department of State Development Groves & Santosh, 2015, GF Griffin et al., 2013, Nature Geoscience
Plume interaction with cratonic setting Generalised convergent margin settings
Fast vs slow mantle lithosphere
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Geodynamic model of the Tasmanides
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Moresi et al., 2014 Nature
Rawlinson et al., 2014 Geology
Seismic anisotropy due to slab roll back
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Broken Hill
Kate Robertson, U of A
Geophysical observables from the Gawler into Curnamona
Seismic reflection
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Flinders AusLAMP MT
8 Department of State Development Kate Robertson, U of Adelaide
Regional MT geotransects
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Peter Milligan, GA
Role of deep fluids in mineral genesis – reducing agent?
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Example of high-resolution (1 km) MT survey across Beverley U-mine
Is electrical resistivity a proxy for strain and metamorphism?
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Thiel et al., in prep
Extension
Compression 1
Present compression
Celerier et al., 2005, Tectonics
Terrane scale exploration - AusLAMP SA 50km grid
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AusLAMP extension – University of Adelaide
3D inversion 88 sites included in modelling with emphasis on data quality: • Red – new AusLAMP
sites • Blue – legacy long-
period MT sites • Open – yet to be
collected and included in modelling
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3D resistivity models
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Mantle fertilisation beneath the Gawler
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Rawlinson et al, 2014, Lithos
Terrane-scale
AusLAMP SA MT
Mantle-crust connection beneath Stuart Shelf
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20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200
0-10000-20000-30000-40000-50000-60000-70000-80000-90000
-100000-110000-120000-130000-140000-150000-160000-170000-180000
0-10000-20000-30000-40000-50000-60000-70000-80000-90000
-100000-110000-120000-130000-140000-150000-160000-170000-180000
Distance (Km)
Dept
h (m
)
1000
794
631
501
398
316
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200
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Ohm.m
Updated from Heinson et al., 2006
Regional-scale
Archaean core
Archaean core
Olympic Dam
Conclusions
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• AusLAMP SA will highlight the terrane to regional lithospheric architecture of the state
• Show fluid related metasomatism events (mantle) and fluid pathways (crust) conducive to “fertility corridors”
• MT needs better integration and analysis with reflection and passive seismic arrays with petrophysical constraints
• Fluid pathways appear structurally controlled and governed by geodynamic controls (stress, rheology)
• Future targeted camp-scale MT and other geophysical surveys will greatly benefit from the lithospheric architecture provided through AusLAMP SA
Stephan Thiel
www.statedevelopment.sa.gov.au
Department of State Development Level 4, 101 Grenfell Street Adelaide, South Australia 5000 GPO Box 320 Adelaide, South Australia 5001
T: +61 8 8204 1181 E: [email protected]
Acknowledgement • Philippa Mawby, Bruce Goleby and Geoff Axford (AusLAMP core field crew, University
of Adelaide), numerous students for field work • Katherine Betschart, Ian Hopton and David Love (DSD) for liaison and access • AARD for Aboriginal liaison • WPA, National Parks SA, traditional owners and numerous pastoralists for land
access • AuScope MT equipment pool