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This document summarizes advances in non-stationary kriging near boundaries. It describes a methodology called soft boundary kriging (SBK) that accounts for non-stationary behavior of grades near boundaries. SBK was shown to better reproduce trends and features of soft boundaries compared to hard or simple soft boundary approaches. The methodology was applied successfully to synthetic and real geological models of porphyry copper deposits. Future work will extend the approach to geostatistical simulation.

Author

Renato Felipe

Language

EN