Erratic behavior of platinum-group elements along an olivine–Cr-spinel cotectic in sulfide-undersaturated basaltic magma: roles of Cr-spinel and alloys

The behavior of platinum-group elements (PGE) in sulfide-undersaturated primitive magmas may be controlled by crystallization of either Cr-spinel, platinum-group minerals (PGM) or olivine. Evaluation of the PGM-hosted PGE portion is challenging because PGM in volcanic rocks are small and rare. We report on the sizes and compositions of PGM associated with Cr-spinel, the PGE content of Cr-spinel and olivine, and the bulk rock PGE content from sulfide undersaturated arc volcanics of the Tumrok range (Eastern Kamchatka). Platinum-iron and Ir-Os alloys (< 30 to > 3000 nm in size) form inclusions in Cr-spinel. Their presence and composition are mostly independent of Cr-spinel chemistry. Bulk rock PGE contents are erratic and PGE concentrations in Cr-spinel are exceptionally variable (up to 2 orders of magnitude). Whereas PGM inclusions in Cr-spinel and PGE in solid solution in Cr-spinel significantly contribute to the bulk rock PGE budget, a considerable portion of the PGE must be present associated with minerals other than Cr-spinel. The variable PGE content of the rocks is attributed to a combination of: (a) disequilibrium kinetic effects at the Cr-spinel-melt boundary layer, strongly affecting PGE partitioning into Cr-spinel and crystallization of PGM in the layer; (b) the presence of some sufficiently large PGM to cause nugget effects; and (c) melt degassing.

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Publication Details

Journal
Scientific Reports
Published
2025-04-24
DOI
https://doi.org/10.1038/s41598-025-97281-z
Citations
2
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
3.73

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article

Erratic behavior of platinum-group elements along an olivine–Cr-spinel cotectic in sulfide-undersaturated basaltic magma: roles of Cr-spinel and alloys

S. G. Kryazhev, Nikolay I. Baykov, V. D. Scherbakov, V. M. Kalugin et al.
2 citations
Scientific Reports
Geological and Geochemical Analysis
3.73
article

Erratic behavior of platinum-group elements along an olivine–Cr-spinel cotectic in sulfide-undersaturated basaltic magma: roles of Cr-spinel and alloys

S. G. Kryazhev, Nikolay I. Baykov, V. D. Scherbakov, V. M. Kalugin, Ivan F. Chayka, Vadim S. Kamenetsky, S. G. Konstantinov, Stephen J. Barnes, Anton V. Kutyrev, Nikolay V. Bryanskiy, Ivan A. Belousov, I Zhukova, Jung‐Woo Park, Alexey V. Ivanov, A.S. Stepanov
article en
2 citations

Abstract

The behavior of platinum-group elements (PGE) in sulfide-undersaturated primitive magmas may be controlled by crystallization of either Cr-spinel, platinum-group minerals (PGM) or olivine. Evaluation of the PGM-hosted PGE portion is challenging because PGM in volcanic rocks are small and rare. We report on the sizes and compositions of PGM associated with Cr-spinel, the PGE content of Cr-spinel and olivine, and the bulk rock PGE content from sulfide undersaturated arc volcanics of the Tumrok range (Eastern Kamchatka). Platinum-iron and Ir-Os alloys (< 30 to > 3000 nm in size) form inclusions in Cr-spinel. Their presence and composition are mostly independent of Cr-spinel chemistry. Bulk rock PGE contents are erratic and PGE concentrations in Cr-spinel are exceptionally variable (up to 2 orders of magnitude). Whereas PGM inclusions in Cr-spinel and PGE in solid solution in Cr-spinel significantly contribute to the bulk rock PGE budget, a considerable portion of the PGE must be present associated with minerals other than Cr-spinel. The variable PGE content of the rocks is attributed to a combination of: (a) disequilibrium kinetic effects at the Cr-spinel-melt boundary layer, strongly affecting PGE partitioning into Cr-spinel and crystallization of PGM in the layer; (b) the presence of some sufficiently large PGM to cause nugget effects; and (c) melt degassing.

Scientific ReportsVol. 15(1)
Université du Québec à Chicoutimi (CA), University of Tasmania (AU), Seoul National University (KR), Novosibirsk State University (RU), University of the Witwatersrand (ZA), Lomonosov Moscow State University (RU), China University of Geosciences (CN), Institute of Experimental Mineralogy (RU), Central Research Institute of Geological Prospecting for Base and Precious Metals (RU), Siberian Branch of the Russian Academy of Sciences (RU), Budker Institute of Nuclear Physics (RU)
National Natural Science Foundation of China, Far East Branch, Russian Academy of Sciences, Russian Science Foundation, Ministry of Science and Higher Education of the Russian Federation, China University of Geosciences, DSI-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis, Russian Academy of Sciences
Climate action
Openalex Percentile: Top 9%
Geological and Geochemical Analysis
3.73
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