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Compositional and structural characterisation of Ni-phyllosilicates in hydrous silicate type Ni-laterite deposits

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Academic year: 2017

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FIGURE 2.1. Orthophotograph showing the mining zones of the Falcondo deposit, including the location of the Loma Caribe peridotite belt in the Dominican Republic (left) and geological map of the same area (right) (modified from Haldemann et al., 1979)
FIGURE 2.2. Schematic lateritic profile of the Falcondo deposit, showing the position of garnierites, and including major textural features, main mineral assemblage and Ni content of each zone of the profile (modified from Lithgow, 1993; Lewis et al., 2006
FIGURE thickness of one grid from sample GAR-1(Si) before the final gentle hand polishing depicted in 3.1
FIGURE direction of movement; joints with random orientations, k) garnierite mineralisation along a fault plane; peridotites (zone E + F); IV in veins; 4.1
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