Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/160419
Title: Garnierites and garnierites: Textures, mineralogy and geochemistry of garnierites in the Falcondo Ni-laterite deposit, Dominican Republic
Author: Villanova de Benavent, Cristina
Proenza Fernández, Joaquín Antonio
Galí Medina, Salvador, 1949-
García-Casco, A.
Tauler i Ferré, Esperança
Lewis, J. F.
Longo, Francisco
Keywords: Mineralogia
Geoquímica
República Dominicana
Mineralogy
Geochemistry
Dominican Republic
Issue Date: Apr-2014
Publisher: Elsevier B.V.
Abstract: Garnierites (Ni-Mg-bearing phyllosilicates) are significant ore minerals in Ni-laterites of the hydrous silicate-type. In the Falcondo Ni-laterite deposit (Dominican Republic), garnierites are found within the saprolite horizon mainly as fracture-fillings and thin coatings on joints. Field observations indicate an important role of active brittle tectonics during garnierite precipitation. Different greenish colours and textures can be distinguished, which correspond to different mineral phases, defined according to X-ray diffraction (XRD) and electron microprobe (EMP) analyses: a) talc-like (10 Å-type), b) serpentine-like (7 Å-type), c) a mixture of talc- and serpentine-like, and d) sepiolite-like types. Compositional data indicate continuous Mg-Ni solid solution along the joins lizardite-népouite (serpentine-like), kerolite-pimelite (talc-like) and sepiolite-falcondoite (sepiolite-like). In general, talc-like garnierite is dominant in Falcondo Ni-laterite and displays higher Ni contents than serpentine-like garnierites. EMP analyses showing deviations from the stoichiometric Mg-Ni solid solutions of serpentine and talc are best explained by talc- and serpentine-like mixing at the nanoscale. A detailed textural study by means of quantified X-ray element imaging provides a wealth of new information about the relationships between textural position, sequence of crystallization and mineral composition of the studied garnierite samples. These results indicate several stages of growth with variable Ni content, pointing to recurrent changes in the physicalchemical conditions during garnierite precipitation. In addition, our detailed mineralogical study of the Falcondo garnierites revealed that the different types identified have characteristic H2O content and SiO2/MgO ratios, which play important roles during the pyrometallurgy process.
Note: Versió postprint del document publicat a: https://doi.org/10.1016/j.oregeorev.2013.10.008
It is part of: Ore Geology Reviews, 2014, vol. 58, p. 91-109
URI: http://hdl.handle.net/2445/160419
Related resource: https://doi.org/10.1016/j.oregeorev.2013.10.008
ISSN: 0169-1368
Appears in Collections:Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

Files in This Item:
File Description SizeFormat 
628945.pdf1.59 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.