Comment on “Compositional and temperature effects on sulfur speciation and solubility in silicate melts” by Nash et al. [Earth Planet. Sci. Lett. 507 (2019) 187–198]

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Abstract

Cooling a silicate melt isochemically may change Fe3+/Fe2+ if interaction with other redox couples is sufficiently rapid relative to the cooling rate. For typical element concentrations in common magmas, re-speciation with sulfide and sulfate anions may be significant.
Original languageEnglish
Article number116843
Number of pages3
JournalEarth and Planetary Science Letters
Volume560
DOIs
Publication statusPublished - 15 Apr 2021
Externally publishedYes

Keywords

  • redox couples
  • silicate melts
  • sulfur speciation

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