3D Integration of seismic, petrophysical and ...€¦ · 3D Integration of seismic, petrophysical...
Transcript of 3D Integration of seismic, petrophysical and ...€¦ · 3D Integration of seismic, petrophysical...
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3D Integration of seismic, petrophysical and lithogeochemicaldata to elucidate the effects of hydrothermal alteration on the
seismic response of the Lalor VMS footwall sequence
Ernst Schetselaar, Gilles Bellefleur, Nadjib El Goumi
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Direct and indirect seismic targets associated to a VMS deposit
hydrothermal vent
regional conformable alteration zone
massive sulphide orefelsic host rocks
mafic cover rocks sulphide stringer ore
Seismic Reflection:
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The Lalor VMS deposit: the ideal ‘laboratory’
Large hydrothermal alteration zone in proximal footwall of mineralization
Digital drill hole database, including >8000 whole-rock lithogeochemical analyses
Multi-method geophysical surveys
Physical rock properties
TGI4 3D seismic & gravity borehole surveys
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Lalor seismic & 3D modelling cubes
Bailes and Galley, 1999
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Hydrothermal alteration Lalor deposit
K-Fe-Mg assocation
K association
Less intense alteration
Balloch basalt
Lalor HW mafic rocks
Threehouse basalt S Ballochrhyodacite
N Ballochrhyodacite
FW basalt
100 m
10 Lens
20 lens
Gold zone
Massive sulphides
Mg-Ca association
Mg-Fe association
sericite-pyrite-biotitekyanite
anthophyllite-cordierite-garnet-biotite-staurolite
quartz-biotite-kyanite
carbonate-chlorite withCa-Mg amphiboles
Caté et al. 2013
ρ1
ρ2ρ3?
W E
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Seismic detection of sulphide ore
time slice at 283 ms (approx. 835 m)
Crossline
Inline
1000
1150
1000
1350
1075
Inline
1000
1150
1075
1175
Crossline
1000
1350
1175
1 km
1 km
F1
FW HW
H7
H6
H3
H5H5?
10, 11, 20F2
?
21
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Seismic synthetics
Synthetic traceOre zone
NESW
T/DDUB245
(2 Points)
0.10
0.20
0.30
500
1000
T-D Chart
5800 6000
LogVelocity(m/s) (g/cm)3
5000 7000
Density
2.62.9 3.2
AI
20000
RC
-0.1 0.1
WaveletExtracted
Ref. log Synthetic Synthetic(Density) (+) (-)
TraceLalor_3D_DMOMIG
Inline:1088, Crossline:1196
Borehole
-400 0
Near-vertical incidence synthetic seismic trace.
and geological model (Inline 1085 DMO-poststackSynthetic seismic trace overlayed on seismic
migrated volume).
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History of VMS footwall rocks1. Volcanic deposition 1.89 Ga
2. Hydrothermal alteration & mineralization 1.88 Ga
3. Tectonic deformation and metamorphism 1.81 Ga
All these processes effect physical rock properties. Can we isolate the effects of hydrothermal alteration?
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Building a curvilinear-faulted grid
1
34
5
6
2
Subsurface Knowledge Unified Approach
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3D modelling of geologic surfaces to define the geometry of the curvilinear grid
strike/dip s0 restored from bedding-core angles (Bailes, 2012)
lithofacies recoded from Hudbay drill logs
Unit contacts from geologic map (Bailes et al, 1993)
lithostratigraphicmarkers from drill logs (Bailes 2012)
3D geologic surface model Lalor deposit
NE SW
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Building a curvilinear grid from geological surfaces
NE SW
Nominal cell size: 20 x 20 x 5m
Chisel-Lalor fault
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Advantages of defining a curvilinear grid for modelling properties
Subsurface Knowledge Unified Approach
Mallet 2004
Dulac 2008
Numerical grid modelling, including structural analysis (characterization of spatial autocorrelation) is conditioned by the modelled geological structure
uvt transform (Mallet, 2003)
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simulated density 1 simulated density 2 simulated density 3
Methods for filling the uvt grid
kriged lithofacies kriged density kriging variance
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3D grid modelling to interpret relationships lithology, alteration & seismic amplitude
3D curvilinear grid
3D CCPI alteration model
3D Lithofacies model
SW
3D geological surface model
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Lithofacies modelling, input drill hole data
82 rock classes 15 rock classes
Zr/TiO2 <= 0.013 basalt mafic fragmentals - tuff mafic gneiss/schist
0.013< Zr/TiO2< 0.019 dacite dacitic fragmetals - tuff interm. gneiss./schist
Zr/TiO2>=0.019 rhyolite/rhyodacite felsic fragmetals - tuff felsic gneiss schist
sulphide ore argillite diorite/gabbro
