Tropical laterite-type bauxite deposits often pose a unique challenge for resource modelling and mine planning due to the extreme lateral variability at the base of the bauxite ore unit within the regolith profile. An economically viable drilling grid is often rather sparse for traditional prediction techniques to precisely account for the lateral variability in the lower contact of a bauxite ore unit. However, ground-penetrating radar (GPR) offers an inexpensive and rapid method for delineating laterite profiles by acquiring fine-scale data from the ground. These numerous data (secondary variable) can be merged with sparsely spaced borehole data (primary variable) through various statistical and geostatistical techniques, provided that the...
A typical laterite-type bauxite deposit is formed from tropically weathered mafic-ultramafic complex...
This item is only available electronically.Ground-penetrating radar (GPR) is a geophysical technique...
Demand for mineral specimens which are naturally occurring in crystallized mineral cavities in rocks...
Ground-penetrating radar (GPR) offers an inexpensive and rapid method for delineating the laterite p...
With the dramatic growth of interest in nickel laterite resource exploitation, fueled by increasing ...
In geostatistics, one of the challenges is to account for the spatial trend that is evident in a dat...
The Ravensthorpe nickel laterite deposits in Western Australia are defined by different regolith lay...
Common industry practice means that geological or stratigraphic boundaries are estimated from explor...
Lateritic soils are widely spread across the southern and central parts of India. Lateritic formatio...
The development of subsoil models represents an important aspect of land resource evaluation, becaus...
The data collected in projects of exploration and evaluation of mineral resources is spatially depen...
The GPR electromagnetic method was tested in the mapping of layered mineral deposits, located in two...
International audienceEstimation of the mineral resources potential is an important issue for most o...
Estimation of the mineral resources potential is an important issue for most of developing countries...
A more complete understanding of the spectral response patterns of bauxite‐rich rocks (and the veget...
A typical laterite-type bauxite deposit is formed from tropically weathered mafic-ultramafic complex...
This item is only available electronically.Ground-penetrating radar (GPR) is a geophysical technique...
Demand for mineral specimens which are naturally occurring in crystallized mineral cavities in rocks...
Ground-penetrating radar (GPR) offers an inexpensive and rapid method for delineating the laterite p...
With the dramatic growth of interest in nickel laterite resource exploitation, fueled by increasing ...
In geostatistics, one of the challenges is to account for the spatial trend that is evident in a dat...
The Ravensthorpe nickel laterite deposits in Western Australia are defined by different regolith lay...
Common industry practice means that geological or stratigraphic boundaries are estimated from explor...
Lateritic soils are widely spread across the southern and central parts of India. Lateritic formatio...
The development of subsoil models represents an important aspect of land resource evaluation, becaus...
The data collected in projects of exploration and evaluation of mineral resources is spatially depen...
The GPR electromagnetic method was tested in the mapping of layered mineral deposits, located in two...
International audienceEstimation of the mineral resources potential is an important issue for most o...
Estimation of the mineral resources potential is an important issue for most of developing countries...
A more complete understanding of the spectral response patterns of bauxite‐rich rocks (and the veget...
A typical laterite-type bauxite deposit is formed from tropically weathered mafic-ultramafic complex...
This item is only available electronically.Ground-penetrating radar (GPR) is a geophysical technique...
Demand for mineral specimens which are naturally occurring in crystallized mineral cavities in rocks...