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cc-by (c)  Tauler, T. et al., 2023
Si us plau utilitzeu sempre aquest identificador per citar o enllaçar aquest document: https://hdl.handle.net/2445/208243

Geochemistry and mineralogy of the clay-type Ni-laterite de-posit of San Felipe (Camagüey, Cuba)

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The Ni-laterite deposit at the San Felipe plateau, located 30 km northwest of Camagüey, in central Cuba, is the best example of a clay-type deposit in the Caribbean region. San Felipe resulted from the weathering of mantle peridotites of the Cretaceous Camagüey ophiolites. In this study, a geochemical and mineralogical characterization of two profiles (83 and 84) from the San Felipe deposit has been performed by XRF, ICP-MS, quantitative XRPD, oriented aggregate mount XRD, SEM, FE-SEM, and EMPA. Core 83, with a length of 23 m and drilled in the central part of the plateau, presents a notable concentration of cryptocrystalline quartz fragments and a rather poor content of NiO, averaging 0.87 wt.%. Core 84, which is 12 m long and drilled at the border of the plateau, lacks silica fragments and presents a higher NiO content, averaging 1.79 wt.%. The smectite structural formulae reveal that they evolve from trioctahedral to dioctahedral towards the top of the laterite profiles. Quantitative XRD analyses indicate that smectite is a dominant Ni-bearing phase, accompanied by serpentine and minor chlorite. Serpentine, as smectite, is enriched in the less soluble elements Fe3+, Al, and Ni towards the top of the profiles. Core 83 seems to have been affected by collapses and replenishments, whereas core 84 may have remained undisturbed.

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TAULER I FERRÉ, Esperança, GALÍ MEDINA, Salvador, VILLANOVA DE BENAVENT, Cristina, CHANG-RODRÍGUEZ, Alfonso, NÚÑEZ-CAMBRA, Kenya, KHAZARADZE, Giorgi, PROENZA FERNÁNDEZ, Joaquín antonio. Geochemistry and mineralogy of the clay-type Ni-laterite de-posit of San Felipe (Camagüey, Cuba). _Minerals_. 2023. Vol. 13, núm. 10. [consulta: 28 de gener de 2026]. ISSN: 2075-163X. [Disponible a: https://hdl.handle.net/2445/208243]

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