Amb motiu del tancament d'estiu, la validació de documents es reprendrà a partir del 28 d'agost de 2026. Disculpeu les molèsties.
Con motivo del cierre de verano, la validación de documentos se reanudará a partir del 28 de agosto de 2026. Disculpad las molestias
Due to the summer closure, document validation will resume starting August 28, 2026. We apologize for any inconvenience.

Files

722176.pdf (372.6 KB)

Document type

Article

Version

Published version

Publication date

2015-07

All rights reserved

Please use this identifier to cite or link to this item: https://hdl.handle.net/2445/184196

Ni-enrichment processes revealed by TEM imaging on garnierites

Journal Title

Authors

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. They usually occur as vein infillings in the lower parts of laterite profiles, and consist of fine-grained, often intimately mixed, nickelmagnesium phyllosilicates, including serpentine, talc, sepiolite, smectite and chlorite (e.g. Brindley & Maksimović, 1974).

Subject

Mineralogia, Níquel

Subject (English)

Mineralogy, Nickel

Citation

Collections

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

Citation

VILLANOVA DE BENAVENT, Cristina, et al. Ni-enrichment processes revealed by TEM imaging on garnierites. MACLA. Revista de la Sociedad Española de Mineralogía. 2015. Vol. 20, num. 149-150. ISSN 1885-7264. [consulted: 11 of August of 2026]. Available at: https://hdl.handle.net/2445/184196

Export metadata

JSON - METS

Share record