2015 Broken Hill Resources Investment Symposium - University of Adelaide - David Giles
Transcript of 2015 Broken Hill Resources Investment Symposium - University of Adelaide - David Giles
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What’s out there and how to find it?
Broken Hill Exploration Symposium Technical Day 27 May 2015
David Giles Program 3 Leader Deep Exploration Technologies CRC The University of Adelaide
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Overview Focus on BHt and Cu-Au systems
Scale reduction • including a time element as well as the critical spatial
element
• what we think we know about the systems at each scale
• what tools can we apply to reduce to the next scale
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Broken Hill type systems
Regional Scale The Curnamona (and especially the BHB) is a small part of a much larger system Spatial – hot, strangled rift on continental lithosphere Spatial/temporal – salt in the basin (paleogeography) Temporal – sulphate available in the oceans
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Hot, throttled rift on continental lithosphere
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Broken Hill type systems
Hot “throttled” rift on continental lithosphere
• Syn-depositional bimodal magmatism
• High Fe-Ti mafic rocks
• Relatively juvenile turbidites fill basin
• Salt
• High preservation potential if rift fails
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Salt in the basin (paleogeography)
• Evidence of evaporites in footwall sequences
from Idnurm (2004)
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Sulphate available in the oceans
from Huston and Logon (2004)
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Broken Hill type systems Camp Scale Spatial – Rift architecture Spatial/temporal – Magmatic centre, heat (+ fluid?) source Spatical/temporal – Seafloor at critical time interval (stratigraphy)
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from Connor and Preiss (2008)
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Broken Hill type systems What about High T – Low P metamorphism and deformation?
• Coincidental not causative
• But critical for coarse grain size and local enrichment
• Highly likely (inevitable?) in tectonic setting • Some degree of deformation required to exhume from
bottom of basin HAVE WE PROPERLY SEARCHED FOR OFF RIFT AXIS OR HIGHER STRATIGRAPHIC LEVEL, LOW METAMORPHIC GRADE EQUIVALENTS?
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Underexplored!
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Broken Hill type systems Target Scale (all spatial) Geophysics
Gravity for dense sulphides + garnet-rich halo Magnetics for magnetite (if present) EM for conductive sulphides All prone to identifying false positives
Geochemistry
Kilometric alteration zones (vectoring?) Matched zones of depletion and enrichment in stratigraphy Blank sheet lithologies
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Geophysics
• Clearly can work
• defining prospective stratigraphy
• Targeting – but does generate false positives
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• BHt systems have large geochemical footprint
• Matching depleted and enriched horizons
• Blank sheet lithologies
Geochemistry undercover
requires dense sampling
within the mineral system
Geochemistry from Groves et al (2009)
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Cu-Au systems
Regional Scale The Curnamona (and especially the BHB) is a small part of a much larger system Spatial/temporal – significant regional thermo-magmatic event Spatial/temporal – salt in the basin (no prior orogenesis)
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Significant regional thermo-magmatic
event at ~1590 Ma
from Reid et al (2014)
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Cu-Au systems Camp Scale Spatial – Lithospheric structural architecture controls flow of melt and fluid Spatial/temporal – Magmatic centre, heat + fluid source Spatial/temporal – Importance of crustal level
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S-type U-enriched I-type
S-type WSG source
U-enriched Fractionated A-type
BRVs at ~1590Ma
Paleosurface and unconformity
Mafics?
from Wade (2011)
from Williams and Betts (2008)
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Cu-Au systems Target Scale (all spatial) Geophysics
Gravity for dense oxides Magnetics for magnetite IP for chargeable sulphides and oxides All prone to identifying false positives
Geochemistry
Kilometric alteration zones (IOCG alteration index)
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• Clearly can work
• Highlights Fe-oxides (not Cu-Au)
• Many false positives
Geophysics
from Belperio (2001)
from Katona (2010)
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Geochemistry undercover
requires dense sampling
within the mineral system
Geochemistry
• Cu-Au systems have vast
geochemical footprint
• Nested halos of (mostly) chalcophile
elements
• But one drill hole won’t do the job…
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Mineral Systems Drilling Program