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Rev. Esc. Minas vol.67 número4

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Academic year: 2018

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Figure 1. Theoretical example of  how folds in the geological phenomenon  (a) may affect the analysis of spatial  continuity, and (b) how unfolding of  the layer can reduce the problem
Figure 3 Histogram of the length  of the sample of interest after the regularization by ore zone.
Table 2 summarizes the mean  calculations ignoring the differences
Figure 6 (a) Directional  variogram of variable thickness and
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