Open system Re-Os isotope behavior in platinum-group minerals during laterization?

Thomas Aiglsperger*, José M. González-Jiménez, Joaquín A. Proenza, Salvador Galí, Francisco Longo, William L. Griffin, Suzanne Y. O’Reilly

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)
33 Downloads (Pure)

Abstract

In this short communication, we present preliminary data on the Re-Os isotopic systematics of platinum-group minerals (PGM) recovered from different horizons in the Falcondo Ni-laterite in the Dominican Republic. The results show differences in the Os-isotope composition in different populations of PGM: (i) pre-lateritic PGM yield187 Os/188 Os varying from 0.11973 ± 0.00134 to 0.12215 ± 0.00005 (2σ uncertainty) whereas (ii) lateritic PGM are more radiogenic in terms of187 Os/188 Os (from 0.12390 ± 0.00001 to 0.12645 ± 0.00005; 2σ uncertainty). We suggest that these differences reflect the opening of the Re-Os system in individual grains of PGM during lateritic weathering. The implications of these results are twofold as they will help to (1) elucidate the small-scale mobility of noble metals in the supergene setting and therefore the possible formation of PGM at these very low temperatures, (2) better refine the Os-isotopic datasets of PGM that are currently being used for defining dynamic models of core–mantle separation, crustal generation, and fundamental plate-tectonic processes such as the opening of oceans.

Original languageEnglish
Article number1083
Pages (from-to)1-8
Number of pages8
JournalMinerals
Volume11
Issue number10
DOIs
Publication statusPublished - Oct 2021

Bibliographical note

Copyright the Author(s) 2021. Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.

Keywords

  • Re-Os isotopes
  • platinum-group minerals
  • Ni laterite
  • Dominican Republic

Fingerprint

Dive into the research topics of 'Open system Re-Os isotope behavior in platinum-group minerals during laterization?'. Together they form a unique fingerprint.

Cite this