Neural Kriging Implementation Checklist
Neural Kriging is a hybrid geostatistical–machine learning methodology that replaces or augments traditional variogram-based spatial interpolation with neural networks trained to learn spatial covariance structures directly from sparse, noisy geological data. It integrates domain-informed inductive biases (e.g., stationarity, anisotropy constraints) into deep architectures to deliver uncertainty-aware, non-stationary grade predictions for orebody modeling. Unlike classical kriging, it learns the underlying spatial correlation function end-to-end while preserving key geostatistical properties such as unbiasedness and minimum variance estimation.
📖 Overview
📑 Key Components
🎯 Applications
- ✓ Orebody delineation in structurally complex deposits
- ✓ Real-time grade control during underground stope optimization
- ✓ Integration of multi-source geochemical/geophysical data into resource models
📐 Key Formulas
Neural Kriging Prediction
Ŷ(x₀) = f_θ(x₀) + Σᵢ wᵢ(θ) · [y(xᵢ) − f_θ(xᵢ)]
Hybrid prediction combining neural mean trend f_θ(x₀) with residual kriging weights wᵢ learned end-to-end; ensures exact interpolation at sampled locations.
Spectral Variogram Loss
ℒ_v = ||ℱ[C(h)] − ℱ[Ĉ_θ(h)]||₂²
Loss term enforcing similarity between empirical variogram C(h) and neural-estimated spectral density ℱ[Ĉ_θ(h)], ensuring learned covariance respects spatial frequency constraints.
Conditional Unbiasedness Regularization
ℒ_ub = λ · E[(Ŷ(x₀) − y(x₀)) · φ(x₀)]²
Penalizes bias conditioned on geological covariates φ(x₀), e.g., rock type or alteration index, to ensure stratified grade estimation fairness.