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Geological stochastic simulation using implicit boundary approach
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Stochastic geological modelling using implicit boundary simulation
Alejandro Cáceres, Xavier Emery, Luis Aedo, Osvaldo Gálvez
Geoinnova Consultores Ltda
Department of Mining Engineering, University of Chile
Advanced Mining Technology Centre, University of Chile
Compañía Minera Doña Inés de Collahuasi
Introduction
• Geological modelling for mineral resources evaluation: definition of homogeneous domains (“geological units”)
Introduction
Main issues with geological modelling
• Hard or soft boundary? contact analysis
Introduction
• Uncertainty in boundary position
Boundary 3
Boundary 2
Boundary 1
Current modelling approaches
Deterministic modelling
• Hand contouring, wireframing
Current modelling approaches
• Implicit modelling
Example of two geological
units:
─ For each sample, calculate a signed distance to the nearest boundary
─ Interpolate the signed distance over the domain of interest.
─ Extract the zero-distance iso-surface as the boundary of the target geological unit
Current modelling approaches
Stochastic modelling
Main geostatistical approaches
• Sequential indicator simulation
• Truncated Gaussian simulation
• Plurigaussian simulation
• Multiple-point simulation
Proposed approach
• Implicit boundary simulation
Principle: A combination of implicit and stochastic
modelling. Instead of interpolating the signed distance function, one can simulate this function using geostatisticalalgorithms
Proposed approach
• Implicit boundary simulation from available data
– Calculate the distance of each sample to the nearest boundary
– Transform the calculated distances into normal scores
– Perform variogram analysis of the transformed distances
– Simulate the transformed distances
– Truncate the resulting realisations to the zero distance
Proposed approach
Proposed approach
• Implicit boundary simulation using a reference model
– In the reference model, calculate the distance Dtrue of each node to the nearest boubdary. Transform the calculated distances into normal scores and perform variogram analysis of the transformed distances
– In the sample data base, calculate the distance Dsample of each sample to the nearest boundary. The true distance to the boundary (Dtrue) belongs to the interval [0,Dsample]
Proposed approach
– Using the transformation function and variogram determined with the reference model, simulate Dtrue conditionally to the previous interval constraint, at the data locations first (Gibbs sampler), then over the domain of interest
– Truncate the realisations to obtain the simulated geological units
Application
• Presentation of the data
– Rosario Oeste deposit
– 53,735 diamond drill hole samples with information on mineral zones: pyritic primary / sulphide zone
Application
• Implicit boundary simulation
– Distances to the nearest boundary are calculated from available data. Their normal score variogram shows a smooth behaviour in space.
Application
– Examples of conditional realisations
Application
• Geological Cross validation
– Two approaches are validated: • implicit boundary simulation (IBS)
• sequential indicator simulation (SIS)
– At each drill hole sample, the mineral zone is simulated 25 times conditionally to the remaining drill hole data.
Application
• Reproduction of the proportion of sulphide zone
Application
• Match percentage between simulation and sample data
Application
• Reproduction of down-the-hole indicator variogram
Application
• Reproduction of sulphide interval length distribution
Conclusions
Implicit boundary simulation (IBS) better reproduces sulphide indicator variogram and interval length distribution. It is able to reproduce regular boundaries and connected patterns
Unlike sequential indicator simulation, IBS also provides the distance to the nearest boundary, which conveys information about the configuration of the mineral zones.
Acknowledgements
• Compañia minera Doña Inés de Collahuasi
• Geoinnova
• ALGES Laboratory at University of Chile