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Dissolution kinetics of Ni-phyllosilicates from the Falcondo Deposit, Dominican Republic

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Ni-phyllosilicates, commonly grouped under the name of "garnierites", are significant nickel ores found in hydrous silicate-type Ni-laterite deposits worldwide, formed by weathering of ultramafic rocks. Garnierites consist of one or more fine-grained nickelmagnesium phyllosilicates, including serpentine, talc, sepiolite, smectite and chlorite. They often occur as poorly crystalline micron-scale mixtures (e.g. Brindley, 1978).

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MACLA. Revista de la Sociedad Española de Mineralogía, 2014, vol. 19, p. 1-2

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(c) Villanova de Benavent, Cristina et al., 2014

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Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

# metadata.dc.title[].value
Dissolution kinetics of Ni-phyllosilicates from the Falcondo Deposit, Dominican Republic