2017
DOI: 10.1007/s11053-017-9364-1
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Grade and Tonnage Uncertainty Analysis of an African Copper Deposit Using Multiple-Point Geostatistics and Sequential Gaussian Simulation

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Cited by 32 publications
(7 citation statements)
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“…Recent developments have also explored TI-free approaches [5,6]. MPS algorithms have found applications across various fields, including reservoir geology [7,8], mineral deposits modeling [9,10], seismic inversion [11], porosity modeling [12], hydrology [13], groundwater modeling [14][15][16], climate modeling [17][18][19], and remote sensing [20][21][22][23].…”
Section: Introductionmentioning
confidence: 99%
“…Recent developments have also explored TI-free approaches [5,6]. MPS algorithms have found applications across various fields, including reservoir geology [7,8], mineral deposits modeling [9,10], seismic inversion [11], porosity modeling [12], hydrology [13], groundwater modeling [14][15][16], climate modeling [17][18][19], and remote sensing [20][21][22][23].…”
Section: Introductionmentioning
confidence: 99%
“…The simulation result can reflect the spatial variation of the target attribute more realistically. Recently, geostatistical simulation methods have been widely used in the quantitative uncertainty of the geological field [14][15][16][17][18][19].…”
Section: Introductionmentioning
confidence: 99%
“…Relevant simulation algorithms include pixel-based simulations, such as the extended normal equations simulation (ENESIM) algorithm [20], the single normal equation simulation (SNESIM) algorithm [25], and direct sampling (DS) algorithm [26,27]; pattern-based simulations, such as the simulation of patterns (SIMPAT) algorithm [28]; the filter-based pattern simulation (FILTERSIM) algorithm [29], and the cross-correlation-based simulation (CCSIM) algorithm [30]. These methods have been effectively applied in reservoir simulation, hydrogeological modeling, porous media reconstruction, and other geoscience fields [31][32][33], but there are few applications related to geochemical exploration [17,34,35]. The main reason for this is that an appropriate training image (TI) is difficult to obtain through the complex geochemical element spatial distribution.…”
Section: Introductionmentioning
confidence: 99%
“…They considered dynamic updatability as one of the metrics to assess 3D geological modelling methods. Paithankar and Chatterjee [14] applied a multi-point geostatistical method and sequential Gaussian simulation to generate multiple equiprobable models of a selected deposit in Africa. Tao et al [15] created a 3D geological model based on geological maps, geological plans, cross sections and boreholes.…”
Section: Introductionmentioning
confidence: 99%