Document type

Article

Version

Published version

Publication date

All rights reserved

Please use this identifier to cite or link to this item: https://hdl.handle.net/2445/183821

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

Journal Title

Director/Tutor

Journal ISSN

Volume Title

Related resource

Abstract

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).

Citation

Citation

VILLANOVA DE BENAVENT, Cristina, et al. Dissolution kinetics of Ni-phyllosilicates from the Falcondo Deposit, Dominican Republic. MACLA. Revista de la Sociedad Española de Mineralogía. 2014. Vol. 19, num. 1-2. ISSN 1885-7264. [consulted: 15 of June of 2026]. Available at: https://hdl.handle.net/2445/183821

Export metadata

JSON - METS

Share record