The critical role of magma degassing in sulphide melt mobility and metal enrichment
Giada Iacono-Marziano (),
Margaux Vaillant,
Belinda M. Godel,
Stephen J. Barnes and
Laurent Arbaret
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Giada Iacono-Marziano: ISTO, UMR 7327, CNRS, Université d’Orléans, BRGM
Margaux Vaillant: CSIRO, Mineral Resources
Belinda M. Godel: CSIRO, Mineral Resources
Stephen J. Barnes: CSIRO, Mineral Resources
Laurent Arbaret: ISTO, UMR 7327, CNRS, Université d’Orléans, BRGM
Nature Communications, 2022, vol. 13, issue 1, 1-10
Abstract:
Abstract Much of the world’s supply of battery metals and platinum group elements (PGE) comes from sulphide ore bodies formed in ancient sub-volcanic magma plumbing systems. Research on magmatic sulphide ore genesis mainly focuses on sulphide melt-silicate melt equilibria. However, over the past few years, increasing evidence of the role of volatiles in magmatic sulphide ore systems has come to light. High temperature-high pressure experiments presented here reveal how the association between sulphide melt and a fluid phase may facilitate the coalescence of sulphide droplets and upgrade the metal content of the sulphide melt. We propose that the occurrence of a fluid phase in the magma can favour both accumulation and metal enrichment of a sulphide melt segregated from this magma, independent of the process producing the fluid phase. Here we show how sulphide-fluid associations preserved in the world-class Noril’sk-Talnakh ore deposits, in Polar Siberia, record the processes demonstrated experimentally.
Date: 2022
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-30107-y
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DOI: 10.1038/s41467-022-30107-y
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