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3D Model of a Ni-Cu-PGE Ore Body
MINERAL RESOURCES
Margaux Le Vaillant, June Hill and Stephen J. Barnes
May 2017
The Kevitsa Cu-Ni-Au-PGE mine, northern Finland
Layered Intrusions
A simplified ore body model | Margaux Le Vaillant and June Hill2 |
• Repositories of some of the largest ore
bodies on earth of Cu, Ni PGE, Cr, V…
• Large intrusions presenting
compositional layering
 This layering gives us
information on the genetic
magmatic processes at
play…
 Need for a meaningful way
to visualise these variations
in 3D
Kevitsa Intrusion
A simplified ore body model | Margaux Le Vaillant and June Hill3 |
Kevitsa Ore
A simplified ore body model | Margaux Le Vaillant and June Hill4 |
plag
ol
px
sulf
Kevitsa 3D Model
A simplified ore body model | Margaux Le Vaillant and June Hill5 |
Variations within the intrusion poorly
modelled
Kevitsa 3D Model
A simplified ore body model | Margaux Le Vaillant and June Hill6 |
 But access to a gigantic assay database! (>92,000 analyses)
Variations within the intrusion poorly
modelled
Ore Classification
A simplified ore body model | Margaux Le Vaillant and June Hill7 |
Ni < 2% - ‘False Ore’
S < 0.5% - ‘Not Ore’
Ni > 2% and Pd > 1,500 ppm
‘Normal Ore – High Pd’
Ni > 2% and Pd < 1,500 ppm
‘Normal Ore – Low Pd’
Ni > 10%
‘High Ni-PGE Ore’
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill8 |
Assay points visualised and classified individually / no ‘lumping’ or domaining
A simplified ore body model | Margaux Le Vaillant and June Hill9 |
3D visualisation
Need for an objective & fast simplification of the model in order to distinguish
the large scale variations from the small scale one
 Upscaling method using continuous wavelet transform (CWT) and
tessellation methods
WORKFLOW
Multiscale Boundary Detection
A simplified ore body model | June Hill10 |
Signal
Signalsmoothing
Increasingscale
Multiscale Boundary Detection
A simplified ore body model | June Hill11 |
Signal
Signalsmoothing
inflection point in signal:
best estimate of
boundary location
Increasingscale
many boundaries
few boundaries
A simplified ore body model | June Hill12 |
continuous wavelet transform
using
2nd derivative of Gaussian wavelet
(convolve wavelet with signal over range of scales)
(smooth & find inflection points)
Method
zero contours of
2nd derivative
A simplified ore body model | June Hill13 |
Multiscale Spatial Domaining
“Tessellation”
of
continuous wavelet transform
Method
involves
depth-correction of
zero contours
A simplified ore body model | June Hill14 |
signal Filter One scaleTessellation
A simplified ore body model | June Hill15 |
Combine
Domain
Boundaries
A simplified ore body model | June Hill16 |
Classify
Combined
Domains
Classification
by Domain
vs Interval
A simplified ore body model | June Hill17 |
Low S
High S, Low Ni
Mod Ni, Low PGE
Mod Ni, High PGE
High Ni
ORETYPES
IntervalDomain
Effect of
Filtering Level
A simplified ore body model | June Hill18 |
Low S
High S, Low Ni
Mod Ni, Low PGE
Mod Ni, High PGE
High Ni
ORETYPES
Weak filter Strong filter
50% 70%
Effect of
Filtering Level
A simplified ore body model | June Hill19 |
Low S
High S, Low Ni
Mod Ni, Low PGE
Mod Ni, High PGE
High Ni
ORETYPES
weak changes disappear
strong changes are preserved
Filter
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill20 |
unfiltered
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill21 |
70% Filtered
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill22 |
Unfiltered
100
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill23 |
70% Filtered
100
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill24 |
Unfiltered
3D visualisation
A simplified ore body model | Margaux Le Vaillant and June Hill25 |
70% Filtered
Interpretation
A simplified ore body model | Margaux Le Vaillant and June Hill26 |
A simplified ore body model | Margaux Le Vaillant and June Hill27 |
Interpretation
Genetic Model
A simplified ore body model | Margaux Le Vaillant and June Hill28 |
Interconnected sill sediment-complex choked with
country rock inclusions
Genetic Model
A simplified ore body model | Margaux Le Vaillant and June Hill29 |
Larger magmatic chamber
Genetic Model
A simplified ore body model | Margaux Le Vaillant and June Hill30 |
Freely convecting magma chamber
Genetic Model
A simplified ore body model | Margaux Le Vaillant and June Hill31 |
Conclusions
A simplified ore body model | Margaux Le Vaillant and June Hill32 |
• Consistent and objective reduction of the number of
units in each drill hole, and creation of a simplified
3D model of the orebody
 Insights on the genetic processes at play
• Advantages of automated domaining process:
 Consistent results over whole data base
 Time saving
• Domaining using CWT and tessellation results in
domains whose size is a reflection of the location of
major changes in the variable values – not fixed
length like in conventional compositing of drill holes
A simplified ore body model | Margaux Le Vaillant and June Hill33 |
Thank you!