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Lithofacies modelling, systematic classification
1 MAFVR mafic volcanic rock (basalt, andesite)
2 INTVR intermediate volcanic rock (dacite)
3 FELVR felsic volcanic rock (rhyolite, rhyodacite)
4 VCLCM mafic coarse-gr volcaniclastic rocks (fragmentals)
5 VCLCI intermediate coarse-gr volcaniclastic rocks (fragmentals)
6 VCLCF felsic coarse-gr volcaniclastic rocks (fragmentals)
7 VCLFM mafic fine-gr volcaniclastic rocks (tuff/lapili tuff)
8 VCLFI intermediate fine-gr volcaniclastic rocks (tuff/lapilli tuff)
9 VCLFF felsic fine-gr volcaniclastic rocks (tuff/lapilli tuff)
10 GNSCHM gneiss/schist mafic protolith
11 GNSCHI gneiss/schist intermediate protolith
12 GNSCHF gneiss/schist felsic protolith
13 ORE sulphide ore
14 ARG argillite
15 DIO feldspar-phyric diorite/gabbro intrusions
COHERENT VOLCANICROCKS
COARSE VOLCANICLASTIC ROCKS (FRAGMENTALS)
FINE VOLCANICLASTIC ROCKS (LAPILLI TUFF /TUFF)
Zr/TiO2 < =0.013
0.013 < Zr/TiO2 < 0.019
Zr/TiO2 >= 0.019
Zr/TiO2 < =0.013
0.013 < Zr/TiO2 < 0.019
Zr/TiO2 >= 0.019
Zr/TiO2 < =0.013
0.013 < Zr/TiO2 < 0.019
Zr/TiO2 >= 0.019
Zr/TiO2 < =0.013
0.013 < Zr/TiO2 < 0.019
Zr/TiO2 >= 0.019
GNEISS / SCHIST(UNRECOGNIZABLE PROTOLITH)
REMAINING CLASSES
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strongest intensity ofhydrothermal alteration
Can we see the effects in 3D lithofacies-seismic amplitude model?
Zr/TiO2 <= 0.013 basalt mafic fragmentals - tuff mafic gneiss/schist
0.013< Zr/TiO2< 0.019 dacite dacitic fragmetals - tuff interm. gneiss/schist
Zr/TiO2>=0.019 rhyolite/rhyodacite felsic fragmetals - tuff felsic gneiss schist
Cate et al., 2013W E
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Impedance contrast hanging wall unaltered versus footwall altered rocks
hanging wall rocks altered footwall rocks
Ỵ-Ỵ density g/cm3 Ỵ-Ỵ density g/cm3
Zr/TiO2 <= 0.013 basalt mafic fragmentals - tuff mafic gneiss/schist
0.013< Zr/TiO2< 0.019 dacite dacitic fragmetals - tuff interm. gneiss./schist
Zr/TiO2>=0.019 rhyolite/rhyodacite felsic fragmetals - tuff felsic gneiss schist
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Vp-density plots borehole geophysical logsV
p (m
/s)
ϒ-ϒ density (g/cm3)
Y-Y densityVp seismic velocity
log sample, n = 67657rock sample, n=42
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Co-locating geophysical borehole logs with lithogeochemistry samples and lithology logs
100 (K2O + MgO)
(K2O + MgO + Na2O + CaO)AI =
100 (MgO + FeO)
(MgO + FeO + Na2O + K2O)CCPI =
ALTERATION INDICES
Drill path
HOLEID Depth ρ Vp Vs Zr/TiO2 CCPI AI LithologyDUB202 831.3 2.49 5421 3289 0.009 87 55 basalt flowDUB202 831.5 2.52 5345 3560 0.009 87 55 basalt flowgeophysical
log datum
1259 of 67657 geophysical log samples (1.9 %) are co-located with geochemical samples within 30 cm
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Vp- density plot felsic-intermediate rocks, FW
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Vp - density plot mafic rocks, footwall
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Seismic Impedance vs. Alteration Box Plot
seismic impedance (kg.m-2.s-1 x 10-6)
hanging wall
footwall
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3D model seismic amplitude and CCPI index
CCPI (%)
footwall
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Conclusions: effects of hydrothermal alteration
Protoliths: density contrasts preserved, acoustic impedance contrast and seismic reflectivity are enhanced
Dominant effect hydrothermal alteration is increase in Vp
Increase in Vp is correlated with CCPI and AI.
Effects are likely due to low density-high velocity Ca-Mg & Fe-Mg alteration minerals (dolomite, anthophyllite)
Follow-up seismic forward modelling and mineral physical property studies required
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Conclusions (integration methodology)
3D data integration instrumental for ore system science
We need co-located samples of lithofacies, mineralogy, lithogeochemistry and petrophysics to calibrate, model and validate
Modelling properties of a curvilinear-faulted grid (Skua) essential to obtain realistic results in hard rock settings
We are equipped these days with sophisticated data-driven methods ….. but we are still searching for a needle in a hay stack if we do not understand how ore forming processes effect our data
We need to pool highly-specific expertise in economic geology, mineralogy, geochemistry, petrophysics and geophysics
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Acknowledgements
Antoine Caté, Patrick Mercier-Langevin
Alan Bailes, Bailes Geoscience
Matt Salisbury
Randy Enkin
Craig Taylor, Peter Dueck, Hudbay Minerals
gOcad research consortium