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The accumulation of Ni in serpentines and garnierites from the Falcondo Ni-laterite deposit (Dominican Republic) elucidated by means of μXAS

  • Published:2017-02 Issue: Volume:198 Page:48-69
  • ISSN:0016-7037
  • Container-title:Geochimica et Cosmochimica Acta
  • language:en
  • Short-container-title:Geochimica et Cosmochimica Acta

Author:

Roqué-Rosell Josep,Villanova-de-Benavent Cristina,Proenza Joaquín A.

Funder

FEDER Funds

Spanish projects

Catalan project

Ministerio de Educación

Director, Office of Science, Office of Basic Energy Sciences, U.S. Department of Energy

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference40 articles.

1. Platinum group minerals (PGM) in the Falcondo Ni-laterite deposit, Loma Caribe peridotite (Dominican Republic);Aiglsperger;Miner. Deposita,2015

2. Critical metals (REE, Sc, PGE) in Ni-laterites from Cuba and the Dominican Republic;Aiglsperger;Ore Geol. Rev.,2016

3. μXANES study of iron redox state in serpentine during oceanic serpentinization;Andreani;Lithos,2013

4. The structure and chemistry of hydrous nickel containing silicate and aluminate minerals;Brindley;Bull. BRGM sec. II,1978

5. The nature of garnierite: I. Structure, chemical compositions and color characteristics;Brindley;Clay Clay Miner.,1973
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