A simplified ore body model | June Hill34 |
35 |
S NiS PdIntervals Domains
Low S
High S, Low Ni
Mod Ni, Low PGE
Mod Ni, High PGE
High Ni
A simplified ore body model | Margaux Le Vaillant and June Hill
Making Sense of the Results

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3D model of a Ni-Cu-PGE ore body - Margaux Le Vaillant and June Hill (CSIRO)

  • 1. 3D Model of a Ni-Cu-PGE Ore Body MINERAL RESOURCES Margaux Le Vaillant, June Hill and Stephen J. Barnes May 2017 The Kevitsa Cu-Ni-Au-PGE mine, northern Finland
  • 2. Layered Intrusions A simplified ore body model | Margaux Le Vaillant and June Hill2 | • Repositories of some of the largest ore bodies on earth of Cu, Ni PGE, Cr, V… • Large intrusions presenting compositional layering  This layering gives us information on the genetic magmatic processes at play…  Need for a meaningful way to visualise these variations in 3D
  • 3. Kevitsa Intrusion A simplified ore body model | Margaux Le Vaillant and June Hill3 |
  • 4. Kevitsa Ore A simplified ore body model | Margaux Le Vaillant and June Hill4 | plag ol px sulf
  • 5. Kevitsa 3D Model A simplified ore body model | Margaux Le Vaillant and June Hill5 | Variations within the intrusion poorly modelled
  • 6. Kevitsa 3D Model A simplified ore body model | Margaux Le Vaillant and June Hill6 |  But access to a gigantic assay database! (>92,000 analyses) Variations within the intrusion poorly modelled
  • 7. Ore Classification A simplified ore body model | Margaux Le Vaillant and June Hill7 | Ni < 2% - ‘False Ore’ S < 0.5% - ‘Not Ore’ Ni > 2% and Pd > 1,500 ppm ‘Normal Ore – High Pd’ Ni > 2% and Pd < 1,500 ppm ‘Normal Ore – Low Pd’ Ni > 10% ‘High Ni-PGE Ore’
  • 8. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill8 | Assay points visualised and classified individually / no ‘lumping’ or domaining
  • 9. A simplified ore body model | Margaux Le Vaillant and June Hill9 | 3D visualisation Need for an objective & fast simplification of the model in order to distinguish the large scale variations from the small scale one  Upscaling method using continuous wavelet transform (CWT) and tessellation methods WORKFLOW
  • 10. Multiscale Boundary Detection A simplified ore body model | June Hill10 | Signal Signalsmoothing Increasingscale
  • 11. Multiscale Boundary Detection A simplified ore body model | June Hill11 | Signal Signalsmoothing inflection point in signal: best estimate of boundary location Increasingscale many boundaries few boundaries
  • 12. A simplified ore body model | June Hill12 | continuous wavelet transform using 2nd derivative of Gaussian wavelet (convolve wavelet with signal over range of scales) (smooth & find inflection points) Method zero contours of 2nd derivative
  • 13. A simplified ore body model | June Hill13 | Multiscale Spatial Domaining “Tessellation” of continuous wavelet transform Method involves depth-correction of zero contours
  • 14. A simplified ore body model | June Hill14 | signal Filter One scaleTessellation
  • 15. A simplified ore body model | June Hill15 | Combine Domain Boundaries
  • 16. A simplified ore body model | June Hill16 | Classify Combined Domains
  • 17. Classification by Domain vs Interval A simplified ore body model | June Hill17 | Low S High S, Low Ni Mod Ni, Low PGE Mod Ni, High PGE High Ni ORETYPES IntervalDomain
  • 18. Effect of Filtering Level A simplified ore body model | June Hill18 | Low S High S, Low Ni Mod Ni, Low PGE Mod Ni, High PGE High Ni ORETYPES Weak filter Strong filter 50% 70%
  • 19. Effect of Filtering Level A simplified ore body model | June Hill19 | Low S High S, Low Ni Mod Ni, Low PGE Mod Ni, High PGE High Ni ORETYPES weak changes disappear strong changes are preserved Filter
  • 20. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill20 | unfiltered
  • 21. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill21 | 70% Filtered
  • 22. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill22 | Unfiltered 100
