Skip navigation
Skip navigation

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

O'Neill, Hugh


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 (Métrich et al., 2009):

CollectionsANU Research Publications
Date published: 2021
Type: Journal article
Source: Earth and Planetary Science Letters
DOI: 10.1016/j.epsl.2021.116843


File Description SizeFormat Image
Compositional and temperature.pdf233.12 kBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  17 November 2022/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator