2012
DOI: 10.1016/s1003-6326(11)61264-8
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Mineralogy and crystal chemistry of a low grade nickel laterite ore

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Cited by 51 publications
(17 citation statements)
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“…Laterite nickel ore [1] is formed by large-scale weathering and deposition of nickel bearing peridotite in tropical or subtropical areas. It is an unconsolidated, hydrous, and clay-like oxide ore, which contains elements such as iron, aluminum, and silicon.…”
Section: Introductionmentioning
confidence: 99%
“…Laterite nickel ore [1] is formed by large-scale weathering and deposition of nickel bearing peridotite in tropical or subtropical areas. It is an unconsolidated, hydrous, and clay-like oxide ore, which contains elements such as iron, aluminum, and silicon.…”
Section: Introductionmentioning
confidence: 99%
“…The U.S. Geological Survey [3] reported that Indonesia has the globally largest nickel reserves of about 21 million tons in the form of laterite deposits (2018 data). These deposits comprise layers such as the limonite layer, which contains a significant amount of goethite (FeOOH), 0.5-1.7% nickel, 40-60% iron and low silica content; and the saprolite layer with containing about 1.5-3% nickel, with lower iron and higher silica contents [4].…”
Section: Introductionmentioning
confidence: 99%
“…The layer close to the surface is the limonitic ore body, the layer near to the bottom of the ore body is the saprolitic ore body, and the limonitic ore can be separated from the saprolitic ore by a transition zone. Because of the low nickel content and variable distribution in nickel laterite ores, these ores cannot be easily concentrated by current technologies [4].…”
Section: Introductionmentioning
confidence: 99%