1. Open System Re-Os Isotope Behavior in Platinum-Group Minerals during Laterization?
- Author
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Thomas Aiglsperger, González-Jiménez, José M., Proenza, Joaquín A., Salvador Galí, FRANCISCO GERALDO LONGO, Griffin, William L., and O’reilly, Suzanne Y.
- Subjects
platinum-group minerals ,Re-Os isotopes ,Dominican Republic ,Mineralogy ,Ni laterite ,QE351-399.2 - 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 yield 187Os/188Os varying from 0.11973 ± 0.00134 to 0.12215 ± 0.00005 (2σ uncertainty) whereas (ii) lateritic PGM are more radiogenic in terms of 187Os/188Os (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.
- Published
- 2021