  • 23. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill23 | 70% Filtered 100
  • 24. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill24 | Unfiltered
  • 25. 3D visualisation A simplified ore body model | Margaux Le Vaillant and June Hill25 | 70% Filtered
  • 26. Interpretation A simplified ore body model | Margaux Le Vaillant and June Hill26 |
  • 27. A simplified ore body model | Margaux Le Vaillant and June Hill27 | Interpretation
  • 28. Genetic Model A simplified ore body model | Margaux Le Vaillant and June Hill28 | Interconnected sill sediment-complex choked with country rock inclusions
  • 29. Genetic Model A simplified ore body model | Margaux Le Vaillant and June Hill29 | Larger magmatic chamber
  • 30. Genetic Model A simplified ore body model | Margaux Le Vaillant and June Hill30 | Freely convecting magma chamber
  • 31. Genetic Model A simplified ore body model | Margaux Le Vaillant and June Hill31 |
  • 32. Conclusions A simplified ore body model | Margaux Le Vaillant and June Hill32 | • Consistent and objective reduction of the number of units in each drill hole, and creation of a simplified 3D model of the orebody  Insights on the genetic processes at play • Advantages of automated domaining process:  Consistent results over whole data base  Time saving • Domaining using CWT and tessellation results in domains whose size is a reflection of the location of major changes in the variable values – not fixed length like in conventional compositing of drill holes
  • 33. A simplified ore body model | Margaux Le Vaillant and June Hill33 | Thank you!
  • 34. A simplified ore body model | June Hill34 |
  • 35. 35 | S NiS PdIntervals Domains Low S High S, Low Ni Mod Ni, Low PGE Mod Ni, High PGE High Ni A simplified ore body model | Margaux Le Vaillant and June Hill Making Sense of the Results

Notas do Editor

  1. mathematical method for performing spatial domaining on numerical drill hole data in order to extract valuable information from large assay datasets
  2. Compositional layering (sometimes cryptic sometime not)
  3. The Kevitsa deposit is a large (237 Mt), low-grade disseminated Ni-Cu-(PGE) sulfide orebody in Arctic Finland formed within a layered ultramafic-mafic intrusion that lacks obviously recognisable internal stratigraphy
  4. This assay database represents a wealth of information  how do you interrogate it to extract fundamental ore genesis information? Major challenge: distinguishing significant trends and patterns from background and short range variability…
  5. new method of analysis of large geochemical datasets specifically intended to address the problem of distinguishing signal from noise
  6. Shallow inward dipping cryptic layering defined by sulfide composition Increasing tenors from bottom towards top of the intrusion Metal enrichment of sulfides is recognized to be the result of interaction between sulfide droplets and silicate melt.
  7. Metal enrichment of sulfides is recognized to be the result of interaction between sulfide droplets and silicate melt  R Factor Explaination of the observed variations: increasing mixing efficiency in an expanded magma chamber leading to higher effective R factors with time
  8. wholesale assimilation of country rocks, combined with a limited amount of stirring, triggered the production of high S - low tenor sulfides, or ‘False ore’
  9. continuous flux of magma being pumped into the system, allowing for more convection of the magma – interaction with larger volumes of magma – enrichment of the sulfide droplets
  10. Progressive trapping of the sulfides within the cumulus pile
  11. large regions in which there is very little change in the value of a variable will be lumped into a single domain, while narrow regions that contain values in strong contrast to their neighbourhoods will be preserved. This is particularly useful for identifying narrow regions of high grade or unusual composition.
  12. OPTIONAL SLIDE